蓝冰洞一日游(包含从雷克雅未克往返的航班)

冰岛南岸是冰岛最受欢迎、最热门的旅游景区之一，也是冰岛明星必游景点最为集中的地区。

黄金圈、杰古沙龙冰河湖(Jökulsárlón)、斯科加瀑布(Skógafoss)、塞里雅兰瀑布(Seljalandsfoss)、斯卡夫塔山等游客们耳熟能详、举世闻名的自然景点都位于冰岛南岸地区。

概括而论，冰岛南部可以分为两个部分：西部的低地平原地区以及东部地区。

冰岛南部的低地地区

冰岛南部的低地地区始自Hellisheiði地热区，终至埃亚菲亚德拉冰川(Eyjafjallajökull)，长达100公里。这一地区分布着平坦且肥沃的耕地，是许多冰岛马和冰岛羊的家园。

从地质方面来看，这一地区非常“年轻”；低地地貌形成于冰河时期，由火山爆发泄出的岩浆流塑造。至今这片地区仍然保存着不少活跃的火山系统，如埃亚菲亚德拉冰川火山、海克拉火山(Hekla)等等。

冰岛最著名的旅游路线黄金圈也属于这片南部低地地区。黄金圈的三大景点包括位于两大地质板块交界的世界遗产辛格维利尔国家公园(Þingvellir)、地热运动活跃的盖歇尔间歇泉地热区(Geysir)与冰岛最大的断层瀑布黄金瀑布(Gullfoss)。

值得一提的是，位于北美与欧亚板块的交界处的辛格维利尔国家公园不仅是地理的瑰宝，还是冰岛主陆唯一一处联合国教科文组织认定的世界文化遗产；世界首个民主议会Alþingi即诞生于此，这也是冰岛乃至世界范围的珍贵历史遗产。

这一地区的活跃地热运动也直接塑造了许多特色地貌，例如1975年韦斯特曼群岛(Westman Islands，也称西人群岛)的火山爆发就促成了一个崭新岛屿的形成。

与大多数早期冰岛聚落不同，冰岛南部的低地地区少有渔业城镇，仅有唯一一个重要的港口城镇：Þorlákshöfn；前往韦斯特曼群岛的渡轮也从Þorlákshöfn出发。

其他城镇则主要位于内陆地区，包括一号环岛公路上的塞尔福斯(Selfoss)、惠拉盖尔济(Hveragerði，“温泉小镇”)、海德拉(Hella)以及科沃尔斯瓦特鲁(Hvolsvöllur)等。

冰岛南部的低地地区也孕育了迷人的文化。冰岛第一位主教的定居地斯考尔霍特(Skálholt)就位于这片地区，而恢弘的《尼雅尔萨迦》的文学情节也在这一地区展开。

游客在这一地区也可以参加如骑冰岛马、钓鱼、徒步、浮潜、皮划艇等特色户外活动。

冰岛南部的东部地区

这一地区大概覆盖了卡特拉火山(Katla)/米尔达斯冰川(Mýrdalsjökull)至杰古沙龙冰河湖一带，以数目众多的火山、冰川与迷人的高地景色闻名。

与冰岛南部的低地地区一样，这一地区的地貌形成也同样受到火山爆发的深刻影响，却呈现出截然不同的地质景观。游客将在这里发现黑沙滩、悬崖石壁、玄武岩石、瀑布、冰川、火山等极具冰岛特色的壮丽地貌。

这一地区的冰川河也衍生出许多瀑布，其中就包括著名的斯科加瀑布与塞里雅兰瀑布。

索尔黑马冰川(Sólheimajokull)也位于这一地区。索尔黑马是米达冰川的一条冰舌，游客可以跟随专业向导，参加冰川徒步旅行团，以双脚丈量冰川的磅礴。在斯科加镇(Skógar)，游客可以参观民俗博物馆，了解冰岛的发展历程。Fímmvörðuháls等著名徒步路线等则沟通了海岸地区与内陆高地地区。

冰岛最南小镇维克镇(Vík)也坐落于此，集聚于小镇周围的雷尼斯黑沙滩(Reynisfjara)、迪霍拉里岬角(Dýrholaey)、Reynisdrangar岩柱都是在冰岛南岸之行中不容错过的美景。

沿一号公路继续东行，游客将抵达斯卡夫塔山自然保护区(Skaftafell)。斯卡夫塔山是冰岛最大国家公园——瓦特纳冰川国家公园(Vatnajökull)的一部分。

被誉为“冰岛自然王冠上最耀眼的宝石”的杰古沙龙冰河湖接近冰岛东部与南部的交界，冰河湖对面布满碎冰的“钻石冰沙滩”也是这一地区最为迷人的自然宝藏之一。

Jökulsárlón is Iceland’s most famous glacier lagoon. Conveniently located in the southeast by Route 1, about halfway between the Skaftafell Nature Reserve and Höfn, it is a popular stop for those travelling along the South Coast or around the circular ring road of the country.

Geography

As a glacier lagoon, Jökulsárlón is a lake that is filled with the meltwater from an outlet glacier. In this case, it is Breiðamerkurjökull, a tongue of Europe’s largest ice cap, Vatnajökull.

It stands out, however, due to the fact that it also fills with icebergs breaking from the glacier, some of which tower several stories high.

These icebergs, other than their scale, are notable for their colouration. Although they are, as expected, largely white, most are also dyed electric blue in part, with black streaks of ash from eruptions centuries past.

When the icebergs finally make it across the lagoon, they either drift out to sea or wash up on the nearby shore. Because of the way they glisten against the black sands of Breiðamerkursandur, this area has been nicknamed ‘the Diamond Beach’.

In spite of being a rather recent formation, Jökulsárlón is the deepest lake in the country, with depths reaching 248 metres. With a surface area of 18 square kilometres, it is also growing to be one of the largest.

History

Jökulsárlón has not been around since Iceland’s settlement; it only formed around 1935. This was due to rapidly rising temperatures in the country from the turn of the twentieth century; since 1920, Breiðamerkurjökull has been shrinking at a dramatic rate, and the lagoon has begun to fill its space.

Today, the expansion of Jökulsárlón is accelerating. As recently as 1975, it was just 8 square kilometres, and now that size has more than doubled.

In the relatively near future, it is expected that the lagoon will continue to grow until it becomes a large, deep fjord.

Though a dark omen for Iceland’s glaciers and ice caps in general, the retreat of Breiðamerkurjökull has resulted in an incredibly beautiful, if temporary, site. This has not been overlooked by Hollywood.

Jökulsárlón has been featured in the James Bond films A View to Kill in 1985 and Die Another Day in 2002, 2001’s Lara Croft: Tomb Raider, and 2005’s Batman Begins.

In 2017, Jökulsárlón was enveloped into the Vatnajökull National Park, thus it is now fully protected by Icelandic law.

Wildlife

Because of the wealth of herring and capelin that the tides bring into the lagoon, Jökulsárlón is somewhat of a hot-spot for Iceland’s wildlife.

In summer, it is a nesting site for Arctic Terns; stay well away from this area, as these birds are notorious for the fierceness with which they protect their eggs, dive-bombing the heads of any they see as a threat. Skuas also nest on the lake’s shores in this season.

Seals can be reliably spotted here throughout the year, swimming amongst or else hauling out on the icebergs. Jökulsárlón provides them with a safe haven to rest and socialise, especially considering the waters of southeast Iceland are renowned for their population of orcas.

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.

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。

Höfn is an Icelandic fishing town of just over two thousand people in southeast Iceland. It is the most significant settlement on Route 1 between the village of Kirkjubæjarklaustur in the south and Egilsstaðir in the east.

Geography of Höfn

Höfn means ‘harbour,’ as the town is located in one of the few natural harbours of Iceland’s South Coast; unlike the rest of the country, this stretch is beachy and flat, and thus there are hardly any small coastal villages when compared to places such as the Snæfellsnes Peninsula.

The town is right at the tip of its own peninsula, which is easy to reach throughout the year. It sits at the base of Route 99, which detours off from Route 1. It is surrounded on three sides by the ocean, which has been known to freeze over in extreme conditions.

The town can also be reached by plane in good weather, as it is one of the few locations in the country with a domestic airport.

The largest glacier in Europe, Vatnajökull, which sits in a National Park of the same name, is within clear view of Höfn.

Nearby Locations to Höfn

Höfn is most often visited by those driving the full Ring Road of Iceland, as a place to stay just before or after visiting the South Coast or East Fjords.

It is also visited independently, however, by those seeking to spend enough time near the sites of southeast Iceland, most notably Vatnajökull National Park, the Jökulsárlón Glacier Lagoon, the Diamond Beach and Vestrahorn Mountain.

All of these sites are incredible. Vatnajökull, for example, is incredibly diverse, boasting a huge array of different sites to marvel over. In its southwestern corner, for example, it is home to the Skaftafell Nature Reserve, an oasis of unbelievable scenery, whereas to its west sits the mighty mountain Snæfell, renowned for its wildlife such as pink-footed geese and reindeer.

The Jökulsárlón Glacier Lagoon has recently been enveloped into the National Park, but warrants its own discussion. Out of all the sites listed, it is here where most visitors to Höfn want to spend the bulk of their time. This lagoon is, in fact, Iceland’s deepest lake, and renowned for being full of great icebergs throughout the year.

These bergs snap off of a tongue of Vatnajökull glacier, before slowly cruising through the waters towards the ocean. As they travel, they often become resting spots for some of the many seals who live in and around the lagoon.

The site is marvellous to behold, with a particular appeal for landscape photographers. Visitors, however, should not spend all their time in the lagoon. By following the channel from Jökulsárlón to the ocean, you will come onto the Diamond Beach, where these icebergs wash up on the shore and glisten against the black sands.

A final site in southeast Iceland, closer to Höfn than those previously listed, is Mount Vestrahorn. This jagged peak is ominous and dramatic, with two sharp peaks that have created the nickname ‘the Batman Mountain.’ Another favourite amongst photographers, it’s distinct silhouette and colouration make it the perfect subject regardless of the weather.

Culture at Höfn

Like many of Iceland’s small, coastal towns, Höfn has a surprising amount of culture. Its cuisine is particularly notable, with the celebration of it coming to a head at the annual Lobster Festival, held every July. This comes as little surprise, considering the town’s long history as an important fishing port.

Höfn also has several art museums where visitors can admire local handicrafts, although it should be noted, in spite of conflicting evidence on the internet, that the Höfn Glacier Museum is now closed.

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

The famed South Coast shoreline stretches from the greater Reykjavík area and is dotted with natural wonders such as cascading waterfalls, volcanoes both active and dormant, black sand beaches and glacier lagoons. 

Geography, Nature & Wildlife

Iceland is divided into eight geographical regions. Out of these, the Southern Region is the largest, as it spans over 24.000 square kilometres with its administrative centre in the municipality of Selfoss. 

What is known as the South Coast embodies the shoreline of this particular region. The area consists of a lowland that is mostly composed of marshlands, bays and cultivated pastures that are met by a series of black beaches where the estuaries to the east and west of the district close off the coastal body. 

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 shore line. 

The region boasts vibrant bird life during all seasons. It is not only rich with both marshland birds and seabirds but also migrating birds such as the North Atlantic puffin. Some species stay throughout the harsh Icelandic winter, including the northern diver, the loom and various species of gulls and ducks.  

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 highlights in their correct order are: 

• Seljalandsfoss Waterfall
• Vestmannaeyjar; The Westman Islands
• Eyjafjallajökull Glacier Volcano
• Skógafoss Waterfall
• Sólheimajökull Glacier 
• Dyrhólaey Peninsula
• Reynisfjara Black Sand Beach
• Reynisdrangar Sea Stacks
• Coastal Village Vík í Mýrdal
• Skeiðarársandur Glacial Sand Plain
• Vatnajökull National Park
• Jökulsárlón Glacier Lagoon 

These attractions count for but 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 close to Seljavellir by the Skógar Village there's Seljavallalaug, one of the oldest swimming pools in Iceland. 

• Explore the many wonders of the area on these South Coast Tours

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.