8日夏季套餐｜格陵兰一日游＋冰岛南岸＋斯奈山＋杰古沙龙＋黄金圈

• 运营日期 6月. - 8月.
• 长度 8 天
• 项目 冰川徒步, 浮潜, 岩洞, 雪地摩托, 骑马, 观鲸, 观光, 船游, 温泉, 文化, 观鸟, 飞机
• 难度 容易
• 最低年龄 10 岁
• 解说语言 English
• 亮点

  

  The Golden Circle is a 300 kilometre (186 mile) route to the three most popular natural attractions in Iceland: the Geysir Geothermal Area, Gullfoss Waterfall and Þingvellir National Park.

  This sightseeing trail is easy to do within half a day from Reykjavík, either by self-drive or on one of many tours. Some of these tours have additional activities, such as snorkelling or snowmobiling, or are conducted in a unique style, such as by helicopter, or under the midnight sun.

  Within the three locations of the Golden Circle are some of the clearest examples of Iceland’s fascinating geological forces, magnificent landscapes, and rich culture.

  The Geysir Geothermal Area

  

  The Geysir Geothermal Area is a hot-spring haven in Haukadalur Valley. As could be guessed, it is home to a famous geyser, the name of which has named all others: Geysir itself.

  Though this feature is currently in a phase of inactivity, its neighbour Strokkur more than makes up for it. Every five to ten minutes, it blasts a column of boiling water to heights that can reach over 40 metres (131 feet).

  The surrounding area is dotted with fumaroles, hot springs, and mud-pits. There are also two other smaller geysers, Smiður and Litlí-Strokkur, that can be easily visited, as well as a hotel, restaurant, cafe and gift shop across the road.

  Gullfoss Waterfall

  The 'Golden Waterfall', Gullfoss one of the most beautiful and powerful waterfalls in Iceland, plummeting 32 metres (105 feet) in two tiers into the river gorge of the popular rafting river Hvítá. It is just a ten-minute drive from Geysir and is the furthest point on the Golden Circle from Reykjavík.

  Gullfoss was very almost lost in the early 20th century when British developers sought to harness its incredible power for geothermal energy. Though they got the lease to the land, allowing them to go ahead with their plans, they met an unlikely adversary: the daughter of the farmer who owned it, Sigríður Tómasdóttir.

  This resilient woman refused to see the waterfall, to which she and her sisters paved the first path, destroyed. She, therefore, walked over 200 kilometres (124 miles) to Reykjavík and back multiple times to meet with a lawyer in order to help change the decision.

  Though the process was arduous and took years, eventually Sigríður managed to exhaust the resources of the businessmen and they withdrew their plans. Because of her, all Icelandic waterfalls are now protected from foreign investors, and she is considered one of Iceland’s first environmentalists and most important historical people.

  Thingvellir National Park

  

  The largest attraction of the Golden Circle is Þingvellir National Park. The Icelandic parliament was founded here in 930 and remained until the year 1798 before moving to Reykjavík, making it the original site of what is now the world’s longest ongoing parliament.

  Today it is a UNESCO World Heritage Site and one of the most important places to visit in Iceland. This is not just for its historical and cultural values, but for also its magnificent landscape and dramatic geology.

  Þingvellir is surrounded by a beautiful mountain and volcanic ranges, as it is located in a rift valley directly between the North American and Eurasian tectonic plates. This makes it one of the few places in the world where you can walk between the continents, in the Mid-Atlantic Rift.

  The daring and qualified even have opportunities to snorkel or scuba dive in this no-mans-land, in a ravine filled with crystal-clear spring water called Silfra. The visibility here can exceed 100 metres (328 feet), revealing incredible geological sites. Though it never freezes over due to the constant flow of water into it, it is 2°C (35°C) throughout the year, thus underwater explorers are always equipped with protective suits.

  Other sites of note are the magnificent Almannagjá gorge, which you can walk down into to reach the rift valley from the North American tectonic plate, and the beautiful lake Þingvallavatn, the largest lake in Iceland, which gleams to the south of the National Park.

  Surrounding sites

  Due to its convenient location in south-west Iceland, it is easy to visit the Golden Circle alongside with many other sites. Those seeking relaxation could head to the Secret Lagoon in Flúðir or Fontana Spa in Laugarvatn, those seeking adventure could book a trip to the ice tunnels of Langjökull glacier, and those seeking culture could visit the Sólheimar ecovillage. For more natural beauty, you can visit the nearby Kerið crater lake.

  There are many tours that include such bonuses, but if driving yourself, you should check out this guide to great detours off the Golden Circle.

  黄金圈,

  

  从地理位置来说，冰岛首都雷克雅未克同属冰岛西部。此外冰岛西部还有三大主要景区：斯奈山半岛(Snӕfellsnes)、博尔加峡湾(Borgarfjörður)和布雷扎峡湾(Breiðafjörður)。冰岛西部集聚着欧洲流速最快的温泉、冰岛最大的熔岩洞穴、迷人的冰川、美丽的瀑布、历史悠久的文化遗迹等景点。

  虽然西峡湾地区和雷克雅内斯半岛(Reykjanes)也都位于冰岛西部，但人们常将其视为两个独立的区域，将其作为特殊地区单独介绍。

  冰岛首都地区

  冰岛的首都是雷克雅未克(Reykjavík)，城市人口约为120,000，整个大雷克雅未克地区的人口则超过200,000。雷克雅未克的历史要追溯至公元870年：第一位定居冰岛的维京人英格尔夫·阿纳尔松(Ingólfur Arnarson)将此处作为定居地。

  雷克雅未克也是冰岛历史最悠久的聚落，也是冰岛文化艺术的心脏。Sónar音乐节、冰岛电波音乐节(Iceland Airwaves)、秘密夏至音乐节(Secret Solstice)都在每年如期举行；同志大游行、冰岛文化之夜等盛大的文化节日也都以雷克雅未克为主阵。城市的博物馆、艺术馆各具特色，街头艺术、雕塑作品随处可见，还有许多听现场音乐、看艺术表演的场地与美味地道的酒吧与餐厅。雷克雅未克是一座充满活力的北欧都市。

  哈尔格林姆斯大教堂(Hallgrímskirkja)、Harpa音乐会议厅、太阳航海者雕塑(Sólfar)等雷克雅未克的著名地标也都是赫赫有名的必游景点。

  雷克雅未克是许多游客的自由行基地，也是很多冰岛旅行团出发的地点。您可以在雷克雅未克攻略页面找到更多由冰岛本地人撰写的实用旅行信息。

  博尔加峡湾

  博尔加峡湾位于雷克雅未克以北，不少著名的历史和自然景点就坐落于此。例如雷克霍特(Reykholt)就是冰岛中世纪文豪斯诺里·斯图鲁松(Snorri Sturluson)的故居，他曾在这里创作出了《散文埃达》、《挪威列王传》等北欧经典文学作品。

  博尔加峡湾地区的最大城市是博尔加内斯(Borgarnes)，这也是冰岛最早有人定居的地区之一。参观当地的冰岛定居中心展览(Settlement Centre)，您将更加深入地了解冰岛历史。

  博尔加峡湾也不乏自然胜景。冰岛第二高的瀑布——格里穆尔瀑布(Glymur)以及熔岩瀑布(Hraunfossar)、儿童瀑布(Barnafoss)都跻身冰岛最美瀑布之列；冰岛最长的熔岩洞穴Viðgelmir、欧洲流速最快的温泉德尔达图赫菲(Deildartunguhver)、冰岛第二大冰川——朗格冰川(Langjökull)也都位于这个迷人的峡湾之内。

  斯奈山半岛

  有“冰岛缩影”之称的斯奈山半岛也同属冰岛西部。磅礴的斯奈菲尔冰川火山(Snӕfellsjokull)与以冰川为中心的斯奈菲尔国家公园就坐落在这座狭长半岛之上。

  斯奈山半岛因地貌丰富多样、极具冰岛特色而被誉为冰岛缩影，您将在半岛上发现火山、冰川、瀑布、山脉、熔岩原等奇妙的地理构造。半岛上最热门的景点是教会山(Kirkjufell，也称草帽山)、Gerðuberg玄武岩壁以及有“怪物海岸”之称的Lóndrangar海蚀柱。

  布雷扎峡湾

  布雷扎峡湾分割了西峡湾与斯奈山半岛，海湾内散落着无数小岛，成千上万的鸟类都以此为家，其中就包括冰岛非官方“国鸟”海鹦。

  古老的Eiriksstadir农场就位于布雷扎峡湾地区，也是维京人红发艾瑞克(Eric the Red)的故居。红发艾瑞克是第一个踏上格陵兰岛的欧洲人(于公元984年)，其子莱夫·艾瑞克森(Leifr Eiríksson)则先于哥伦布500年发现了北美洲(约于公元1000年)。

  西部冰岛,

  

  Reykjavík is the capital of Iceland and the northernmost capital of any sovereign state in the world.

  Despite a small population (approximately 120,000, with just over 200,000 in the Greater Reykjavík area), it is a vibrant city that draws an ever increasing number of visitors every year. It is the financial, cultural and political centre of Iceland, and has a reputation of being one of the cleanest and safest cities in the world.

  Geography

  The city of Reykjavík is located in southwest Iceland by Faxaflói Bay. Throughout the ages, the landscape has been shaped by glaciers, earthquakes and volcanic eruptions and the area is geothermal; after all, its name translates to ‘Smoky Bay’.

  Much of the current city area was subglacial during the Ice Age, with the glacier reaching as far as the Álftanes peninsula, while other areas lay under the sea.  After the end of the Ice Age, the land rose as the glaciers drifted away, and it began to take on its present form.

  The coastline of Reykjavík is set with peninsulas, coves, straits and islands, most notably the island of Viðey, and seabirds and whales frequent the shores. The mountain ring as seen from the shore is particularly beautiful.

  Mount Esjan is the highest mountain in the vicinity of Reykjavík and the most distinctive feature of the coastline. This majestic summit is also highly popular amongst hikers and climbers. Other notable mountains that can be seen from the seaside are Akrafjall and Skarðsheiði.

  On clear days, one may even see as far to the legendary Snæfellsjökull glacier, at the end of the Snæfellsnes peninsula.

  The largest river to run through the city is Elliðaá in Elliðaárdalur valley, which is also one of Iceland’s best rivers for salmon fishing.

  Transportation

  There are no trains or trams in Iceland, but most people travel by car. The city also operates a bus system. There are two major harbours in town, the old harbour in the centre and Sundahöfn in the east.

  The domestic Reykjavík Airport is located at Vatnsmýrin, not far from the city centre and close to the hill Öskjuhlíð and the restaurant, vantage point and exhibition centre Perlan. The international Keflavík Airport at Miðnesheiði heath then lies around 50 kilometres (31 miles) from the city.

  Cars, jeeps and bicycles can be readily rented in the city and many organized tours are also being offered. It is, however, quite easy to walk between the major sites.

  What to See & Do in Reykjavik

  The local arts scene is strong in Iceland, with annual events and festivals, many of artists from which have hit the international stage.

  Major events taking place in Reykjavík include Iceland Airwaves, Reykjavík Pride, RIFF (The Reykjavík International Film Festival), The Reykjavík Literature Festival, Culture Night, the Reykjavík Arts Festival, Food & Fun, the Reykjavík Fashion Festival and the Sónar music festival.

  Amongst the famous people from Reykjavík are musicians like Björk Guðmundsdóttir and Sigur Rós, and writers Halldór Laxness (born on the main street, Laugavegur) and Arnaldur Indriðason.

  Those eager to soak up the local culture should visit the city’s many museums, exhibitions and galleries, and check out live music at the cafés, bars, and concert venues dotted around. You could look at the programmes of what’s on at the Harpa music hall or the theatres, or else plan a few hours at the lighthouse at Grótta, the shopping street of Laugavegur, or the old harbour and the flea market.

  You could even book a bird- and whale watching tour or a visit to Viðey island. There are a lot of things to do and the possibilities are endless.

  

  Make sure to visit the public square of Austurvöllur, one of the city’s most popular gathering places, where you’ll also find the national parliament, the Alþingi, as well as the state church, a statue of independence hero Jón Sigurðsson, cafés, bars and restaurants.

  Austurvöllur was central in the protests following the banking collapse of 2008, along with Lækjargata, home to the House of Government. You are also not likely to miss the great church of Hallgrímskirkja that towers over the city from the hill of Skólavörðuholt, from which you’ll get a great view of the city.

  Try a walk by the city pond, Tjörnin, to greet the many birds that frequent the area and to visit the city hall, stationed by its banks. A beautiful park lies by the pond, ideal for a nice walk, and sometimes concerts get held there.

  Further off is the campus of the University of Iceland, the Nordic house and the Vatnsmýrin wetland, a particularly pleasant place, but be mindful to not disturb the wildlife there by keeping to the pathways.

  For a nice swim on a warm day, we particularly recommend Nauthólsvík beach, which is heated with geothermal water. Those who love a dip should also visit the Laugardalur valley, home to one of the city’s best swimming pools, which sits a short walk away from Ásmundarsafn gallery, a beautiful botanical garden and a domestic zoo.

  A walk by the Ægissíða beach, with its old fishing sheds, in the west part of Reykjavík also holds a particular charm. From there, you can see all the way to president’s house at Bessastaðir, which is also a historical site in its own right, having been the educational centre of Iceland for centuries. 

  Another place that offers one of the city’s best views is Perlan, up on Öskjuhlíð hill. The hill itself is a popular place to spend a few hours, with over 176,000 trees and great opportunities for walking and cycling. Perlan also has and observation deck with great views, a café and an exhibition centre.

  Furthermore, the city is a short drive from many of Iceland’s major attractions, most famously the Golden Circle and the Blue Lagoon. In close vicinity you’ll also find the Heiðmörk preservation area, a favourite local site of the people of Reykjavík, as well as the Blue Mountains, one of Iceland’s best skiing venues.

  Finally, we’d like to stress that these are only some suggestions of the many things you might check out in Reykjavík. Whatever you choose to do, we hope you’ll be able to make the most of your visit and we wish you a pleasant stay in our capital.

  雷克雅未克,

  

  冰岛南岸的杰古沙龙冰河湖(Jökulsárlón)是冰岛最著名的冰泻湖，位于冰岛一号环岛公路沿途，处于斯卡夫塔山自然保护区(Skaftafell)和霍芬镇(Höfn)之间，是冰岛旅行最热门的必游自然景点之一。

  地理

  杰古沙龙冰河湖由Breiðamerkurjökull冰舌的冰川融水滋养，而这条冰舌则发源自欧洲最大冰川——瓦特纳冰原(Vatnajökull)。

  一年四季无分昼夜，冰湖内始终漂浮着许多巨型冰块，其中的一些甚至与楼房等高。

  浮冰的巨型体积引人瞩目，而纯白与冰蓝混合的冰块颜色、掺杂火山灰的冰块纹理。也都令造访冰河湖的游人颇感震撼。

  

  浮冰跟随水流渐渐漂流入海，进入广袤的大西洋，而有些冰块则会被冲刷到Breiðamerkursandur黑沙滩上；这片聚集了无数如钻石般闪耀的碎冰的沙滩，也因此被冠上了“钻石冰沙滩”的名号。

  虽然杰古沙龙冰河湖只是近代才出现的自然景观，如今却已经成为冰岛最深的湖泊。目前杰古沙龙冰河湖深约248米，面积约为18平方公里。随着冰川不断消融退却，在不久的将来，杰古沙龙冰河湖也会逐步演变成冰岛最大的湖泊。

  历史

  杰古沙龙冰河湖并非自移民定居时代就一直存在的自然景观，而是在1935年才开始慢慢形成的。自20世纪以来，冰岛的平均气温逐年升高。1920年，Breiðamerkurjökull冰舌开始迅速融化退却，其融水也逐步填满了冰川脚下的大片空地，形成了一片冰河湖。

  杰古沙龙冰河湖的面积仍在持续扩张，现在的面积已经比1975年扩大了两倍以上。随着扩张持续，杰古沙龙冰河湖最终会变为峡湾。

  冰岛冰川的消融一直都是严峻的自然灾难，但无意中形成的冰河湖也称得上是一个短暂的“美丽错误”。

  

  世界各地的电影导演早已发现了杰古沙龙冰河湖的绝世之美。詹姆士·邦德系列电影《007之雷霆杀机》(1985年)、《择日而亡》(2002年)、《蝙蝠侠：侠影之谜》(2005年)等电影大片都曾在此取景拍摄，将冰河湖之美搬上了大荧幕。

  2017年，杰古沙龙冰河湖正式被纳入冰岛瓦特纳冰川国家公园，成为受冰岛法律保护的自然景点。

  野生生态

  潮汐为杰古沙龙冰河湖带来了众多的鲱鱼和毛鳞鱼，也因此吸引了许多野生动物来此安家，聚居觅食。

  夏季时，许多北极燕鸥会在此筑巢繁衍。北极燕鸥是攻击力极强的鸟类，它们会奋不顾身地攻击接近其鸟蛋的生物。如果在夏天到访冰河湖，一定不要走近北极燕鸥的巢穴，以防被攻击。此外贼鸥也会在此筑巢孵蛋、繁衍后代。

  野生海豹则一年四季都以冰河湖为家。无论任何季节到访杰古沙龙冰河湖，游人都有机会看到海豹们在巨型浮冰之间戏水嬉闹、慵懒躺卧的可爱景象。杰古沙龙冰河湖不但为海豹们提供了丰富的食物，也成为了它们避开冰岛东南部海域的虎鲸的避风港。

  杰古沙龙冰河湖,

  

  Hvíta is a glacier river in Arnessysla in South Iceland. It is one of the most popular rivers in Iceland for rafting, salmon fishing, and it is home to Iceland's most famous waterfall.

  Gullfoss Waterfall

  The river has its source in Hvítarvatn, by the roots of Langjökull. Many tributaries join it as it travels towards the ocean, making Gullfoss waterfall, which lays on its course, mightily powerful.

  At 32 metres (105 feet) tall, it falls in two steps into a magnificent canyon. There are several viewing platforms around it, and a café and visitors centre a short distance away.

  It can be seen in all seasons, with rainbows flying from its mists in summer and ice cladding the rocks around it in winter.

  Rafting in Hvíta

  Downstream from Gullfoss is the part of Hvíta that is most popular for kayaking, canoeing and rafting. To participate in rafting tours here, no experience is needed.

  These tours are not only exhilarating but expose guests to beautiful nature and geology.

  Hvítá River,

  

  Vatnajökull glacier is the largest glacier in Europe, covering 8% of Iceland’s landmass.

  It is the central feature of the Vatnajökull National park, found in the south west of Iceland, a popular spot for activities like glacier hiking from Skaftafell, boat tours in the Jökulsárlón glacier lagoon, and ice caving tours between November and March.

  Facts about Vatnajokull

  Vatnajökull has a surface area of approximately 8,100 square kilometres (3127 square miles); though it is rapidly shrinking due to climate change, its recession is not quite as advanced as at other glaciers, such as Langjökull and Mýrdalsjökull. In parts, it is a kilometre deep (over three thousand feet), and its average thickness is around half of that.

  Vatnajökull also holds the tallest peak in Iceland beneath its ice; Hvannadalshnjúkur is 2,200 metres tall (7,218 feet). It also conceals some of the most active volcanoes in the country, the most notable being Grímsvötn, Öræfajökull and Bárðarbunga.

  Volcanic activity in the region has occurred on and off throughout the centuries, and many geologists believe that several eruptions are overdue. If their calculations are correct, it would mean significant volcanic activity for Vatnajökull over the scope of the next half-century.

  Depending on winds, this could result in worldwide consequences in terms of air-travel, agriculture and the general climate.

  The glacier boasts over 30 outlet glaciers, which are channels of ice that flow out of ice caps but remain constrained on the sides of the valley. The major outlet glaciers of Vatnajökull include Dyngjujökull in the north, Breiðamerkurjökull, and Skeiðarárjökull to the south. To the west, one can find the outlet glaciers Síðujökull, Skaftárjökull and Tungnaárjökull.

  Numerous rivers run out of Vatnajökull, making up some of the greatest glacial rivers in Iceland. The most notable are:

  • Tungnaá (west)

  • Köldukvísl (west)

  • Þjórsá (west)

  • Jökulsá á Fjöllum (north)

  • Skjálfandafljót (north)

  • Jökulsá á Brú (northeast)

  • Jökulsá í Fljótsdal (northeast)

  • Jökulsá í Lóni (south)

  • Hornafjarðarfljót (south)

  • Jökulsá á Breiðamerkursandi (south)

  • Skeiðará (south)

  • Núpsvötn (south)

  • Hverfisfljót (south)

  • Skaftá (south)

  Vatnajokull National Park

  

  Vatnajökull National Park was established in June 2008 and has slowly grown to include more and more areas. The park now covers an area of 14,141 square kilometres (5,460 square miles), 14% of the country. It is the second largest national park in Europe.

  Rivers divide the highland plateau to the north of the park. The volcanic table mountain Herðubreið towers over this particular region, along with volcanoes Askja, Snæfell and Kverkfjöll.

  The canyon Jökulsárgljúfur was carved out by glacial floods centuries ago. At the upper end of the canyon, you'll find Dettifoss, the most powerful waterfall in Europe. Further north, the horseshoe-shaped canyon Ásbyrgi is believed to have formed when Óðinn's eight-legged horse, Sleipnir, stepped his foot down from the heavens.

  East around Snæfell, one can find wetlands and ranges, home to roaming herds of wild reindeer and abundant birdlife. Steep mountain ridges make up the south side of Vatnajökull, where outlet glaciers crawl onto the lowlands. The sandy plains of Skeiðarársandur also lie to the south, and the glacial river Skeiðará runs through this vast desert.

  One of Iceland's most visited landmarks in the National Park is the Jökulsárlón glacier lagoon, which sits at the base of the outlet glacier Breiðamerkurjökull. Here, large icebergs that have broken off the glacier float across a vast lake before ending up in the Atlantic Ocean, or washed ashore on the nearby Diamond Beach.

  This is one of the best seal-watching spots in the country.

  The Future of Vatnajokull

  

  The volume of Vatnajökull reached its peak around 1930 but has since been in a steady process of decline. Because of rising levels of global temperature, Vatnajökull has on average lost about a metre (three feet) of its thickness annually over the past 15 years.

  If temperature levels continue to rise, the glacier could be all but gone nearing the end of the next century, leaving only small ice caps on top of the highest mountain summits.  

  Efforts are being made to prevent what some say is the inevitable, with reforestation projects going on all around the glacier, a proven method of cooling the area. Time will tell how successful they are.

  Vatnajokull and Jokulsarlon in Popular Culture

  The beauty of Vatnajökull National Park has not gone unnoticed by those in film or television. Many famous scenes have been shot here, starting with James Bond: A View to Kill in 1985. Other notable films with scenes here include Batman Begins, Lara Croft: Tomb Raider, and James Bond: Die Another Day.

  Most famously, however, many places in Vatnajökull have been used in the HBO Series Game of Thrones, north of the Wall. The Wall itself is constructed with CGI using shots of the glacier.

  瓦特那冰川,

  

  Snæfellsjökull is a glacier-capped volcano found on the tip of the Snæfellsnes Peninsula in west Iceland. It stands in a National Park of the same name, one of the only three National Parks in the country.

  It stands at 1,446 metres (4,744 feet) tall, and on clear days, is visible across the bay from Reykjavík. The stratovolcano beneath Snæfellsjökull is 700,000-year-old.

  The mountain is actually called 'Snæfell' (Snowy Mountain), though the 'jökull' (Glacier) is often added to help distinguish it from other mountains of the same name.

  For the first time in recorded history, Snæfellsjökull had no snow or ice at its peak in August 2012, causing concern amongst locals that climate change is threatening the nature of the mountain.

  History

  Snæfellsjökull has several small villages surrounding it, including Hellissandur, Rif and Ólafsvík, all of which were some of the busiest commercial and fishing hubs in the country for much of the last millennium.

  Fishing took off primarily in the 13th-Century, with fishing stations being built in all areas with easy access to the open ocean. The Snæfellsnes Peninsula was a notable centre of this industry, due to the fertile waters within Breiðafjörður bay.

  One notable example would be the settlement of Dritvík; in spite of its minuscule size today, it once utilised around forty to sixty boats and employed up to six hundred people.

  Fishing in the region declined during the 19th century due to change in Iceland’s industry and fish stocks, though it is still an important source of livelihood for those living on the Peninsula.

  The Snæfellsjökull National Park was established in 2001, and tourism is rapidly changing the trade of the area.

  In Folklore

  Snæfellsjökull has, for centuries, been considered to be one of the world’s ancient power sites, a source of mysticism, energy and mystery for the peninsula’s superstitious population.

  The feature takes a prominent role in Bárðar saga Snæfellsáss, a late 14th-century saga that tells the story of  Bárður, half-human-half-troll, who became the 'guardian spirit of Snæfellsjökull'.

  There are many rock formations on and around Snæfellsjökull that are said to be trolls petrified by sunlight, or else homes of the hidden people.

  On November 5th, 1993, thousands of people came to Snæfellsjökull as some paranormal enthusiasts believed there would be an alien landing; CNN even showed up with a camera crew. Though the evening passed without a galactic invasion, the incident shows the strange significance of Snæfellsjökull to many.

  In Literature

  Snæfellsjökull serves as the entrance to a fantastical subterranean world in Jules Verne’s classic 1864 novel 'Journey to The Centre of The Earth.' Given its central place in the novel, Snæfellsjökull has become one of the most popular spots for visitors in Iceland and has inspired a wealth of writers, poets and artists.

  Since 'Journey to The Centre of The Earth', Snæfellsjökull has appeared in the ‘Blind Birds’ trilogy by Czech science fiction writer Ludvík Souček (partially based on Jules’ work) and in ‘Under The Glacier’, a novel by Iceland’s only Nobel laureate, Halldór Laxness.

  Nearby Attractions

  

  Along with the glacier, attractions on the Snæfellsnes Peninsula include the two nearby basalt cliffs called Lóndrangar and the many fascinating lava formations at the beautiful Djúpalónssandur beach, such as the arch rock Gatklettur.

  At Djúpalónssandur, one can also test their muscle as historic sailors once did with the four 'strength' stones, Amlóði ('Useless'), Hálfdrættingur ('Weakling'), Hálfsterkur ('Half Strength') and Fullsterkur ('Full Strength').  

  In the area, one can also explore the Saxhóll volcano crater and 'the singing cave' Sönghellir, which is named after the loud echoes inside.

  斯奈菲尔冰川,

  

  Skógafoss is one of the country’s biggest and most beautiful waterfalls with an astounding width of 25 meters (82 ft) and a drop of 60 meters (197 ft). Due to the amount of spray the cascade produces, a rainbow is present any time the sun emerges from behind the clouds.

  Located on the Skógá river, this mighty cascade is clearly visible from Route 1 and is an excellent place to stop and stretch the legs while travelling Iceland’s South Coast. The river below Skógafoss holds a large char and salmon population and is thus a favourite spot for fishermen in the summer.

  The land underneath the waterfall is very flat, allowing visitors to walk right up to the wall of water. Keep in mind, however, that this will get you drenched. Skógafoss can also be viewed from the top as a steep staircase leads to an observational platform above the cascade.

  Geography

  Skógafoss is located near the small village of Skógar, south of the Eyjafjallajökull glacier volcano. There you’ll find the Skógasafn folk museum, an open-air museum with both old wooden houses and turf houses, as well as a regional museum with various artefacts from this area.

  A part of the Skógasafn Regional Museum is the Museum of Transportation, which showcases the history and evolution of transportation, communication and technologies in Iceland. There, you can see how this nation evolved from the age of the working horse to the digital communications of the 21st century.

  The Skógasafn museum also includes a café and a museum shop, and in the village of Skógar, you will find both a hotel and a restaurant.

  At the eastern side of Skógafoss, you will find one of Iceland’s most famed hiking routes; the Fimmvörðuháls pass. The 22 km (14 mi) trail takes you along Skógá river, between two glaciers, Mýrdalsjökull and Eyjafjallajökull, before ending in the beautiful Þórsmörk valley.

  Folklore

  A gold ring is on display at the Skógasafn museum. According to legend, the ring is from a chest that was owned by Þrasi Þórólfsson, one of the first Viking settlers in the area. Folklore states that before his death in 900 AD, Þrasi buried a chest filled with gold in a cave behind Skógafoss waterfall.

  Many attempts were made to retrieve the chest after Þrasi’s death, and years later, locals managed to grasp a ring on the side of the chest. As they pulled, the ring broke off, and the treasure was lost forever. The ring was then given to the local church before it made its way to the museum.

  斯科加瀑布,

  

  Seljalandsfoss is a waterfall that can be fully encircled, situated on the South Coast of Iceland with a drop of 60 metres (200 feet).

  Due to the waterfall’s close proximity to the Ring Road and impressive natural features, it is one the country's most famous and visited falls. Majestic and picturesque, it is one of the most photographed features in all of Iceland.

  Geology and Surroundings

  Seljalandsfoss waterfall, part of the river Seljalandsá, has its origins underneath the glacier Eyjafjallajökull. The volcano beneath this ice cap was the one that erupted in 2010 and caused havoc at airports across Europe.

  The cascade of the falls is relatively narrow but falls from a tall cliff that once marked the country's coastline, the sea is now located across a stretch of lowlands and is visible from the site.

  

  The most distinguishing feature of Seljalandsfoss is a pathway that stretches all the way around it. The cliffs behind the falls have a wide cavern, and rocks and paths allow guests to fully encircle it in summer.

  Though a mesmerising opportunity, visitors should be prepared to get dampened due to the perpetual mist of the falls, which also tends to make the rocks of the pathway slippery. 

  Floodlights have been set up on both sides of the waterfall, which impressively illuminate the scene during the night when the midnight sun is not out. The lights were installed in 2001 due to the growing popularity of the falls as a tourist destination.

  After visiting Seljalandsfoss, it is common for visitors to continue north to the waterfall Gljúfrabúi, which is found partially hidden behind a rock face. Because of Seljalandsfoss extreme popularity, Gljúfrabúi is widely considered the hidden gem of the scene, as it is too often overlooked.

  Seljalandsfoss is also usually visited alongside the nearby Skógafoss. The waterfall falls from the same height, and while it cannot be encircled, it is much more powerful and steeped in the legend of a giant’s hidden treasure.

  Visitor Centre Controversy

  In 2017, it was announced that a visitor’s centre was to be constructed near the falls. The design of the building indicated that it would be seven metres (23 feet) high and 2,000 square metres (21,500 square feet) in size. Landowners in the area opposed to the idea, proclaiming that the centre would greatly alter the natural appearance of the waterfall’s renowned scenery.

  The project has neither been fully approved nor wholly cancelled, with ideas surfacing of either significantly reducing the size of the construction, or moving the visitor centre’s location further away, for instance to the nearby farmstead Brekkuhorn.

  Seljalandsfoss in Popular Culture

  Along with a multitude of South Iceland’s most famous natural attractions, Seljalandsfoss can be seen in Justin Bieber’s music video for his song ‘I’ll Show You’. Please enjoy the video without emulating any antics that will endanger yourself or the environment.

  The waterfall was also a featured waypoint during the first leg of the sixth season of The Amazing Race, an American reality TV series.

  塞里雅兰瀑布,

  

  Geysir is a famous hot spring in the geothermal area of Haukadalur Valley, found in south-west Iceland.

  Making up just one of the attractions along the world-renowned Golden Circle sightseeing route, alongside Þingvellir National Park and the mighty Gullfoss waterfall, Geysir is most well-known for having lent its name to geysers all around the world.

  Geography 

  Though Geysir itself is rarely active these days, Haukadalur Valley boasts a plethora of hot springs and geysers, including the powerful Strokkur, Smiður and Litli-Strokkur.

  Strokkur is, arguably, the country’s most famous hot spring, shooting vast jets of boiling water from 20 metres (65 feet) up to 40 metres (130 feet) high. Don’t worry about missing this incredible spectacle of nature, as Strokkur erupts every five to ten minutes; just make sure to have your camera ready.

  

  Geysir is much larger, but years can go by between eruptions here; it is currently in an inactive phase. When it does erupt, the water can shoot up in the air as high as 70 metres (230 feet).

  Just a few minutes walk north of Geysir are a wealth of fumaroles emanating steam and gas into the cool Icelandic air. Aside from watching the hypnotic pillars of steam, you will also be able to observe the yellow sulphuric stains along the fumaroles themselves, a result of the earth’s minerals crystallising around the rock bed.

  At the southern part of the valley, Þykkuhverir, you’ll find various bubbling mud pots. These spooky brown cauldrons are actually fumaroles that boil up through the loose ground; after a dry spell, these mud pools are likely to transform into a hardened fumarole.

  Nearby Attractions 

  About two kilometres (one mile) from Geysir is a preserved natural pool called Kúalaug. It has room for three to five people at a time, but care should be taken, as the area around the pool is very delicate. The temperature is 39-43°C (102-109°F), depending on where you are positioned in the pool.

  The water is slightly muddy, as the pool is built on soil, and the bottom is slippery due to algae, so caution is advised when relaxing here.

  Haukadalur has also seen a rise in reforestation in recent times thanks to continued experiments and research in the area. Today, Haukadalsskógur is one of the largest forests in south Iceland, boasting accessible walking paths (also for wheelchair users), fascinating vegetation and The Tree Museum, built in the memory of forester Gunnar Freysteinsson.

  History 

  Haukadalur has been inhabited and used as a church site since the Age of Settlement. Given its historic value, it should be noted that scholar, Ari “The Wise“ Þorgilsson, grew up here; it was also where the first pastoral school in Iceland was built.

  The current wooden church was last rebuilt in 1938 but its architectural style dates back to 1842, making it well worth a visit to see how Iceland looked before industrialisation.

  For accommodation, Hotel Gullfoss is approximately 7 kilometre from the Geysir area, and closer still is Hotel Geysir on the other side of the road from the attraction, where you will also find a restaurant, café and a souvenir shop.

  盖歇尔间歇泉,

  

  Gullfoss (translated to ‘Golden Falls’) is one of Iceland’s most iconic and beloved waterfalls, found in the Hvítá river canyon in south-west Iceland.

  The water in Hvítá river travels from the glacier Langjökull, before cascading 32 meters (105 feet) down Gullfoss’ two stages in a dramatic display of nature’s raw power. This incredible site is seen by most visitors, as it is on the Golden Circle sightseeing route.

  Because of the waterfall’s two stages, Gullfoss should actually be thought of as two separate features. The first, shorter cascade is 11 metres (36 feet), whilst the second drop is 21 metres (69 feet). The canyon walls on both sides of the waterfall reach heights of up to 70 metres (230 feet), descending into the great Gullfossgjúfur canyon. Geologists believe that this canyon was formed by glacial outbursts at the beginning of the last age.

  In the summer, approximately 140 cubic metres (459 cubic feet) of water surges down the waterfall every second, whilst in winter that number drops to around 109 cubic metres (358 cubic feet). With such energy, visitors should not be surprised to find themselves drenched by the waterfall’s mighty spray.

  As mentioned, Gullfoss makes up a part of the highly popular Golden Circle sightseeing route, alongside Geysir geothermal area and Þingvellir National Park. Many Golden Circle tours include additional activities that can be taken from Gullfoss, such as ascending the mighty nearby glacier Langjökull and entering its ice tunnels, or snowmobiling along its gleaming surface.

  History

  

  In the early days of the last century, Gullfoss was at the centre of much controversy regarding foreign investors and their desire to profit off Iceland’s nature. In the year 1907, an English businessman, Howell, sought to utilise the waterfall’s energy and harboured ambitions to use its energy to fuel a hydroelectric plant.

  At the time, Gullfoss was owned by a farmer named Tómas Tómasson. Tómas declined Howell’s offer to purchase the land, stating famously “I will not sell my friend!” He would, however, go on to lease Howell the land without the knowledge of a loophole that would allow him to proceed with his plans.

  It was Tómas’ daughter, Sigríður Tómasdóttir, who would lead the charge to stop Howell’s ambitions. Having grown up on her father’s sheep farm where she helped pave the first road to Gullfoss, she sought to get the contract nullified, hurriedly saving her own money to hire a lawyer.

  The ensuing legal battle was an uphill struggle; the case continued for years, forcing Sigríður to travel many times by foot to Reykjavík, a distance of over 100 kilometres (62 miles). Circumstances became so difficult that Sigríður threatened to throw herself into the waterfall if any construction began.

  Her tenacity, however, resulted in success. In 1929, Howell’s withdrew from the lease, unable to keep up with the costs and difficulties of his plan. The waterfall fell back into the hands of the Icelandic people.

  Today, Sigríður is recognised for her perseverance in protecting Gullfoss and is often hailed as Iceland’s first environmentalist. As such, she is one of the most famous figures in Iceland’s history. Her contribution is forever marked in stone; a plaque detailing her plight sits at the top of Gullfoss.

  Interestingly, the lawyer who assisted Sigríður, Sveinn Björnsson, went on to go down in history too; he became the first president of Iceland in 1944.

  Restaurant / Cafe

  Besides Gullfoss, visitors can enjoy the views from Gullfoss Cafe, a locally run delicatessen that serves a wide variety of refreshments and meals. The menu has options to tantalise everyone’s taste buds: hot soups, sandwiches, salads and cakes. There is also a shop on site where visitors’ can browse and purchase traditional Icelandic souvenirs.

  黄金瀑布(居德瀑布),

  

  The glacier volcano of Eyjafjallajökull is notorious the world over for causing havoc to air travel in 2010, and stumping television anchors everywhere as they tried to pronounce it. 1651 metres (5427 feet) tall, it is one of the most dominant features of the South Coast.

  Geography

  The glacier of Eyjafjallajökull is approximately 100 square kilometres (39 square miles), making it the country’s sixth largest. It sits close to the fourth greatest, Mýrdalsjökull, which also conceals another notorious volcano, this one called Katla.

  While Eyjafjallajökull’s eruption was huge and disruptive, it pales in comparison to the potential of Katla. Far more explosive, and under much thicker ice, an eruption here in unfavourable wind conditions could have worldwide consequences.

  The magma chambers between both of these mighty volcanoes are connected, and, unfortunately for us, an eruption at Eyjafjallajökull is usually followed by one at Katla within a decade.

  Eyjafjallajökull has many glacial outlets, the most famous being Gígjökull. Many rivers flow from its meltwater, and one of these falls into the beautiful South Coast waterfall, Seljalandsfoss, which it is possible to fully encircle.

  Eruptions

  Eyjafjallajökull’s most recent eruption was no doubt the most famous in Iceland’s history (although the honour really should go to Laki, the 1783-4 eruption of which caused an ash cloud so great that Europe fell into a famine that many historians believe led to the French Revolution). On March 27th, 2010, magma began to bubble from beneath the surface, and by April 14th, ash was starting to billow from the peak.

  800 people were evacuated, in fears not of magma, but of equally dangerous glacial floods, which have decimated Icelandic towns in the past. Animals were ordered to be kept inside, and those with respiratory problems told they should also stay indoors.

  Air travel across Europe was halted, as, by the evening of April 15th, the ash was already over the UK, Scandinavia, and parts of Germany. Holidaymakers were trapped, waiting for news, and would end up stuck for eight days; in Scotland and Ireland, there were even flights delayed in May due to lingering effects.

  Thankfully, no one was injured, although the ash is thought to have caused respiratory issues for some in the south of the country. Many farms were also destroyed by the ash and floods, with some farmers still struggling to recover today.

  Since settlement in 874, Eyjafjallajökull has also erupted in 900, 1612, and from 1821 to 1823. The latter released a huge amount of fluoride which is believed to have affected the bone health of humans and animals alike at the time.

  Eyjafjallajokull today

  Eyjafjallajökull is now entirely safe to visit and is seen on most tours of the South Coast in clear weather. In the town of Hvolsvöllur, there is a visitor’s centre on the volcano, which focuses on the experience of one family whose farm, Þorvaldseyri, was one of the many destroyed by the floods, lava and ash.

  It is very unlikely that Eyjafjallajökull will erupt again any time soon, with hundreds of years between each eruption, but as mentioned, its neighbour Katla might start rumbling...

  埃亚菲亚德拉冰盖（艾雅法拉火山）,

  

  Dyrhólaey Peninsula is a 120-metre promenade famed for its staggering views of Iceland’s South Coast, as well as its historic lighthouse and wealth of birdlife. It is home to a rock arch of the same name.

  Dyrhólaey, which translates to Door Hill Island, is of volcanic origin and was once an island before joining up to the Icelandic mainland. In ancient times, passing sailors used to refer to Dyrhólaey as ‘Cape Portland’.

  It is also the southernmost part of the Icelandic mainland, making it a popular stop for sightseers travelling along the Ring Road, and can be found close by the coastal village of Vík í Mýrdal.

  Other features along the South Coast en route to Dyrhólaey from Reykjavík include the waterfalls Seljalandsfoss and Skógafoss, and the glacier Eyjafjallajökull.

  Dyrhólaey Arch

  Dyrhólaey’s most instantly recognisable attraction is the promenade’s massive rock arch, a result of centuries of erosion. As a result, its name is in direct reference to this enormous arch. In fact, this natural feature is so large and dramatic that one daredevil pilot even flew through it, back in 1993. Boats can easily cruise through its opening.

  Dyrhólaey Wildlife

  Dyrhólaey has an abundance of birdlife, the most common year-round being Eider Ducks. Iceland’s favourite winged resident, the migratory Atlantic Puffin, can be found here from May to September.

  It is one of the best places to reliably locate them, and one of the closest to Reykjavík after the islands in Faxaflói Bay which can be visited by boat from the Old Harbour.

  While watching puffins, it is striking how little they seem to fear people, as they allow you to get very close. Be aware, however, they do not like to be touched, and if one flies off in a panic, the whole flock might follow it, so be respectful.

  Features at and around Dyrhólaey

  From your position atop the promenade of Dyrhólaey, you can enjoy staggering views over Iceland’s black sand beaches, complemented by the glittering waves of the Atlantic on one side, and distant mountainscapes to the other.

  The most notable stretch of coast here is called Reynisfjara, renowned for its incredible geology, with the sea-stacks of Reynisdrangar jutting up out to sea. If you visit this beach while seeing Dyrhólaey as part of a South Coast adventure, be sure to follow the warning signs and stay away from the water as dangerous sneaker waves here are commonplace.

  To the north, you will also able to see the creeping glacier, Mýrdalsjökull. This amazing ice cap conceals a secret; beneath its surface is one of the most explosive and notorious volcanoes in all of Iceland, Katla. Long overdue, experts say that it is a matter of when - not if - it will erupt over the coming years.

  On top of Dyrhólaey stands Dyrhólaeyjarviti, a beautiful old lighthouse that consists of a white, square concrete tower. The first lighthouse in the area was built in 1919; the current construction was completed in 1927. Visitors here will be able to see the lighthouse flicking out beams of white light to sea every ten seconds.

  

  迪霍拉里,

  

  辛格维利尔国家公园，又译辛格韦德利国家公园，是冰岛大陆上唯一被联合国教科文组织认证为世界文化遗产的地点。它和盖歇尔间歇泉、黄金瀑布，组成了著名的黄金圈旅游线路。公园南侧是冰岛最大的湖泊－辛格瓦德拉湖（Þingvallavatn）。

  地理

  辛格维利尔的地理地质特性在世界上独一无二。欧亚大陆板块与美洲大陆板块在此相会，且暴露在海平面之上。全世界只能在冰岛看到两大地质板块在海平面之上相会的地质奇观。

  游览时，建议从美洲大陆板块一侧开始观光，在这里的信息牌上可以阅读到这个地区的更多有趣信息和历史，之后可以再走入其下的山谷。

  历史

  

  辛格维利尔在冰岛语中的意思为“议会土地”，从它的名字就不难猜出它的历史。在这里，世界上的第一个民主议会诞生－公园930年，维京人选址在此，创立了冰岛的议会。

  民主议会也许和维京人喜欢战争掠杀的名声背道而驰，但当时的30多个氏族急需在恶劣的新环境中求得生存与繁荣。第一次集会的空前成功，让议会得以保留。每年，人们聚集在此，解决争端、审判罪犯、制定让所有人都能受益的法律。

  冰岛联邦就此诞生，让冰岛人在成为挪威王国的选民前就获得了独立与自由。冰岛在辛格维利尔的年度议会一直延续到了1798年。

  丹麦王国取消了冰岛的议会，直至1845年，冰岛的议会在雷克雅未克重生。

  辛格维利尔在冰岛历史上的另一个重要角色与信仰有关，公园1000年，挪威入侵冰岛，冰岛人在辛格维利尔舍弃异教信仰、北欧众神，转而投信基督教。

  冰岛的法律演讲人、议长Þorgeir Ljósvetningagoði是冰岛的这场信仰危机中起到了决定性的作用，他考虑了一天一夜，才回到这里宣布了他的决定。

  为了见证冰岛信仰的转变，Þorgeir将北欧众神的神像抛入北部的众神瀑布－Goðafoss，瀑布正得名于此。

  丝浮拉裂缝

  

  辛格维利尔是冰岛最受欢迎的自然景点之一，而除了上述的自然、历史原因，它还有另一大独特的景观－丝浮拉裂缝（Silfra，又译史费拉裂缝）。丝浮拉裂缝流淌着冰川水，是世界上排名前十的浮潜、潜水地。

  丝浮拉在冰岛语中意为“银”，是公园内的一个水下峡谷，能见度高达100余米，温度常年保持在零上。世界各地的人们在这里穿上潜水衣，去水下享受完美的失重感，以及遨游在两大地质板块间的难得体验。

  辛格维利尔,

  

  Hraunfossar ('Lava Falls' in English) in Borgarfjörður district is a series of beautiful waterfalls formed by rivulets streaming out of the Hallmundarhraun lava field. It is located in West Iceland near another waterfall called Barnafoss.

  Geography and Surroundings of Hraunfossar

  The lava field that Hraunfossar trickles through flowed from an eruption of one of the volcanoes lying under the nearby glacier of Langjökull, the second largest ice-cap in Iceland. The waterfalls pour into the Hvítá river from ledges of less porous rock in the lava.

  The Hvítá river is one of the most popular rivers amongst visitors for two reasons. Firstly, it is the most easily accessible rafting river from Reykjavík, with rapids that are manageable even for total novices. Secondly, it is the river that hosts the mighty waterfall Gullfoss, one of the three sites of the popular the Golden Circle route.

  

  Because the area around Hraunfossar used to be the site of constant eruptions, the lava fields are known for their hidden caves. The country's longest cave, Víðgelmir, can be found near the waterfall. This amazing feature is 1,595 metres long (5,200 feet), up to 15.8 metres high (52 feet) and 16.5 metres wide (54 feet).

  Its geological history may be fascinating, being just a thousand years old, though its human history stirs just as much intrigue as the lava field was once home to bandits and, according to folklore it is the home of trolls.

  Another major site near Hraunfossar is an incredibly short walk away, and though also a waterfall, could not be more different. Barnafoss surges down a narrow, rocky valley with ferocious power, foaming and churning quite spectacularly. According to legend, however, the force of these rapids led to tragedy.

  It was said that an old stone bridge once went over the falls, and two boys at a nearby farm, bored at home, attempted to cross it to catch up with their parents at church. However, they felt dizzy due to its height, fell, and drowned.

  The legend ends in two different ways, with the least interesting saying the mother in grief simply ordered the bridge destroyed. Other tales say that she cursed the bridge using an Icelandic rune so that any who crossed would meet the same fate as her sons.

  In this version, the bridge and curse were later broken by an earthquake.

  The story led the waterfall its name; it translates to ‘Children’s Falls’.

  Settlements near Hraunfossar

  The nearest settlement of significance to Hraunfossar is Reykholt.

  This tiny village has a huge history, being home to the legendary writer, chieftain, lawspeaker and poet Snorri Sturluson. Without Snorri, huge amounts of Icelandic, Nordic and even British history would be unknown.

  He alone at the time catalogued a history of Norwegian kings and their relations with other monarchs through the work Heimskringla, as well as the Norse mythological beliefs through Prose Edda. It is also believed that Snorri first wrote many of the sagas still read today.

  Reykholt has a centre dedicated to Snorri called Snorrastofa, which discusses his fascinating life as much as his works. Working during the times of Iceland’s tumultuous civil war as a chieftain, lawspeaker and spokesman of the Norwegian king, who had ambitions to take the country, it is a story with as much politics, betrayal, blood and sexual impropriety as Game of Thrones.

  Hraunfossar is also reasonably close to Borganes, another town with a long history. Here, visitors can see the Settlement Centre with its two exhibitions on Iceland’s past, one is on the first people to reach this island over a thousand years ago, and the other is on Iceland’s most famous saga, Egil’s Saga.

  赫伦瀑布群(熔岩瀑布),

   

  

  Deildartunguhver is a hot spring located in Reykholtsdalur, a district of west Iceland. Deildartunguhver is the highest flowing hot spring in Europe and is widely known for its rapid flow rate of 180 litres (380 pints) per second.

  Geothermal activity at Deildartunguhver

  Reykholtsdalur is one of Iceland’s most popular places to see hot springs, along with the Geysir Geothermal Area, the Highlands, the Reykjanes Peninsula, Reykjadalur Valley and Námaskarð Pass. While each of these areas have their appeal, at no other does the water rise with such ferocity.

  The water at Deildartunguhver hot spring emerges at a constant 97 degrees Celsius (207 degrees Fahrenheit), making it incredibly dangerous for those who venture too close. Thankfully, there are a number of wooden walkways and observation points that lead you around the hot springs without putting you at any risk.

  Due to the sheer energy bubbling under Deildartunguhver, much of the water is used for heating Icelandic homes. One pipe travels 34 kilometres (21 miles) to Borgarnes, whilst another travels 64 kilometres (40 miles) to Akranes.

  This means that if you’ve taken a shower or bath within a 64-kilometre radius of Deildartunguhver, you will have touched the water from the hot spring.

  All Icelandic hot water comes from hot springs such as this, except in some parts of the Westfjords which are now geologically much older than the rest of the country, and thus less active.

  This is a fantastic example of how Icelanders efficiently use the geothermal energy provided and is one of the major reasons as to why Iceland has such an excellent reputation for green energy.

  Points of Interest at Deildartunguhver

  

  Whilst in the area, many visitors choose to make a stop at Krauma Geothermal Bath & Spa, a fantastic and relaxing complex that makes for a cheaper, more isolated alternative to the Blue Lagoon.

  Visitors to Kraua will experience the hot water of Deildartunguhver blended perfectly with glacial water from Iceland’s smallest ice cap, Ok (which rhymes with ‘talk’), creating the perfect bathing temperature.

  Krauma has a total of six pools, a relaxation room and two steam baths.

  Visitors to Deildartunguhver with an interest in botany will also be able to check out the Blechnum Spicant, aka; “deer fern”, a type of plant that grows nowhere else in Iceland.

  Surroundings of Deildartunguhver

  Deildartunguhver is located in west Iceland. The two most notable points of interest nearby are two waterfalls, Hraunfossar and Barnafoss.

  Hraunfossar, or the ‘Lava Falls’, is, in fact, a series of tiny cascades that trickle through an old lava field. Barnafoss, or ‘the Children’s Falls’, is a more powerful rapid, steeped in a dark legend.

  Deildartunghver is also near Víðgelmir, the longest lava cave in the country, trailing for 1,595 metres (5,200 feet) beneath the surface of the earth.

  The most significant settlement near Deildartunghver is Reykholt, a beautiful village with a fascinating history. This settlement was once home to Snorri Sturluson, a historian, writer, chieftain and poet without whom we would know very little of the Nordic mythology, folklore and history at the time.

  His works, and life--full of politics, betrayal, affairs and war--can be learnt about in the town at the Snorrastofa Centre.

  德尔达图赫菲,

  

  Strokkur is Iceland’s most visited active geyser. One of the three major attractions on the world-famous Golden Circle sightseeing route, it is usually visited alongside Gullfoss Waterfall and Þingvellir National Park.

  Strokkur is found in the Geysir Geothermal Area, titled after the Great Geysir, which lent its name to all others across the world. It is the greatest active geyser on site; Geysir itself is in a period of inactivity. Strokkur erupts more regularly than Geysir ever did, blasting water to heights of around fifteen to twenty metres every five to ten minutes, although it is known to reach up to forty metres. 

  Strokkur and Haukadalur Valley

  

  Strokkur is the primary feature of the Haukadalur valley and the main reason why it is one of the most visited sites in the country. While Geysir will very occasionally still erupt to enormous heights, it is nowhere near reliable enough to justify the area’s popularity.

  Haukadalur valley, however, has many other features that make it worth a visit. The natural beauty of the area is shaped by the forces of the earth; fumaroles, hot-springs, mud-pits and other little geysers are littered around, and the ground itself is dyed vividly by elements such as sulfur (yellow), copper (green) and iron (red).

  Opposite the main geothermal area in Haukadalur Valley is a restaurant, cafe, hotel and luxury gift shop.

  Science behind Strokkur

  

  Active geysers like Strokkur are rare around the world, due to the fact that many conditions must be met for them to form. They are thus only found in certain parts of highly geothermal areas.

  The first condition that is necessary is an intense heat source; magma must be close enough to the surface of the earth for the rocks to be hot enough to boil water. Considering that Iceland is located on top of the rift valley between the North American and Eurasian tectonic plates, this condition is met throughout most of the county.

  Secondly, you will need a source of flowing underground water. In the case of Strokkur, this comes from the second largest glacier in the country, Langjökull. Meltwater from the glacier sinks into the surrounding porous lava rock, and travels underground in all directions.

  Evidence of this flowing water can be found in Þingvellir National Park, where there are many freshwater springs flowing straight from the earth.

  Finally, you need a complex plumbing system that allows a geyser to erupt, rather than just steam from the ground like a fumarole. Above the intense heat source, there must be space for the flowing water to gather like a reservoir. From this basin, there must be a vent to the surface. This vent must be lined with silica so that the boiling, rising water cannot escape before the eruption.

  Environmental Issues with Strokkur

  One of the main reasons that Geysir entered a period of inactivity was due to the fact soap used to be pumped into the vents to make the eruptions more dramatic; it damaged the structure of the vent and prevented water building up. Strokkur, therefore, is guarded against all interference, with chains keeping visitors a good distance away.

  Unfortunately, however, there have been incidents where people have meddled with its natural state. For example, an artist called Marco Evaristti once poured food colouring into it to make the eruption pink. He defended himself by claiming that nature was open to artists to utiltise and the fact the colouring was all-natural, but he became a pariah amongst many Icelanders, and was arrested and fined (though never paid it).

  史托克间歇泉,

  

  Snæfellsnes is a large peninsula extending from West Iceland, often nicknamed ‘Iceland in Miniature’ due to its wealth and diversity of natural features found there.

  Home to the Snæfellsjökull National Park, at the centre of which is a subglacial volcano that towers over the scenery, this peninsula is home to waterfalls, rock formations, beautiful beaches, historic villages, and an intricate folklore.

  In particularly clear weather, the Snæfellsnes Peninsula can sometimes be seen from Reykjavík, making views across the water from the capital of Iceland particularly beautiful. Those with an extended stay in Iceland are recommended to look into spending at least a day here.

  Natural Sites of Snaefellsnes

  

  The peninsula stretches 90 kilometres (56 miles) from West Iceland, between the Reykjanes Peninsula to the south and Westfjords to the north. A mountain range runs along it, consisting of both active and dormant volcanoes, culminating at the magnificent, ice-capped Snæfellsjökull volcano.

  Starting along the south side of the Snæfellsnes Peninsula, you will first come to the Eldborg crater, which can be scaled for some incredible views, and the Gerðuberg basalt cliffs, where hundreds of hexagonal basalt columns are arranged with geometric precision. You will then start hugging the coast, where animal-lovers can find the Ytri-Tunga beach and its year-round seal colony.

  The next site of particular natural beauty is the Rauðfeldsgjá Gorge, a cleft in a huge cliff face that it is possible to climb into. A stream runs through here, so those who want to plumb its depths will get wet. Those with decent clothing, sturdy shoes and reasonable fitness, however, will be able to get quite far.

  After Rauðfeldsgjá, you will come to the mighty basalt plugs of Lóndrangar. All that remains of what was once a massive crater, these two enormous pillars are not only awe-inspiring in their scale, but home to thousands of nesting seabirds.

  You will then enter Snæfellsjökull National Park, which, in spite of being the smallest of the country’s three national parks, is pregnant with destinations worth visiting.

  The most historic of these is Djúpalónssandur beach. Comprised of black, volcanic sands, it is best-known for the four lifting stones that remain on the beach from a bygone age. Fishermen would use these stones to mark their strength, and gage their suitability to working on the dangerous waves.

  Within the National Park are also two lava caves that can be entered in summer. Sönghellir is renowned for the musical qualities of its echoes, whereas Vatnshellir is favoured for its easy access and vivid colouration. There is a small entry fee to the latter and you cannot enter it without a guide.

  Of course, however, the highlight of this part of the Peninsula is no doubt Snæfellsjökull itself. Even if you are not ascending it on a glacier hiking tour, it is worth stopping by to marvel at.

  This is particularly the case for literature enthusiasts. The adventure in the Jules Verne novel ‘A Journey to the Centre of the Earth’ begins here, and it is the backdrop to the lesser-known novel ‘Under the Glacier’, by Nobel-Prize winning Icelander, Halldór Laxness.

  On the north side of the peninsula is the haunting Berserkjahraun lava field, near the town of Bjarnarhöfn, the history of which weaves deception and murder. Most notable on this stretch, however, is the mountain Kirkjufell, often described as the most photographed mountain in Iceland, and known as "the mountain shaped like an arrowhead" from the popular HBO series, Game of Thrones.

  Cultural Sites of Snaefellsnes

  

  There are a few small and beautiful villages dotted across the peninsula, the majority of which are on the northern side, where the fishing is better. Most notable are Arnarstapi, Hellnar, Búðir, Hellissandur, Ólafsvík, Grundarfjörður and Stykkishólmur.

  The last of these is highly popular for travellers, featuring a volcano museum and a ferry that takes you across the fascinating Breiðafjörður bay to the south border of the Westfjords with a stop at the remote island of Flatey.

  Other museums of note are the Maritime Museum at Hellissandur, the regional museum at Ólafsvík, and, last but not least, the shark museum at Bjarnarhöfn, where you can taste the Icelandic ‘delicacy’, hákarl, or fermented shark.

  斯奈山半岛,

  

  Hvalfjörður is a fjord in southwest Iceland. The fjord is approximately 30 kilometres (19 miles) long and five (three miles) kilometres wide.

  Nature and Landscape

  The landscape of Hvalfjörður is varied and beautiful, with wide areas of flat land along majestic mountains, green vegetation in summer and beaches cut with creeks.

  The area is rich in bird life and is home to seals, but despite its name, which translates to ‘Whale Fjord,’ it is not known for its whale or dolphin populations. Two theories exist on how it got its name; either that it was once home to whales before fish stocks moved away, or because of the general shape of the bay.

  The area has recently been part of Iceland’s successful reforestation effort. 

  Natural attractions in the area are plentiful but most significant is Iceland's highest waterfall, Glymur, in the river Botnsá. There are also plenty of interesting hiking trails in the area, such as Síldarmannagotur, leading north, and Leggjabrjótur, leading east towards the area of Þingvellir National Park. 

  History and Culture

  Historically, Hvalfjörður was home to one of the main whaling stations in Iceland, with ships heading out into Faxaflói Bay. It was one of the most important naval stations in the North Atlantic during World War Two, when Iceland was occupied by the Allies after the Nazis conquered Denmark.

  The old whaling station and a war museum can be found in the fjord. 

  Iceland's main psalm poet, Hallgrímur Pétursson, writer of the ‘Passia Hymns,' lived in Hvalfjörður. The area was also the home of the late Sveinbjörn Beinteinsson, poet and performer and head of the Icelandic Pagan Association. 

  Economy

  Most inhabitants of the fjord live in rural areas, and there is some farming in the area. Until the 1990s those travelling between Borgarnes and Reykjavík had to take a long detour around the fjord, but this was solved with a tunnel that travels beneath it, finished in 1998.

  Grundartangi promontory in Hvalfjörður has one of the largest harbours in the country and two industrial plants. One is a ferrosilicon plant, operated since 1979, the other an aluminium smelter, operated since 1998.

  Both of these were controversial during their construction, and continue to be controversial during their ongoing operation. Along with whaling and hydroelectric dams, smelters and silicone plants are the hottest environmental debates going on in Iceland.

   

  Hvalfjörður,

  

  Sólheimajökull is an outlet glacier of the mighty icecap of Mýrdalsjökull on the South Coast of Iceland. It is one of the most easily accessible glaciers to reach from Reykjavík, just 158 kilometres (98 miles) away.

  For those who are based in Reykjavík, it is by far the favourite spot on which to take guided glacier walks, competing nationally for popularity only with Svínafellsjökull in the south-east.

  Geography of Solheimajokull

  About eight kilometres long and two kilometres wide (five miles long and just over a mile wide), Sólheimajökull is an impressive feature. Due to the way it descends from Mýrdalsjökull, however, without a clear distinction between the two, it appears much bigger.

  Mýrdalsjökull itself has many other outlet glaciers; overall, it is the fourth largest ice cap in Iceland. Beneath its thick surface is one of the country’s most infamous volcanoes, Katla.

  The nearby Eyjafjallajökull erupted in 2010 causing widespread havoc at European airports. Throughout history, eruptions in Eyjafjallajökull mean that Katla will also erupt, and so the volcano is due to go off soon. However, volcanoes and all seismic activity in Iceland is highly monitored, meaning that it is perfectly safe to travel around the area and even take an ice cave tour in the glacier above.

  Sadly, like all the glaciers in Iceland bar one, Sólheimajökull is shrinking rapidly. A glacier lagoon at its base reveals how quickly it is receding: the length of an Olympic swimming pool every year. It seems like this change is already an irreversible consequence of climate change, and it may be gone within decades.

  Visitors to Iceland should, therefore, make sure they witness the ice-cap while it is still with us.

  

  Sólheimajökull has several distinctive traits that separate it from other glaciers. Firstly, it is incredibly easy to find, laying just off of the Ring Road that encircles Iceland. Secondly, it is not surrounded by tall mountains, meaning those who ascend it can attain incredible views of the South Coast. Thirdly, it is home to many walls of ice that can be climbed up with ice axes on certain tours.

  There are also crevasses that snake across the surface, spectacular ice ridges and formations, and a vivid colouration that dances between a gleaming white, electric blue, and ash black. Occasionally, you will even find an ice cave, though these can never be guaranteed.

  A river runs from the meltwater of the glacier tongue, called the Jökulsá á Sólheimasandi. This river runs through a glacial outwash plain - otherwise known as a black-sand-desert - of Sólheimasandur to the nearby ocean.

  Tours on Solheimajokull

  Many day tours run from Reykjavík to Sólheimajökull, for glacier hikes or as part of a greater South Coast tour.

  Greater South Coast tours include visits to other features, such as the incredible waterfalls of Skógafoss and Seljalandsfoss, the black sand beach Reynisfjara, and some even reach Vatnajökull National Park and the Jökulsárlón glacier lagoon.

  Hidden crevasses and ice caves, slippery surfaces, and the threat of rock- or ice-falls all pose dangers on glacier hikes, but glacier guides have to pass several training courses to deal with these eventualities, making the activity quite safe for those in a fit state of health.

  All guests are equipped with helmets, ice axes, and crampons, and should arrive wearing warm clothes and sturdy hiking boots.

  It is forbidden to ascend glaciers without the correct equipment or training, for your safety and the safety of others. There have been injuries and deaths on Sólheimajökull before, and glacier guides have had to risk their lives to rescue those who flouted the rules.

  索尔黑马冰川,

  

  斯卡夫塔山是冰岛Öræfasveit地区的一个自然保护区，它曾经是一个国家公园，2008年，和杰古沙格鲁夫尔(Jökulsárgljúfur)国家公园合并为如今的瓦特那冰川国家公园(Vatnajökull National Park)。

  斯卡夫塔山地区的植被非常有特色，它们生长在沙地与冰川形成的特色地貌上，给整个地区带来盎然生机和独特的自然风光。从斯卡夫塔山游客中心可以沿徒步路径通向斯瓦蒂瀑布(Svartifoss，意为黑瀑布，又译为魔鬼瀑布)、Hundafoss瀑布，以及斯卡夫塔山冰川，远处是Kristinartindar山和Morsardalur山谷。

  对于户外爱好者，斯卡夫塔山是前往冰岛最高峰－华纳达尔斯赫努克火山(Hvannadalshnjúkur)的最佳营地选择。

  斯卡夫塔山游客中心(Skaftafell Visitor Center)

  在斯卡夫塔山的游客中心，您可以找到此地区最完备的信息，以及它的历史、地理知识。您可以了解以此为出发地的各个徒步线路、观光建议、住宿选择等。

  斯卡夫塔山,

  

  Silfra is a fissure filled with fresh spring water within Þingvellir National Park, and one of the country’s most cherished wonders. Snorkelling and diving in its crystal-clear waters is an experience that is both thrilling and relaxing, and it is now considered to be one of the top five dive sites in the world. It takes around an hour to reach Silfra from Reykjavík. 

  Geography of Silfra

  

  Silfra fissure opened in 1789, due to the movements of the tectonic plates that frame Þingvellir National Park. The North American and Eurasian plates, which run all the way through Iceland, separate at about 2 centimetres per year, and as they do, they tear open fissures in the land between them. 

  Some of the ravines fill with water travelling underground through the porous lava fields in the area, originating from Langjökull glacier about 60 kilometres north. It can take the water up to a century to reach Silfra and this long filtration process results in the water being both extremely clear and drinkable.

  

  Because the water travels underground, it maintains a constant temperature of two to three degrees Celsius and does not freeze over immediately at the source of the spring. Snorkelling and diving tours are thus open throughout the year.

  The clarity of the water is what draws most visitors. The visibility can extend to over 100 metres, allowing you to see the canyon walls and bottom like you are floating over a great cathedral.

  The last colour that water absorbs is blue, which means that when you look forward in Silfra, it is as if you are looking into an ethereal, vivid, azure world. The clarity also means that sun-rays refract through the surface of the water, creating rainbows on Silfra’s bed when the weather allows. 

  Snorkelling in Silfra

  

  Snorkelling in Silfra fissure is a highly enjoyable activity, but you must meet some prerequisites to be able to join. These are as follows:

  • You must be able to swim
  • You must be over 16
  • You must be in good physical health
  • You must be at least 145 centimetres and 45 kilograms
  • If you are over sixty, you will need a medical waiver
  • If you are over forty-five with a history of heavy alcohol use and pipe smoking, you will also need a waiver

  The most common option for snorkelling is to conduct it in a drysuit. Drysuits work with a fluffy undersuit to keep your body free from water and insulated against the cold, making the task of swimming through the near-freezing temperature more than achievable. 

   

  While drysuit snorkelling is the most comfortable and popular option, a few tours allow you to go through Silfra wearing a wetsuit. Wetsuits, made of neoprene, allow water to surround your body in a thin layer, that your body then heats up and uses to protect you. Though they grant you more flexibility, they are not so warm, so this should be done by the daring; you will also need to be at least 50 kilograms to snorkel in a wetsuit.

  In all tours, you wear neoprene on your head and hands to allow for better mobility, a mask and snorkel, and a pair of fins, all of which are provided on site. The course of Silfra takes approximately forty minutes, and there is a gentle current throughout, meaning it requires minimal energy to traverse.

  Diving in Silfra

  

  Diving through Silfra gives an extra dimension to its beauty, as you will be able to look up and see the sun glistening upon the surface as you cruise through the crystal clear waters. However, considering the risks associated with diving in cold water and cumbersome equipment, all who partake must meet all the requirements above, as well as one of the following:

  • You must be a qualified diver with a certification in a drysuit speciality, OR
  • You must be a qualified diver with at least 10 logged dives in a drysuit conducted over the past two years, signed by an instructor or divemaster.

   

  Silfra,

  Photo from Thrihnukagigar Volcano Tour

  Þríhnúkagígur is a dormant volcano in west Iceland, famous for its enormous magma chamber. It is the only magma chamber in the world that can be entered, and has a depth of 213 metres (699 feet).

  Formation of Þríhnúkagígur

  Þríhnúkagígur was a normal volcano in Iceland’s Blue Mountain range, also call Bláfjöll. However, its last eruption, almost 2,000 years ago, had some very unusual consequences.

  After an eruption, the magma chamber of a volcano, now free of pressure, usually remains full of lava that cools into solid rock until the next eruption. If the magma chamber is fully emptied, the volcano will usually collapse in on itself.

  To the bewilderment of scientists, however, neither of these things happened to Þríhnúkagígur.

  It seems that a rift beneath the chamber drained it of all remaining lava, leaving behind an enormous chamber, that covered an area of 3,270 square metres (35,200 square feet). To give some idea of the scale of this, the Statue of Liberty could stretch her limbs within it, and it could comfortably fit Hallgrímskirkja church.

  Unusually, the volcano did not collapse, and it has remained unchanged since.

  Discovery and Exploration of Þríhnúkagígur

  The vast magma chamber under Þríhnúkagígur would not be discovered until 1974, by an Icelandic cave explorer. Its discovery made world news, as volcanologists had not seen anything like it before, and were fighting to try to explain its existence.

  In 2012, it was opened for tourism. A lift, akin to those used in mining, was installed, and visitors were now allowed to join tours plumbing its depths.

  Its popularity comes not only from the uniqueness of the tour and the scale of the chamber, but the incredible colouration within it. Mineral deposits dye the walls vivid shades of red, yellow, green and blue, making the incredible space that much more ethereal.

  Reaching Þríhnúkagígur requires a short but uphill hike, which can be done by any steady on their feet with a reasonable level of fitness. Tours only operate in summer.

   

  Þríhnúkagígur,

  Reynisfjara is a world-famous black-sand beach found on the South Coast of Iceland, just beside the small fishing village of Vík í Mýrdal.

  With its enormous basalt stacks, roaring Atlantic waves and stunning panoramas, Reynisfjara is widely considered to be the most beautiful example of Iceland’s black sand beaches. In 1991, National Geographic voted Reynisfjara as one of the Top 10 non-tropical beaches to visit on the planet.

  Reynisfjara is found around 180 kilometers (112 miles) from Iceland’s capital city, Reykjavík, and is a popular stop-off for those taking a sightseeing tour along the popular South Coast.

  Driving to the beach is particularly easy, taking an approximate two and a half hours from the capital, so can easily be done within half a day, or a full one combined with other features.

  Folklore

  Upon visiting the beach, travelers will immediately observe rocky sea stacks sitting off the shoreline, known as Reynisdrangar.

  According to local Icelandic folklore, these large basalt columns were once trolls trying to pull ships from the ocean to shore. However, these trolls were dim and went out too late in the night; dawn broke on the horizon, turning the trolls into solid stone.

  Another legend tells of a husband whose wife was kidnapped and killed by two trolls. The man followed the trolls down to Reynisfjara where he froze them, ensuring that they would never kill again.

  So mesmerizing are these features that they featured in Season 7 of the HBO Series Game of Thrones; you can spot them in a few scenes shot ‘North of the Wall’.

  The sea stacks themselves are home to thousands of nesting seabirds. Species that can be found here include puffins, fulmars and guillemots, making it a must-see location for all birdwatchers out there.

  Surrounding Sites

  

  Reynisfjara beach is located conveniently in the middle of the South Coast, adjacent to the village of Vík. This means that those taking the Ring Road around the country, or else those heading to the Jökulsárlón glacier lagoon, will pass it, and are encouraged to make a stop.

  The closest major landmark is the Dyrhólaey rock arch and cliffs. While many seabirds are found at Reynisfjara, it is nothing compared to the numbers here. From May to August, it is one of the best places to see puffins from land.

  En route to Reynisfjara from Reykjavík, you will discover waterfalls, such as Seljalandsfoss and Skógafoss, and glaciers, such as Eyjafjallajökull and Mýrdalsjökull. Further along the South Coast, you will reach the Vatnajökull National Park, with its many glacier tongues, glacier lagoons, black sand deserts, and the incredible Skaftafell Nature Reserve.

  Potential Dangers

  

  Visitors to Reynisfjara must be made well aware of the potential dangers present at the beach. First of all, the rolling, roaring waves of Reynisfjara are particularly violent, often pushing far further up the beach than many would expect.

  These are called sneaker-waves, and they can appear when least expected, even on incredibly still days. There are no significant landmasses in between Antarctica and the shores of Reynisfjara, meaning waves have thousands of kilometers to build.

  Visitors are advised to never turn their back on the waves, and keep a safe distance of at least 30 meters (98 feet).

  Aside from these sudden and dramatic shifts in the tide, the rip currents offshore are infamous for their strength and ability to drag helpless people out into the freezing cold open ocean. A number of fatal accidents have occurred at Reynisfjara, the last of which occurred in January 2017.

  Reynisfjara黑沙滩,

  

  Hellnar is an old fishing village on the westernmost part of the Snaefellsnes peninsula. It used to be one of the largest fishing stations of the peninsula, with the oldest written record of seafaring there from 1560.

  History of Hellnar

  Historically, the settlement was a hub of activity, with many trading and fishing vessels pulling in and out of the harbour daily. There were many farms around the area, and by 1703, 38 houses.

  Though by modern international standards this was nothing, it was rather significant for Iceland at the time.

  Throughout the nineteenth and twentieth centuries, however, Iceland began to develop and industrialise, and its fishing and trading industries began to move to Reyjavík, bringing with them many people.

  Hellnar, therefore, rapidly lost its population and importance, like many other places in Iceland particularly on the Snӕfellsnes Peninsula. The change in the economy hit Hellnar particularly hard, however, considering it was increasingly neglected for the neighbouring village of Arnarstapi, which was favoured by the ruling Danish.

  The settlement was abandoned but for a few farms and a few resilient locals, until tourism began to boom in Iceland. Now, it is a centre for visitors in the area, with many options for rural accommodation.

  Hellnar hosts the guesthouse for Snӕfellsnes National Park, which has a very interesting exhibition about the economy of former times, and on the geology, flora and fauna of the park.

  Sites near Hellnar

  At the shores of Hellnar are spectacular rock formations; much of the Snӕfellsnes Peninsula is incredibly dramatic along its coast, due to the previous volcanism of the area and the waves shattering the brittle lava rock that makes up the land.

  Most notable amongst these that can be reached on foot is a protruding cliff called Valasnös. It has tunnels into the cliff, and its colouration is affected by the time of the day, the movements of the sea, and the prevailing weather conditions.

  Large colonies of birds nest in the area, although it should be noted that puffins do not.

  Hellnar, located at the tip of the peninsula, is a convenient hub for those travelling in their own car, offering easy access to the incredible natural sites nearby. These include the Lóndrangar sea stacks, the mountain Kirkjufell, and the Ytri Tunga seal watching beach.

  Like many other places on Snӕfellsnes, it is easy to see the beautiful glacial capped volcano Snӕfellsjökull from the village.

  海勒那尔小镇,

  

  Reykholt is a tiny village in west Iceland, which was once home to one of the world’s greatest medieval writers. Packed with history and culture, this little settlement should not be overlooked

  Reykholt: Home of Snorri Sturluson

  Reyholt’s fame comes from the fact that it was the home of the legendary writer, historian, chieftain and lawspeaker Snorri Sturluson. Though his name is not well-known outside of the Nordic world, without him we would know much less about medieval northern European history than we do today.

  His two most famous works are Prose Edda and Heimskringla. The former is an account of the Old Norse Mythology, which was otherwise kept alive only by oral tradition.

  It tells about how the pagans thought the world was created and how it would end, and the deities that sparked fear and awe in them, most famously Odin, Thor and Loki. Considered an epic poem akin to Homer’s Odyssey to many, it has inspired the fantasy genre perhaps more than any other work in the world.

  Heimskringla is an account of Norwegian kings, told as sagas. It depicts what most historians consider to be an accurate depiction of relations across northern Europe from the 9th Century to the end of the 12th.

  It is through this work, therefore, that we can learn about how the Vikings related to the kings of places such as the not-yet United Kingdom, how the jarls and clans disputed, and how they formed governments that have lasted to this day.

  Though Snorri is best remembered for his works, his life was also a fascinating tale somewhat similar to that of a Game of Thrones character.

  Aside from being a beloved poet and writer, he was a chieftain and later lawspeaker for Icelandic parliament, as well as a spokesperson, agent and, to some, lackey of the Norwegian king.

  His influence and actions propelled Iceland’s civil war into chaos, and he met betrayal from every side, resulting in his eventual assassination. The taboo of this execution, however, meant that Snorri was remembered as a hero, rather than the divisive figure he often was.

  To add to the Game of Thrones flavour, he was also notorious for infidelity, and fathering children up and down the country.

  In honour of Snorri’s life and works, Reykholt is home to Snorrastofa, a centre on his contribution to medieval studies.

  Reykholt and Surroundings

  

  Even if you have little interest in Snorri, Reykholt is a beautiful town, well worth a visit. It has a wealth of geothermal activity, and one of the country's oldest structures, Snorralaug geothermal pool, can be found here.

  Reykholt is also the closest settlement to the popular waterfalls of Hraunfossar and Barnafoss. The former of these, the ‘Lava Falls’, are serene and unique, while the latter, the ‘Children’s Falls’, is rapid and dramatic.

  It is also close to Deildartunghver, the highest flowing hot spring in Europe.

  If you're looking to stay more than a day in Reykholt or nearby, there are several hotels in the vicinity, among them the the beautifully built boarding school that functions as an Edda-hotel in the summer. There are also a wealth of cabins and bungalows to be rented here.

   

  Reykholt,

  

  Barnafoss is a rapid waterfall in West Iceland, just a short walk away from the serene Hraunfossar falls. It is best known for its dark history in folklore, and for how much it contrasts with its neighbour.

  Folklore of Barnafoss

  Barnafoss translates to ‘the Children’s Falls’ because of a legend long told about it. Back in Iceland’s early days, it was said that a family with two boys lived at the nearby farm of Hraunsás. The parents left home for church one morning, ordering the young ones to remain at home, but with nothing to entertain them, the children soon decided to follow.

  They knew a shortcut to the church: a stone bridge, arching over the nearby rapid waterfall, that back then would have had a different name. They started to cross it, but found the heights and surging water below dizzying. In a tragic turn of events, neither boy made it across the bridge, and both fell to their deaths.

  Though both parents were grief-stricken, the mother veered towards insanity. Some versions of the tale end with her demanding the bridge be torn down. Others say she turned to witchcraft, placing a rune on the bridge that made any who crossed it plummet to their deaths just like her beloved sons.

  If the latter version is true, her spell was broken when an earthquake shattered the passage.

  While Iceland’s tales of magic were, of course, exaggerated as they were passed down in oral tradition, it is very possible that this story is true; Barnafoss would kill whoever fell into it in all likelihood, and many Icelanders scratched runes to spread curses to their neighbours and rivals.

  It is, of course, equally possible that like many Icelandic tales, it was simply created as a way to ensure that young children respected their parents, and feared the country’s unpredictable nature.

  

  Surroundings of Barnafoss

  Barnafoss is a magical site in and of itself, twisting, turning, foaming and churning as it races down a narrow valley, from which you can view it from above. It is even more fantastical, however, due to its contrast with Hraunfossar.

  Rather than being a narrow rapids, Hraunfossar is a wide series of trickling waterfalls, flowing from a plateau of lava rock. Seeing the drama of one, followed by the peace of the other, is an excellent example of how Iceland’s scenery is ever-changing, and completely different spectacles can exist within mere metres of each other.

  Other sites of the west near Barnafoss include the highest-flowing hot spring in Europe, Deildartunguhver, which is fascinating to admire but impossible to bathe in due to its extreme heat.

  There are also the settlements of Reykholt and Borgarnes, both of which should be visited by those passionate about Icelandic history and culture. Reykholt hosts the Snorrastofa Exhibition, where you can learn about the village’s most famous resident, Snorri Sturluson. Snorri wrote many of the Icelandic texts that reveal huge amounts about Nordic kings, Norse mythology, and Icelandic folklore.

  Borgarnes, meanwhile, has the Settlement Centre, where guests can learn about the brave first arrivals to this stark new home, and one of the country’s most famous sagas, Egil’s Saga.

  儿童瀑布群,

  The mighty Langjökull, the ‘Long Glacier’, is the second-largest glacier in Iceland, at 935 square kilometres (361 square miles). For jeep and snowmobile trips, Langjökull is the most popular glacier in Iceland, and skiing and hiking here is possible as well.

  Highland tracks

  

  Langjökull is located in the Highlands, and two main highland tracks, connecting the north and the south of Iceland, lie alongside it.

  The Kaldidalur road stretches from Þingvellir National Park northwards to Húsafell. The Kjalvegur road, meanwhile lies east of Langjökull and west of Hofsjökull glacier, starting near the famous Gullfoss waterfall to the south, and passing through the beautiful Hveravellir geothermal area to the north.

  The landscape of Langjokull

  Langjökull is about 50 kilometres (31 miles) long and up to 20 kilometres (12 miles) wide, and the ice is around 580 metres (1,903 feet) deep at its thickest. The glacier reaches its highest point in its northernmost part, which is called Baldjökull, rising around 1,450 metres (4,757 feet) above sea level.

  The glacier lies over a massif of hyaloclastite mountains. The tops of these mountains can be seen in certain places on the glacier. It also conceals at least two active volcanic systems, the calderas of which are visible from the air.

  The best known of these systems fuels the geothermal area of Hveravellir, east of Baldjökull. Also in the east lies the Kjalhraun lava field, which formed about 7800 years ago.

  To the northwest of the glacier is another system that produced the vast Hallmundarhraun lava field, through which the Hvítá river runs in the direction of Gullfoss waterfall. Also in the area is Iceland‘s longest lava cave, the fascinating Surtshellir.

  Southwest of Langjökull is the Presthnúkur lava field, fissures of which creep under the ice. South of the glacier is the Lambahraun lava field and even further south lies the Skjaldbreiðarhraun lava field and the Skjaldbreiður shield volcano.

  Compared to other regions in Iceland, the area is considered relatively calm, with only 32 eruptions in the last 10,000 years.

  Into the glacier

  Near the highest peaks of Langjökull exists a man-made ice tunnel, a true spectacle for any visitor passing by the glacier. Designed and constructed by geophysicist and presidential candidate Ari Trausti Guðmundsson, the tunnel exists to allow visitors to explore the inside of a glacier without having to come to Iceland in mid-winter for a chance to see the less-than-reliable ice caves.

  Guests traverse beneath Langjökull's thick ice sheet, experiencing the vivid blue colouration within, and gaining an insight into the glacier's beauty, formation and processes. It is the only place in the world where this is possible. ‘Into the Glacier’ tours are often combined with adventure activities such as snowmobiling.

  Nearby glaciers

  The glaciers located nearest to Langjökull are Eiríksjökull, which conceals the highest mountain in west Iceland, and Þórisjökull. Hrútfellsjökull also lies on the east side of Langjökull.

  Between Þórisjökull and Geitlandsjökull is a valley called Þórisdalur. Along with stunning views, it features prominently in Icelandic folk tales; the outlaw Grettir the Strong of Grettis Saga, for example, is reported to have resided here for one winter.

  Langjokull and the Golden Circle

  

  Iceland’s most popular sightseeing route, the Golden Circle, would not be possible if not for Langjökull glacier; none of its three iconic features would exist in their current state without the melting ice.

  Gullfoss waterfall is the most obvious example of this. The river that feeds into it, the Hvítá, is a glacier river flowing straight from Langjökull; the scale of the ice cap is hinted at by the sheer volume of water that cascades here every second.

  The hot springs at Geysir, meanwhile, are supplied with water underground. Meltwater from Langjökull feeds into the surrounding lava fields, which have very porous rock, and flows in a subterranean river to the geothermal area, where it comes bursting out of the naturally forms vents.

  While Þingvellir would still have its National Park and World Heritage status without Langjökull, which it received for being the original site of what is now the longest-running representative parliament in the world, it would be notably less beautiful.

  Many springs exist throughout the park, also formed by the underground meltwater of the glacier. Due to its long filtration process, the water emerges as some of the clearest naturally occurring water in the world.

  Silfra fissure, therefore, is the best snorkelling and diving location in the country and consistently ranked as one of the top ten places for such activities in the world.

  Global warming

  Langjökull is shrinking fast and concerns have been raised about the glacier due to the effect of global warming. Some researchers fear that if climate change continues at its current rate the glacier may be gone in 150 years. Less optimistic scientists have said it could be gone in as few as 50.

  朗格冰川,

  Wikimedia, Creative Commons, Photo Credit: Geri340

  Gerðuberg is a row of perfectly shaped hexagonal basalt columns that run along a cliff on the southern side of the Snӕfellsnes Peninsula, in west Iceland.

  Geology of Gerðuberg

  The cliff on which the Gerðuberg columns reside is over a kilometre long, with columns between seven and 14 metres (23 to 46 feet) tall and up to one and half metres (five feet) wide. Many have compared the feature to a fortress wall.

  The most unusual thing about Gerðuberg is how the columns are so geometrically symmetrical that they seem to be carved by hand. Such features are rare around Iceland and the rest of the world, but easily explained by science.

  During an eruption thousands of years ago, rivers of lava ran off the cliffs here, in very equal flows. The sea rapidly cooled them, causing them to take this unique and unusual shape.

  Other places in Iceland that they can be found include Hofsós, in north Iceland, and from the river Hvíta on a rafting tour.

  The Snӕfellsnes Peninsula is defined by a long range of volcanoes, with the Snӕfellsjökull glacier volcano being the most renowned. Lava flows like those that cause Gerðuberg have not occurred in the area for hundreds of years.

  Getting to Gerðuberg

  Gerðberg is usually the first major site visitors to the Snӕfellsnes Peninsula see as they as they approach it from Reykjavík, and travel along its southern side (excluding the Eldborg crater, which is a little inland). The cliffs with these strange columns runs adjacent to the road and sea, making them impossible to avoid.

  While a marvellous feature to see, they are just one of many on the peninsula. Travelling clockwise from Gerðuberg, guests will get to marvel over the Ytri Tunga seal-watching beach; Rauðsfeldja gorge; the Lóndrangar sea-stacks; Snӕfellsjökull National Park; and Mount Kirkjufell, to say nothing of the many fishing villages, swimming pools and cultural sites along the way.

   

  Gerðuberg,

  

  Arnarstapi is a village on the southern side of the Snæfellsnes peninsula, once a fishing hub and now a place for travellers to refuel before entering Snæfellsjökull National Park. The area has several old and charming houses with interesting stories to them and is renowned for its beautiful nature.

  History of Arnarstapi

  Records of settlements around Arnarstapi date back to the Bárðar saga Snæfellsáss, an ancient Icelandic Saga that tells of the half-human, half-ogre who once lived on the Snæfellsnes peninsula. Since his death, he has been considered the area's guardian spirit.

  The region was popular with settlers due to its natural harbour, meaning fishing in the rich herring grounds of the surrounding waters was easy. When Norway, and to a much greater extent when they took over, Denmark, were in control of Iceland, Arnarstapi grew increasingly as a trading port.

  Denmark invested a lot of money into Arnarstapi throughout the eighteenth and nineteenth centuries (for their own interests, unfortunately not those of the Icelanders). Many of the resulting buildings still stand today, being some of the oldest in the country, such as the Danish Prefect’s Residence, which was built in the 1770s.

  In the industrial revolution, Arnarstapi’s population radically shrunk which was common in the countryside at this time. The vast majority of Iceland’s jobs were now centralised in Reykjavík, reducing opportunities for small-time fishermen and their businesses, and the town became little more than a hamlet as a result.

  As Iceland’s infrastructure rapidly improved after independence in 1943, and more people abroad began to see the many wonders of this island as a travel destination; Arnarstapi, like many other settlements in the area, got a new lease on life.

  Fishing and trade remain vital parts of the economy, but they now play second fiddle to tourism and services. The village has essential services for those travelling on the peninsula, a wide array of accommodation options, and tour companies operating from it.

  Nature and Sites around Arnarstapi

  

  The beach at Arnarstapi holds a particular attraction. It has an eroded circular stone arch, called Gatklettur, and here, the interplay of spectacular waves and the light of the sun create a fascinating spectacle. Large colonies of the arctic tern also nest in the area, and both these features make it very popular amongst photographers.

  An old horse trail through the lava field Hellnahraun is highly popular for hiking, due to the impressiveness of the surrounding landscape.

  Arnarstapi, however, should never be too long a stop on a tour of the peninsula. As lovely as it is, the natural attractions nearby simply warrant more time. The village, for example, sits on the cusp of Snæfellsjökull National Park, home to the Snæfellsjökull glacier and volcano, the beauty of which has inspired writers and artists for centuries.

  This is one of only three National Parks in the country, but it is to the credit of the peninsula’s beauty that it is far from the only must-see destination around. Very close to Arnarstapi is the Lóndrangar basalt cliffs, huge towers of lava that from a distance look like a fortress.

  Vatnshellir and Sönghellir and two nearby lava caves (the former of which can only be entered on a guided tour). There is also a beautiful cleft in a mountainside called Rauðfeldsgjá Gorge that it is possible to climb into.

  Though a little further away, on the north of the peninsula, Kirkjufell mountain is also a wonderful site to behold.

  阿尔纳斯塔皮,

  

  Vík í Mýdral, or just Vík, is the southernmost village on the Icelandic mainland, located 186 kilometres (110 miles) from the capital Reykjavík.

  Often visited by those travelling the popular sightseeing route along the South Coast, it is a wonderful place to stop, recharge, and if you are taking your time, rest for the night. Though it only has around 300 residents, the village is very popular amongst tourists for its convenience and beautiful surrounding landscapes.

  Features near Vik

  Reaching Vík from Reykjavík takes approximately two and a half hours, and en route, there are many marvellous features to admire. Two of the country’s most famous waterfalls, Skógafoss and Seljalandsfoss, lay between the two destinations; the former has awe-inspiring power, whereas the latter can be fully encircled.

  The glaciers Eyjafjallajökull and Mýrdalsjökull can also be seen on clear days; both of these cover volcanoes which are particularly explosive, with Eyjafjallajökull famously disrupting European air travel in 2010. Out to sea in especially good weather, the Westman Islands can also be seen on the horizon.

  Just before Vík are the popular birdwatching cliffs of Dyrhólaey, where you can also find an enormous rock arch curving out into the ocean. This is one of the best places for birdwatching in Iceland, with thousands of puffins nesting here from May to August.

  The village itself sits opposite one of the country’s most famous features: Reynisfjara black sand beach. Considered one of the world’s most beautiful non-tropical beaches, it boasts incredible geology.

  

  Particularly of note are the Reynisdrangar sea-stacks, said to be two trolls frozen in the light of the morning sun as they tried to pull a ship into shore.

  Though this beach makes for a lovely walk, particularly for those staying in Vík overnight, as they can see it under the midnight sun or northern lights, it has its dangers. Sneaker waves can be notorious here, so visitors should stay far from the water’s edge, and never go for a swim. Lives have been lost here before.

  The route to Vík from Reykjavík is beautiful and continues to be so as you travel further along the South Coast, through the Skeiðarásandur black-sand-plains into Vatnajökull National Park. This beautiful region is often the final destination of those passing through Vík, as it is home to the largest glacier in Europe, the Skaftafell Nature Reserve, and Jökulsárlón Glacier Lagoon.

  Of course, ambitious travellers will carry on from here to encircle the full country.

  Wildlife around Vik

  Vík, due to its closeness to the Reynisfjall and Dyrhólaey cliffs, has a rich birdlife. Short walks from the village will take you to the nesting grounds of gulls, fulmar, guillemots, and in summer, puffins.

  Due to its coastal location, visitors to Vík have a decent chance to see seals on the shore. There is also a slim chance to see whales or dolphins; the twenty or so species that live in Iceland’s waters can appear at any time.

  Services in Vik

  Vík has a wide variety of public services, due to its remoteness and its importance in connecting the east and west of Iceland. There are gas stations, shops and cafes, a swimming pool, a wool factory that can be visited, and a wide range of accommodation options for all budgets.

  Please note, however, that as the village has such a small year-round population, those with special dietary requirements should purchase their food from Reykjavík before departing.

  维克镇,

  

  Gljúfrabúi (or Canyon Dweller) is a beautiful waterfall located at Hamragarðar in South Iceland, close to its better known counterpart, Seljalandsfoss waterfall. It is one of the hidden gems of the South Coast, and thus a great spot for photographers and those seeking to admire nature in peace.

  ---

  Image from Regína Hrönn Ragnarsdóttir

  ---

  Nature of Gljúfrabúi

  The 40 metre (131 feet) high Gljúfrabúi is hidden behind a huge cliff which faces out towards Iceland’s South Coast and the Atlantic Ocean. Because of its decent ‘hiding place’, it is overlooked by most travellers, in spite of the fact that thousands of people visit Seljalandsfoss, less than a kilometre away, every day.

  A stream, the Gljúfurá, runs through a cleft in the cliff, and those who wish to approach the falls must do so by wading through these waters.

  After a few metres of travelling through a narrow valley, the space will open, and here, Gljúfrabúi tumbles before a great boulder, which it is possible to climb upon for some great photos. With the open sky above, mossy walls, silver mist and black lava, it is one of Iceland’s most breathtaking gems, seemingly from a fantasy story.

  This is especially the case on sunny days, where rainbows curve through the water’s spray.

  It is also possible to see Gljúfrabúi from above. There is a steep path that allows you to clamber up the cliff, at some points with the aid of ropes.

  Both these routes are mildly challenging and have their dangers, so only attempt to reach Gljúfrabúi if you are in a decent state of health and confident on your feet. They should only be attempted when there is not ice on the ground, and in the case of the path up the cliff, when it is wet and slippery.

  Surroundings of Gljúfrabúi

  

  Gljúfrabúi is in one of the most travelled regions of Iceland, on the South Coast along the Ring Road. This means that it is very easy to reach, either alone or on a guided tour, just an hour and a half’s drive from the capital.

  As mentioned, Gljúfrabúi is about ten minutes walk north Seljalandsfoss. Interestingly, this is one of the country’s most famous and photographed waterfalls, due to the fact it falls from a concave cliff which allows visitors to fully encircle the cascade.

  Seljalandsfoss is taller than Gljúfrabúi at 60 metres (196 metres), with a similar waterflow. Both are fed by the meltwater of the glacier Eyjafjallajökull, the volcano beneath which caused widespread problems to air traffic across Europe when it erupted in 2010.

  A much more powerful waterfall can be found just half hour’s drive or so along the Ring Road, called Skógafoss. This is a similar height to Seljalandsfoss, but up to 30 metres (98 feet) wide after a heavy rain.

  Another popular site in the area is Sólheimajökull, the most popular glacial outlet in Iceland for glacier hiking. This feature is on Sólheimasandur, a vast expanse of volcanic ash that resembles a black sand desert.

  Those who travelling a little further along the South Coast will reach the cliffs of Dyrhólaey, with their beautiful rock arch and resident puffins in summer, and the beach of Reynisfjara, renowned for it powerful waves and basalt sea-stacks, called Reynisdrangar.

  All these sites can be visited with ease within a day.

   

  Gljufrabui,

   

  

  Reykjavík Airport refers to the predominantly domestic airport within Iceland’s capital, often shortened to RVK or BIRK.

  While Keflavík International Airport deals with flights abroad, planes from Reykjavík Domestic Airport only fly to select towns around Iceland, as well as to the Faroe Islands and Greenland. It will, however, serve as a landing place for international flights if conditions are problematic at Keflavík.

  History of Reykjavík Airport

  Flights had been going in and out of Reykjavík to an extent before 1940, but this was the year when construction began at the airport.

  It was built by the British Troops who invaded the country after Denmark (the colonial ruler of Iceland at the time) was invaded by the Nazis. Initially, it was called RAF Reykjavík but received its current name when it was handed back to Icelanders in 1946.

  In 2000, the airport underwent two years of renovation. During this time, there was a successful referendum in which the people spoke in favour of moving the airport out of the city centre, but due to complications in voting and the fact that the vote was not binding, these plans are yet to move forward.

  The renovations were finished in 2002, and the airport has not changed much since, other than becoming much busier with the dramatic increase of tourism.

  Reykjavík Airport Today

  

  Today, Reykjavík Airport has four airlines that operate from it. They head to the following destinations in Iceland:

  • Akureyri

  • Egilsstaðir

  • Húsavík

  • Ísafjörður

  • The Westman Islands

  • Bíldudalur

  • Gjögur

  This means that guests who are pressured for time, fearful of driving on the icy roads, or have come in the depths of winter and roads are closed, can still reach all corners of the country.

  Flights also go to Nuuk, Kulusuk and Ilulissat in Greenland, and Vágar in the Faroe Islands.

  Very occasionally, flights will go back and forth to Copenhagen.

  The airport is also regularly visited by tourists staying in Reykjavík, however, as it is the departure location for many helicopters and small plane excursions, which allow guests to have incredible aerial views of Iceland.

  Some of these tours take guests as far out as to remote parts of the Highlands, while others are short flightseeing trips around the greater Reykjavík area. These, however, are still exhilarating and rewarding; there is no better way to see Reykjavík than from above, witnessing the patchwork quilt of colourful tin roofs unfold beneath you, and landmarks such as Hallgrímskirkja church from a whole new angle.

  It also provides a great chance to see the nature around Reykjavík. In clear weather, you will be able to see the Snæfellsnes and Reykjanes Peninsulas, the flat-topped mountain Esjan, the bay of Faxaflói and the Bláfjöll Mountain Range.

  The airport is located about two kilometres from Reykjavík’s city centre, putting it within easy walking, bus or taxi distance from all downtown hotels. It is right beside the forested hill Öskuhlíð, home to the popular restaurant, viewing point and exhibition centre, Perlan.

   

  Reykjavík Airport,

  

  Keflavík International Airport (KEF) is Iceland’s only international airport and the port of arrival for the vast majority of visitors to the country. In 2016 alone, almost seven million passengers went through its gates.

  The History of Keflavík International Airport

  Keflavík International Airport is a relic from the ‘invasion of Iceland’ in World War II, when Allied troops took over the island nation following the defeat of its colonial ruler, Denmark, at the hands of the Nazis.

  The British laid out a landing strip in the town of Garður, but considering Iceland’s incredibly strategic position in the middle of the Atlantic Ocean, one strip was not quite enough.

  After taking control of the ‘occupation’, US troops constructed and opened two airfields for military purposes in 1942 and 1943. Though they returned the property after the war, the United States reclaimed it in 1951 after a controversial defence alliance with Iceland.

  This pact, and the general joining of NATO in 1949, caused decades of national protest, comparable to the ‘Women’s Day Off’ marches in 1975 and the ‘Kitchenware Revolution’ which followed the 2008 economic crash. The circumstances of it, however, also allowed decades of development at Keflavík Airport.

  The airport first started to separate civilian and military use in 1987, with the opening of the Leifur Eríksson Terminal. Named after the first European to settle the Americas, it would go on to handle all the guests coming to or leaving Iceland.

  The arrangement that the US would provide Iceland’s defences continues to this day, but their permanent bases at Keflavík were left at the expiration of the treaty in 2006. The airport was thus moved into full control of Icelanders and has expanded as a civilian hub ever since.

  Keflavik International Airport Today

  

  Keflavík International is located on the tip of the Reykjanes Peninsula, Iceland’s south-westernmost region. The drive to the capital city of Reykjavík is only about forty-five minutes, and there is a bus service that continuously runs between the locations, day and night.

  This service provides guests with the option to stop at the Blue Lagoon en route in either direction, the iconic health spa renowned for its healing azure waters. The lagoon sits between the airport and the capital, refreshing guests after a long flight, or revitalising them in preparation for one.

  The airport itself has all the modern amenities one would expect from a port that experiences so much traffic. It has restaurants, bars and cafés, banks and money transfers, car rental options available, a smoking area and, of course, many options for duty-free shopping.

  Considering the price of and lack of availability of alcohol in Iceland, it is the best place to stock up on any tipple desired for your trip. Otherwise, you will have to locate specialist alcohol shops, which have limited opening hours, are sparse in the remote regions of the country, and have high taxes and duty.

  The main airlines that arrive at and depart from Keflavík are the two national carriers, the prestigious Icelandair and budget airline WOW. Over thirty different carriers have chartered flights to the port, however, which head to over ninety different destinations. This is only ever increasing, with new travel routes emerging as Iceland’s popularity continues to skyrocket.

   

  Keflavik International Airport,

  

  Kirkjufell, or 'Church Mountain', is a distinctly shaped peak found on the north shore of Iceland’s Snæfellsnes Peninsula, only a short distance away from the town of Grundarfjörður. It is often called ‘the most photographed mountain in Iceland’, due to its dramatic formation and perfect coastal location.

  Kirkjufell takes its name from its resemblance to a church steeple, sharpened at the top with long curved sides. From other angles, the mountain has been compared to a witch’s hat or even a freshly scooped ice cream.

  Photography at Kirkjufell & Kirkjufellsfoss Waterfall

  Peaking at 463 metres, 1519 feet, Kirkjufell is an impressive landmark. Throughout the centuries, Kirkjufell’s striking slopes have acted as a visual landmark for seafarers and travellers. More recently, it has attracted amateur and professional photographers alike.

  Within walking distance from Kirkjufell is the serene and perfectly located waterfall Kirkjufellsfoss, or 'Church Mountain Falls', an excellent subject for photographers who can easily frame the mountain in the background. Despite its relatively diminutive height, Kirkjufellsfoss’ three-steps, gentle flow, and dramatic differences between seasons make it as impressive as some of Iceland’s larger waterfalls.

  

  At the base of the mountain, visitors will also be able to find a lake; on calm and clear days, this lake reflects a perfect mirror image of Kirkjufell, only adding to the fantastic photo opportunities around this area.

  On top of that, the colours of Kirkjufell change with the passing seasons; the summer sees it a lush green, full of life, whilst the winter months scar the mountain’s face with a mask of barren brown and white. Of course, it is more impressive under the midnight sun in the weeks surrounding the June equinox, and under the northern lights, best seen between September and April.

  Fans of the HBO series Game of Thrones will recognise Kirkjufell as a shooting location from Season 7 of Game of Thrones. The mountain is showcased from the scenes ‘North beyond the Wall’ when Jon Snow, The Hound and Jorah Mormont, amongst others, brave the wilderness in hopes of catching an undead wight.

  Having seen it in a vision, The Hound acknowledges Kirkjufell as “[...] the mountain like an arrowhead”, and the events that happen beneath it are some of the show’s most dramatic.

  Hiking Kirkjufell

  There is a fairly steep trail to the top of Kirkjufell, from where there are magnificent panoramas of the surrounding fields, coastlines and rivers. The mountain takes roughly an hour and a half to ascend, with another one and a half hours needed to get back to the bottom.

  Given the steep elevation and treacherous trail, you should only hike Kirkjufell if you are a very experienced and confident mountain climber, preferably in the company of an expert guide. Sadly, there have been three fatal accidents on the mountain, most recently in 2018.

  Getting to Kirkjufell

  Kirkjufell is extremely close to Grundarfjörður, a small town on the Snæfellsnes Peninsula, which is just over two hours drive from Iceland's capital city, Reykjavík. From Grundarfjörður, one travels a few minutes west down Route Snaefellsnesvegur 54 to the base of Kirkjufell. Visitors have plenty of parking space to choose from, all free of charge.

  教会山(草帽山),

  

  Reynisdrangar are impressive rock formations situated near the shore of Reynisfjara beach by the coastal village Vík on the South Coast of Iceland.

  The formations are the remains of large and imposing sea cliffs, made up of basalt, that serve as a vital part of the area’s allure; they shoot dramatically out of the ocean under the looming cliffs of Mt. Reynisfjall, making for a beautiful site, and have a folklore that is equally impressive.

  More modern visitors will be excited to know that these pillars also feature in Season 7 of Game of Thrones, at Eastwatch by the Sea.

  Dangerous Waves

  

  Before getting into the wonders of Reynisdrangar, it is important for potential visitors to be aware of the dangers at the site.

  These majestic rock pillars rise from the sea just off of Reynisfjara, a famous black sand beach on the South Coast, by the village of  Vík. Though incredible due to its diverse and dramatic geology, Reynisfjara is gaining a notorious reputation for its sneaker waves.

  There are no significant landmasses between Antarctica and Reynisfjara, giving waves the entire length of the Atlantic Ocean to build strength. This means that even on still, summer days, they can rise from seemingly nowhere and chase far further up the sand than would ever be expected.

  It is absolutely imperative, therefore, that guests stay at least 30 metres (98 feet) from the water’s edge. Those who flout these rules put their lives and the lives of others at risk; people have died here before.

  Folklore

  

  As with almost all bizarre features in this country, there is an Icelandic folk tale that explains the origin of the Reynisdrangar pillars and their eerie appearance.

  According to legend, a couple of trolls saw a ship out to sea by night, and waded out to reach it. They got hold of it, and began to drag it to shore, but as so often happens in troll stories, they got their timing wrong.

  Before they were even close to getting to the shade, dawn broke. The trolls and ship were instantly frozen into stone, and they have remained immortalised since, as a warning to their kin.

  This is not the only folk tale in this area. According to local legend, two other trolls murdered a woman, whose husband hunted them down, tricked them into coming out at night, and ensured they too were turned to stone. Their remains can be found inland.

  Surroundings & Wildlife

  Most visitors will only see the Reynisfjara sea-stacks from the shore of Reynisfjara, although there is an incredibly rewarding alternative view of them from above. Those with a reasonable level of fitness can venture up the bewitching cliffs of Mt. Reynisfjall, by a road to the west of Vík.

  The mountain furthermore holds thousands of puffins every summer, from May to August. These adorable creatures have very little fear of people, and can be approached within metres (although you should never try to touch them). Other birds can be seen gliding around the cliffs such as Arctic terns, fulmars and seagulls.

  The oceans of Iceland are pregnant with life, so lucky visitors may also see seals in the water, or even one of Iceland’s twenty species of whale and dolphin.

  Reynisdrangar石柱群,

  

  Haukadalur is a geothermal valley in South Iceland on the popular Golden Circle route. 

  Lying to the north of Lake Laugarvatn, it is home to hot springs, fumaroles, mud pots and geysers, including the famous Great Geysir and the active Strokkur. The area is noted for the vivid colouration of its surrounding hills, caused by elements deep in the earth being brought to the surface by the geothermal activity.

  History of Haukadalur

  Haukadalur has been mentioned in historic writings as far back as 1294, in which its geysers were described following an earthquake that activated them. Since the 18th Century, it has been drawing visitors to the island including two different Kings of Denmark in 1907 and 1922.

  Throughout the 20th Century, images of the Great Geysir erupting at Haukadular began to symbolise Iceland. It’s activity, however, was unreliable, so unnatural efforts were made to stimulate it more regularly, such as lowering the water table in 1935 and pumping soap into it 1981. 

  These, however, limited the geyser’s long-term activity, so that it rarely goes off today, although, in the early 2000s, it did have a period where it was spouting water over 140 metres (459 ft) high. Even so, the geyser Strokkur is still very active, erupting to heights of 30 metres (98 ft) every five to ten minutes.

  Today, most of the near-two million visitors to Iceland will see Haukadalur Valley on their travels.

  Surroundings of Haukadalur

  Haukadalur Valley is located about an hour and a half’s drive inland from Reykjavík, thus making many sites of the South and West easily accessible. The most notable of these are the other points on the Golden Circle: Gullfoss Waterfall (about five minutes away) and Þingvellir National Park (about forty minutes away).

  It is also, however, within an easy driving distance of Flúðir, home of the Secret Lagoon, the Kjölur Highland Road, which leads into Iceland’s interior, Sólheimar eco-village, and Faxi Waterfall.

   

  Haukadalur,

   

  Photo by Regína Hrönn Ragnarsdóttir.

  Eldborg is a crater on the base of the Snæfellsnes Peninsula that it is possible to hike to the top of and around. It is 60 metres (197 feet) tall.

  Formation of Eldborg

  Eldborg is located on a short volcanic rift, just 200 metres (656 feet) in diameter, and 50 metres (164 feet) deep. It is the largest crater on this rift, and was created in an eruption which occurred somewhere between 5000 and 6000 years ago. Unlike many of Iceland’s volcanoes, it has a very classic shape, with smooth sloping sides and a very definite crater.

  Elborg is a spatter cone. This means that it erupted explosively, hurtling highly viscous lava into the air that would land back onto the crater in a semi-solid, ‘taffy’-like state. This would ooze down the sides of the crater, welding thick blobs of rock together to provide a unique appearance.

  Like most other spatter cones, the sides of the Elborg crater are wall-like, although the feature is much larger than most of its other counterparts around the world. Of the five craters in this area, it is by far the greatest.

  Ravens are often seen nesting inside the pockets of lava in the walls of the crater.

  Hiking at Elborg

  Photo by Regína Hrönn Ragnarsdóttir.

  Elborg is situated in a large plain of lava, being the only prominent feature rises from it for several miles. It requires a 2.5 kilometre (1.5 mile) hike to reach, and is most accessible in summer, when the path is clear of snow.

  This hike is largely across flat ground, although unpaved. The path up to the top is rather steep, but chains are on site to help those who are losing energy.

  To reach Eldborg from Reykjavík is easy. Guests simply have to take Route 1 North, passing through the Hvalfjörður Tunnel, before turning left onto Route 54 at the town of Borgarnes. Turn right at Route 55, and the crater will be clearly visible.

  This journey takes about two hours, but puts you right on the edge of the Snæfellsnes Peninsula, making it easy to visit other incredible sites such as Rauðfeldsgjá Gorge, the Lóndrangar sea stacks, Kirkjufell Mountain, and Snæfellsjökull glacier and National Park.

  Eldborg,

  Photo from Into the Underworld | Vatnshellir Caving Tour

  Vatnshellir Cave is a lava tube on the Snæfellsnes Peninsula and a popular site for caving tours.

  Geology of Vatnshellir Cave

  Vatnshellir is one of Iceland’s older lava tubes that can be explored, having been formed in an eruption 8,000 years ago. To compare, Iceland’s other most popular lava tunnels for caving, Viðgelmir and Leiðarendi, are only one and two thousand years old respectively.

  Like all lava tubes in Iceland, Vatnshellir was created when during an eruption, a river of molten rock began to cool from outside in. The effect left a crust over still-flowing lava, which, after flushing away, left a hollow tube.

  The minerals of this lava can still be seen in Vatnshellir today. The rocks are vividly coloured, with reds representing deposits of iron, yellows representing sulphur, and greens representing copper.

  Vatnshellir is 200 metres (656 feet) long, with a deepest point of 35 metres (114 feet).

  Lava Caving in Vatnshellir

  Lava caving is possible in Vatnshellir throughout the summer months with a guided tour. Taking such a tour is essential, as guides know the caves in and out, and will bring all the equipment you need. Alone, they are notoriously easy to get lost and hurt in.

  Vatnshellir is easier to enter than its cousin Leiðarendi, as it has a staircase descending into it. Unlike Viðgelmir, however, the ground is not paved and the walls are not lit, so you need a reasonable level of fitness and confidence on your feet to traverse it comfortably. Even so, children as young as five can join the fun.

  When travelling the cave, you will learn about Iceland’s geology and folklore, as trolls were said to make the caves their homes in many tales. You will also get to experience total darkness by shutting off your lights at the deepest point.

  Location of Vatnshellir cave

  Vatnshellir is a protected site, as it is within the Snæfellsjökull National Park. This park sits right on the tip of the Snӕfellsnes Peninsula, meaning you can include many nearby sites in a visit to it.

  These include the basalt sea stacks of Lóndrangar, the fishing villages of Arnarstapi and Hellnar, and the pyramid-shaped peak Kirkjufell.

  Vatnshellir火山洞穴,

  

  The Lóndrangar basalt cliffs are amongst the many geological wonders of the Snæfellnes peninsula.

  Geology of Lóndrangar

  Once a volcanic crater, all that remains after aeons of ocean battering are two great pillars upon a cliff, one 75 metres (246 ft) high and the other 61 metres (200 ft).

  Their dramatic scale has earned this incredible formation the nickname ‘the rocky castle.’

  The cliffs can be accessed easily from the Visitor’s Centre, through fields of mossy lava, but they can also be seen from the sea. Surfing is relatively popular in the area and doing so in the shadows of these great peaks only adds to the experience.

  Folklore of Lóndrangar

  The surrounding lands are steeped in folklore; farmers have never made use of the fields around the Lóndrangar basalt cliffs due to the elves that are rumoured to live there.

  Nearby, at Þúfubjarg, another cliff on the Snӕfellsnes Peninsula, it was said that the poet Kolbeinn Jöklaskáld met the devil and struck a deal with him.

  Lóndrangar,

  

  Djúpalónssandur is an arched-shaped bay of dark cliffs and black sand, located on the Snæfellsnes Peninsula in western Iceland. 

  History & Monuments 

  The location was once home to a prosperous fishing village, similar to other abandoned hamlets and ports of the area such as Búðir and Hellnar. These thrived back when the Snæfellsnes Peninsula functioned as one of the most active trading posts of the island, but now are simply centres for tourism.

  Fascinating remnants of this period are found in the form of four ancient lifting stones that still occupy the beach. The stones range in weight from 23 kg (50 lbs) to 155 kg (342 lbs) and were used to test the strength of fishermen. Their names are Amlóði (useless), Hálfdrættingur (weakling), Hálfsterkur (half-strong) and Fullsterkur (full-strong). Even today, you can see how you would have fared working on Iceland's dangerous seas by trying your luck at lifting these stones.

  In 1948, the English trawler Epine GY 7 from Grimsby shipwrecked on the shore, with fourteen dead and five survivors. The rusty iron remains of the vessel remain scattered on the beach, now protected as a monument to those who perished. 

  Environment & Surroundings

  The Snæfellsnes Peninsula boasts countless natural wonders, where locals and travellers both flock on a daily basis to enjoy the unique landscape and stunning coastlines. Djúpalónssandur’s black pebble beach is particularly stunning with its rocky coastal lava formations, which include a large lava rock with a hole in the middle through which you can directly spot the Snæfellsjökull glacier volcano. 

  Behind the rocks are two freshwater lagoons called Djúpulón and Svörtulón, with the former serving as the namesake of the bay. Though believed in olden times to be bottomless, the water bodies were later revealed to reach the depth of just five metres.

  Lagoons such as these are held in high regard amongst the Icelandic people, and Svörtulón is thought to possess healing properties, especially after having been blessed by Bishop Guðmundur góði ('the good') in the late 1100s. 

  A natural monument of the area is Söngklettur, or “singing rock”, a large lava rock with a reddish hue that resembles an elfish church. Other rock formations of folklorish appeal rest close by, including the alleged trolls-turned-to-stone Kerling and Lóndrangar. 

  Warning

  When visiting Djúpalónssandur, take heed that these are treacherous waters and the Atlantic Ocean’s powerful suction can easily carry you out to sea. This beach is not one for wading, but enjoying from a safe distance, especially if the weather is stormy. 

  The video below shows the power and shocking speed of sneaker waves that occur at locations such as Djúpalónssandur and Reynisfjara in the south.

  The glistening pebbles that make up the beach known as Djúpalónsperlur, or “pearls of the deep lagoon”, are gorgeous to look at and might seem appealing to stone collectors, but they are protected by law and should not be removed from the area by visitors.

  Djúpalónssandur黑沙滩,

  

  The South Coast of Iceland is the country's most visited sightseeing route, along with the Golden Circle.

  This incredible shoreline stretches from the greater Reykjavík area in the west to the magnificent Jökulsárlón glacier lagoon in the east and is lined with countless natural wonders such as cascading waterfalls, volcanoes, black sand beaches and glaciers.

  Geography, Nature & Wildlife

  The South Coast is the most easily accessible part of the country’s southern region, found along the Route 1 highway (the Ring Road), which encircles Iceland. The area consists of a diverse lowland that transitions between, marshlands, bays, cultivated pastures, estuaries and black sand deserts.

  Underneath the soil rests a vast lava field, known as Þjórsárhraun. Its edges reach several hundred metres offshore where the ocean waves crash upon them, thereby protecting the lowland from the invasion of the sea. This results in the South Coast being unusually lacking in the deep fjords that so distinctly characterise the rest of Iceland's shoreline.

  

  The region boasts vibrant bird life during all seasons. Freshwater birds nest in the marshlands and around the estuaries, while seabirds flock around the cliffs of Reynisdrangar and Dyrhólaey, including the North Atlantic puffin between May and August. Some species stay throughout the harsh Icelandic winter, including the northern diver, the loom and various species of gulls and ducks.  

  Seals are often found along the shore, particularly around the Jökulsárlón Glacier Lagoon and Diamond Beach. As with everywhere in Iceland, you should always keep an eye out to sea, as whales and dolphins reside all along its coastline.

  Highlights of the South Coast

  The South Coast offers an unprecedented array of natural wonders that draw thousands of visitors each day.

  When driving the route from Reykjavík city, the first major features are the two great waterfalls of Seljalandsfoss and Skógafoss, which sit beneath the notorious subglacial volcano, Eyjafjallajökull. On clear days from these beautiful cascades, the Westman Islands can be seen across the ocean.

  A little further down the route is the glacier Mýrdalsjökull, which covers one of Iceland’s most explosive volcanoes, Katla. Many glacier hikes are taken here upon the outlet of Sólheimajökull.

  The aforementioned Dyrhólaey cliffs are next, home to many seabirds. Even if you come outside of puffin season, they are well worth a visit; jutting out to sea is an enormous rock arch of the same name, which you can marvel at from many angles.

  

  Adjacent to the village of Vík is the famous black-sand beach, Reynisfjara, home to the rock pillars of Reynisdrangar, said to be two trolls frozen by the light of the sun. Though beautiful, this area is gaining notoriety for its dangerous sneaker waves, so visitors should be sure to stay well away from the edge of the water, even on a calm, still day.

  There are no landmasses between Reynisfjara beach and the continent of Antarctica, so you can imagine how the waves can build momentum.

  After passing through Vík, you will cross the glacial sand plain of Skeiðarársandur, before entering Vatnajökull National Park, home to the largest ice cap in Europe, Vatnajökull itself, dozens of glacial outlets and the magnificent Jökulsárlón glacier lagoon.

  While almost all of these sites can be seen from Route 1, they make up a fraction of what the South Coast has to offer. The vast sand plains of Sólheimasandur are home to a crashed DC-3 Plane Wreck, and within the Vatnajökull National Park is the dramatic Skaftafell Nature Reserve.

  Less than a kilometre from Seljalandsfoss is the hidden gem of Gljúfrabúi waterfall, and short distances from Jökulsárlón you will find the Diamond Beach, where icebergs wash on the black-sand shore, and another glacier lagoon, Fjallsárlón.

  南岸,

  

  The Diamond Beach is a strip of black sand belonging to the greater Breiðamerkursandur glacial plain, located by Jökulsárlón glacier lagoon on the South Coast of Iceland.

  Here, the icebergs which fill Jökulsárlón glacier lagoon wash up on shore, standing dazzling and defiant in stark contrast to the black sand beach. It is, therefore, a favourite amongst photographers, nature-lovers, and wildlife-enthusiasts. Many seals call this beach home, and it is one of the best places in the country to see orcas from the shore.

  Breiðamerkursandur

  Breiðamerkursandur is a glacial outwash plain located in the municipality of Hornafjörður. The sand stretches approximately 18 kilometres along Iceland’s South Coast, more specifically from the foot of Kvíárjökull Glacier to the famed glacier lagoon Jökulsárlón, that nests by the foot of Breiðamerkurjökull Glacier.

  Both glaciers make up part of the 30 outlets of Vatnajökull, Europe’s largest ice cap and the central feature of the Vatnajökull National Park. Many of these are seen en route to the Diamond Beach as you travel along the South Coast.

  The outwash plain was formed when three of Vatnajökull’s outlet glaciers, Breiðamerkurjökull, Hrútárjökull and Fjallsjökull, flowed forward due to volcanic activity and ground the rocks of the underlying surface, creating and pushing forward the glacial sediments.

  Such sand plains are a common part of the Icelandic landscape, due to the island being volcanically active as well as boasting numerous ice caps. The terminus (the tip of a given glacier) also dug deep into the ground and left what is now the Jökulsárlón glacier lagoon. Although now the deepest lake in all of Iceland, it only began to form in 1935.

  The glacier lagoon and Diamond Beach are fantastical sites, however, the rate of their expansion is, unfortunately, a consequence of climate change. With the rate that the glaciers are melting, there may be no ice left at either site within decades.

  Jökulsárlón Icebergs

  

  Jökulsárlón glacier lagoon is one of the most famed and visited attractions in Iceland. Floating on the lagoon are enumerable icebergs that have broken off the resident glacier, creating an ever-changing scenery of incredible allure.

  The river Jökulsá connects the lagoon to the Atlantic Ocean, meaning that these icebergs eventually drift out to sea where they are polished by the waves before floating back to the black sands of Breiðamerkursandur. The name ‘Diamond Beach’ thus comes from the white ice on the black sand appearing like gemstones or diamonds, as they often glisten in the sun and sharply contrast their jet black surroundings.  

  Safety at the Diamond Beach

  The Diamond Beach is a safe place for any responsible traveller; unlike at Reynisfjara, another South Coast black-sand-beach, sneaker waves and rip currents are not notorious for whisking unwitting tourists out to sea. However, there are still dangers to consider.

  The main one of these is the icebergs themselves. Under no circumstance should you climb upon an iceberg, due to their slippery surfaces and sharp edges.

  This is especially the case if the iceberg is at all in the water, as it could flip and trap you underneath, or else be pulled out to sea by a current with you on it.

  The risk of injury and illness in the form of hypothermia is so great that extortionate fines exist to deter any ‘rebels’ looking for a thrill-seek. These have only come about due to serious incidents, to protect not only tourists at the lagoon but guides and staff who may feel obligated to embark on a dangerous rescue if they see someone at risk.

  ---

   

  Diamond Beach

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