亮点 The Reykjavík Capital Area is the country's largest and most populated city and currently home to 211.282 people, that's two-thirds of the entire Icelandic population!
Although it's one of the smallest capital cities in the world, it's still big enough to fit in six super-sized districts, with Reykjavík as the largest having a population of 121.230. Each district has its own elected council that governs the community and is responsible for the execution of legally determined projects.
A unique waterfall in the river Seljalandsá, about 30 km west from Skógar. It is 60 meters high with a foot path behind it at the bottom of the cliff, but with a thin cascade. It is the only known waterfall of its kind, where it is possible to walk behind it. The waterfall is very picturesque and therefore its photo can be found in many books and calendars.
Access to the waterfall is from the farm of Seljaland along the Ring Road, Iceland's main highway. A little further to the west there are several other falls, among them the interesting Gljúfrabúi which is partially masked by its own canyon. Access to it is from Hamragarðar farm along the road, east of Markarfljót.
Both of these "do-not-miss" attractions lie very close to the main Ring Road at the base of the Eyjafjallajökull Glacier, on the road leading in to Thorsmörk.
SKOGAFOSS - WATERFALL
Only a few kilometers away from the south shores of Iceland, lies the village of Skógar along the Southern Ring Road. It is a popular summer-resort centre surrounded by unusual scenic beauty. The breath-taking view of Skogáfoss waterfall and scenic surroundings and the snow-capped heights of two towering glaciers are Skógar's major summer attractions. There are two settlements by this name. One is Ytri-Skógar (outer or western Skógar) and the other Eystri-Skógar (eastern Skógar), located at a short distance from each other. Ytri-Skógar, commonly referred to as Skógar, is the main settlement. It is an old farm and has a church from 1890. It is located between the Skógá and Kverná rivers.
The greatest attraction of Skógar is of course the beautiful 60-metre high Skogáfoss waterfall in the river Skógá. Like the legends of buried treasures of Egill Skallagrímsson in Mosfell near Reykjavík and Ketilbjörn in Mosfell near Skálholt, there is a similar legend about the settler Þrasi who is believed to have buried his chest of gold under the Skogáfoss waterfall.
If the sun conditions are favourable - one can see a vivid rainbow in front of the waterfalls. The river below the falls holds a large salmon and char population and fisherman are seen here fishing July - October. The path leading to the top of the waterfalls continues following the river upstream - where numerous more dramatic waterfalls of sheer beauty are to be found. A great hike - to say the least!
One of the finest folk museums in Iceland is situated in extraordinarily beautiful natural surroundings. The interesting local folk museum has a collection of over 6000 artifacts and examples of various types of dwellings in Iceland since the early times. The collection of tools and equipment used at land and sea is outstanding. The museum also has an old turf farmhouse, where guests can experience the standards of living in Iceland in past centuries.
From Skógar the Ring Road runs eastwards along the foot of Mýrdalsjökull glacier, across the southern sandy plains and over glacial rivers, passes Seljavellir and continues along the soaring glaciated massive of Eyjafjöll and the two waterfalls Seljalandsfoss and Gljúfrabúi. From here runs a 10 km long trek along the river Skógá over the Fimmvörðuháls Pass between the Eyjafjallajökull and Mýrdalsjökull glaciers to the mountain oasis of Þórsmörk.
Skógar is a place to explore the natural diversity of the south or, if the weather is good, to spend a holiday amid beautiful and rugged landscapes. It is also very close to the ocean and the unique black beach.
Reynisdrangar are basalt sea stacks situated under the mountain Reynisfjall near the village Vík í Mýrdal, southern Iceland which is framed by a black sand beach that was ranked in 1991 as one of the ten most beautiful non-tropical beaches in the world.
Legend says that the stacks originated when two trolls dragged a three-masted ship to land unsuccessfully and when daylight broke they became needles of rock.
Contemporary legends note the story of a husband who found his wife taken by the two trolls, frozen at night. The husband made the two trolls swear to never kill anyone ever again. His wife was the love of his life, whose free spirit he was unable to provide a home for; she found her fate out among the trolls, rocks, and sea at Reynisfjara.
Vatnajökull National Park was established in 2008. It includes the national parks in Skaftafell (est. 1967) and Jökulsárgljúfur (est. 1973) along with the Vatnajökull ice cap itself and extensive areas around it.
Vatnajökull National Park is characterised by diversity on all fronts, be it landscape, biosphere, cultural remains or service levels. For simplification, however, it may be placed into two categories: uninhabited highland areas with limited services and lowland areas with higher service levels.
The park‘s visitor centres are all located in lowland areas. Each of them has an exhibition about the park‘s nature and cultural heritage. Each also has a souvenir shop with special emphasis on local handicraft and products.
In 2018, Vatnajökull National Park was nominated for inclusion in the World Heritage List. The nomination [PDF - 28 MB]is currently being reviewed by UNESCO.
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.
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.
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.
VÍK
Mýrdalshreppur region is one of three municipalities in Katla UNESCO GLOBAL Geopark. Vik is the central town in the Geopark and has developed as an important local commercial centre and service for the travel industry. Mýrdalur is the southernmost district of Iceland, bordered by the glacial river Jökulsá to the west and the river Blautakvísl to the east. Its northern border is the Mýrdalsjökull glacier (700 km2, Iceland's fourth largest glacier). Approximately 600 metres below the ice lies the dormant subglacial volcano Katla which the Geopark is named after. Its southern limits are black sands and the rolling Atlantic waves. Vik is the only seaside settlement in Iceland left without a harbour due to natural circumstances. Nevertheless, Vík's inhabitants used to go fishing and got products from ship before the roads were imposed in 1939.
The natural beauty of the area is spectacular. There are many places of interest in the vicinity of Vik. Just east of the outskirts of the village lies one of Europe's biggest arctic tern breeding grounds. A short hike within the close vicinity of Vik is sure to satisfy all serious nature lovers and birds watchers. To the south of Reynisfjall mountain a spectacular set of rock columns called Reynisdrangar rise majestically out of the Atlantic Ocean. Dyrhólaey is a 120 meters high headland extending into the sea and forming an impressive natural arch located in the western part of the Mýrdalur district. In the summer, the peninsula is home to hosts of puffins.
Mýrdalshreppur region has a good travel services all year around and offers plenty of camping, hostels, guesthouses, apartments and hotels. We have over 1200 rooms to be precise. Among the many aspects of Vík that make it attractive to tourist are the hiking trails, bird watching, paragliding in the blue sky, snowmobile tour on Mýrdalsjökull glacier, ATV tour or horse riding on the black beach, glacier walk on Sólheimajökull glacier, short or long jeep tours around the region, a wool centre and a wool gallery, our local fish store where you can get both fresh and smoked Arctic char, to list but a few. Not many other places in Iceland offer as many contrast of nature as Mýrdalur. The area is therefore an ideal place to visit for travellers who want to enjoy good service and the best of what the country's natural environment has to offer.
Vestrahorn, Vesturhorn or Stokksnes, these are all names for this same place. The area is approximately a ten-minute drive away from Höfn. The Horn area is below Vestra-Horn, a 454-meter-high mountain. It is an interesting geological site composing of un-stratified plutonic rock, mostly gabbro but with some granophyre. East of the mountain is a strange-shaped outcrop called Brunnhorn that stretches out to sea.
One of the first settlement farms in Iceland was Horn, Built by Hrollaugur, son of Rögnvaldur earl of Møre in Norway. Hornafjörður Municipality and several natural sites are named after the settlement farm. In the Second World War, the Horn area became a base for the British army and later a NATO radar station was set up at Stokksnes, south of Horn. At Stokksnes you can feel the power of the Atlantic Ocean as the waves hit the rocky shore with massive force.
Vestrahorn is a photographer’s paradise. Come here to photograph the dramatic landscape, or just sit and enjoy the vast beauty. A very beautiful unspoiled natural site.
The shore features stunning lava dunes, that are constantly being shaped by the natural forces of water and wind. Down towards the sea, it is possible to get perfect reflections in the wet sand. Seals also tend to hang out on the stretch of sand, so if you’re lucky you can catch a picture of a lazing seal as well.
Mývatn offers a unique natural environment. With large contrasts and small distances you can experience the most and the best that Iceland has to offer. Large open spaces with roads and walkways lead travellers to unworldly locations, where volcanic eruptions have played a crucial role in the formation of the landscape. Whether the plan is to enjoy the landscape, examine unique natural phenomena or take a closer look at the pant and bird life, Mývatn has it all. Furthermore the area offers a variety of services in accommodation, food and entertainment, based on years of experience and knowledge. A large number of travellers visit Mývatn in the summer, but many believe the lake and its surroundings to be no less impressive in the wintertime.
Mývatn is the 4th largest lake in Iceland, 37 km2 in area. Its shores are indented with many coves and inlets and its surface is dotted with around 50 small islets and skerries. Midges (Chironomidae) are abundant and the ubiquitous swarms of these tiny flies give the Lake its name.
The lake itself is very shallow, and the rays of the sun reach the lake bed over its entire surface. The ecology of the lake area is extremely diverse and interesting; one important characteristic of Mývatn, being the prolific growth and abundance of freshwater seaweed. On the bed of the lake are great quantities of diatoms, while, nearer the surface, Mývatn's famous arctic char weave their way between aquatic plants and little islets topped with fertile vegetation.
On and around the lake there is a teeming and varied birdlife, and Mývatn is the habitat of many kinds of lake and marsh birds. However, much of Mývatn's fame is due to the fact that, during summer, there are more different species of duck gathered on and around the lake than anywhere else in the world. Mývatn is a legally protected conservation area and appears on the register of internationally important wetlands, along with the Laxá river which flows out of the lake.
Hvítserkur, otherwise known as the Troll of Northwest Iceland, is a 15 m (49 ft) tall basalt rock stack protruding from Húnaflói Bay. The rock is a nesting ground for seagulls, shag and fulmar, making it appear constantly in motion, further enforcing the idea that Hvítserkur is, in some way, very much alive.
Hvítserkur is best viewed along the eastern shore of Vatnsnes Peninsula and takes its name from the birdlife that nests on top of it. In Icelandic, the name translates to “white shirt”, a nod to the colour of the bird droppings that cover the rock.
Photographers tend to be drawn to Hvítserkur as a subject due to the way the sun, moon, and aurora borealis reflect off of the flat water around its distinctive form.
Folklore of Hvítserkur
It should come as no surprise that Hvítserkur is often referred to as a troll—most distinctive Icelandic rocks are. Folklore says that Hvítserkur was originally a troll from the peninsula, determined to rip the bells down from Þingeyraklaustur convent; trolls, unlike elves, are said to be terrified of Christianity.
The beast was so enraged and persistent that it did not notice the rising sun, and was instantly petrified for eternity in its rays.
In hindsight, like most of Iceland’s folktales, it seems this one had a Christian message not so subtly weaved into it. It is likely that the story was an allusion to the people’s stoic resistance to the Christianisation of Iceland, implying those who held onto the view were as stubborn, stupid, violent and wicked as trolls, and perhaps on their way to a similar fate.
Iceland converted to Christianity in 1000 AD under the threat of invasion from Norway, and the transition was not easy; those who practised the religion of the Old Norse Gods were ostracised and punished for the millennium that followed.
Formation of Hvítserkur
The scientific community has another explanation for how Hvítserkur formed. Erosion from the cascading sea water has carved three large holes through the basalt rock, sculpting and shaping it into what appears as some petrified, mythological animal.
The base of the stack has been reinforced with concrete to protect its foundations from the sea, but this has not stopped visitors’ interpreting the rock’s peculiar shape.
Some say Hvítserkur looks like more like an elephant than a troll, while others claim it looks like a rhino. Some onlookers have gone as far as to claim the rock appears as a dragon or dinosaur drinking.
DETTIFOSS WATERFALL
The Dettifoss waterfall is with the greatest volume of any waterfall in Europe, 500 cubic metres of water per second plunges over the edge. Dettifoss is 45 m high and 100m wide. A nice hiking trail, 34km, goes along the canyon from Dettifoss to Asbyrgi. Camping possible in Vesturdalur.
Road 864 goes from road 85 past Dettifoss on the east side towards road 1. This is a gravel road and driving speed depends on road conditions each time. Road 864 is closed durning winter time due to snow or wet condtitions (muddy road) and does not open until early summer (end of May).
Gravel road 862 is on the west side of river Jökulsá. The road is passable for normal vehicles from Asbyrgi to Dettifoss, with Vesturdalur (Hljodaklettar) and Holmatungur between. Up until 2011 this road was categorised as a mountain road (F-road) but is now served as a gravel road. The conditions of gravel roads in Iceland can vary, so travellers are asked to be aware of road conditions at any time and adjust driving speed to the conditions.
Road 862 is closed durning winter time, due to snow or wet conditions (muddy road) and does not open until late May or early June. From Dettifoss onwards south to road 1, on the west river bank, there is a new, paved road which is passable for all vehicles. This road is not in service from January until the beginning of April.
Goðafoss Falls
Nicknamed by one local as ‘The Beauty’ in comparison to ‘The Beast’ of Dettifoss, the name Goðafoss could be translated roughly as The Waterfall of The Gods. An impressive site any time of year, in late spring, if you can catch it while there´s still icicles bedecking its sides, it’s a particularly otherworldly place to visit.
History
In the year 999, a holy man by the name of Þorgeir made Christianity the official religion of Iceland. To mark the occasion, he chucked some Pagan statues into the water here, making Goðafoss the famous symbolic site of Iceland´s conversion.
Námaskarð Pass is a geothermal area on the mountain Námafjall, in north Iceland, less than half an hour’s drive from Lake Mývatn. It is located by Route 1, which encircles the country.
Connected to the Krafla volcano system, Námaskarð is home to many hot-springs and fumaroles.
Geography of Námaskarð
Námaskarð is notable due to its barrenness; no vegetation grows on its slopes. This is due to the heat beneath the earth, the acidity in the soil, and poisonous fumes being expelled.
That is not to say, however, that the site is dull; its life comes from the vivid colours that streak through the earth, dyed by the elements brought up with the steam. Expect to see shades of red, orange, yellow and green, particularly concentrated around the springs themselves.
The air smells intensely of sulphur throughout the area, which, while unpleasant, is a constant reminder of the powerful forces at work beneath your feet. Though it would be damaging for your health to spend too long breathing it, a visit for a few hours will not cause any problems.
While exploring Námaskarð, be sure not to touch any of the running water, as it is likely to be boiling. Also, give all the hot springs a reasonably wide berth, as the land surrounding them may be unstable, with scalding steam just beneath the surface.
Námaskarð is about 400 metres (1312 ft) above sea level.
Surroundings of Námaskarð
Námaskarð is situated between the mighty waterfalls of the Jökulsá á Fjöllum river (which include Europe’s most powerful waterfall, Dettifoss) and the Lake Mývatn area, making it a natural part of anyone’s itinerary if they are exploring the north from Akureyri or Mývatn.
Namaskard hverir
This spectacular high temperature area (410 m above sea level) is situated by road no. 1 by the Namaskard pass in the vicinity of Lake Myvatn. It is a prototype of such areas, consisting of stinking steam vents, solfataras and boiling mud pits. The whole area is metamorphosed by the geothermal activity and thick deposits of silica, gypsum and sulphur cover the ground. One has to be very careful crossing such areas, because the thin crust might brake.
Unfortunately too many people have been severely burnt by stepping through. The almost pure sulphur of this area was exported during the last few centuries. These sulphur mines were considered the richest in the country and the so-called Reykjahlid-brothers, the proprietors of the area, are said to have become rich by processing the sulphur and exporting it.
In 1563 the mines came into the possession of the Danish king and the sulphur processing continued with intervals to the middle of the 19th century. In 1939 a sulphur factory was built in Bjarnarflag, near the mines. Its operation came to an end after a few years. After that some entrepreneurs started building a factory on the spot and had some five or six boreholes sunk in the area to pipeline the steam to the factory. The foundations of the factory house had been built and the boreholes had been sunk, when the shareholders realized, that the end price of the product would be to high for the world market and decided not to continue with the project.
DIMMUBORGIR
Dimmuborgir is an area of randomly strewn lava rocks and cliffs, surrounded by vegetation, such as low bushes and plants. Dimmuborgir is a place of surprises with its myriad forms and images, small caves and towering volcanic rock, pierced by natural apertures.
The most famous of these formations is "The Church", aptly named, as this is a cave, open at both ends and with a dome-like ceiling.
Grundarfjörður's beautiful landmark is the most photographed mountain in Iceland. Its isolated position jutting out into the sea makes it a focal point for tourists and seamen alike. Surrounded by beaches, Kirkjufell has a lovely walking trail around it as well as a more challenging climb up to the top where bird and fish fossils can be found.
Arnarstapi
Arnarstapi was an important trading post in the past and had a much bigger population than it has now.
Columnar basalt, ravines and grottoes surround the Arnarstapi pier. There is good anchorage for small boats.
There is quite a large arctic tern colony in the village itself. A walk along the coastline is recommended to watch the birds and the magnificent lava formations. The seaside and the cliffs between Arnastapi and Hellnar have been made a Natural Reserve in 1979.
A very interesting old path follows the coastline where you can see old lending places of fishermen, lots of birds like the kittiwake, the Arctic tern and the fulmar and pass through a lavafield. If you take a guided tour, you will also hear a ghost story.
A sculpture of Bardur Snaefellsas by Ragnar Kjartansson stands by the beach at Arnarstapi.
SNAEFELLSJOKULL NATIONAL PARK
Snæfellsjökull National Park was established on June 28th, 2001.The Park's purpose is to protect and conserve the area's unique landscape, indigenous plants and animal life as well as the important historical relics. At the same time, the Park is meant to allow visitors easier access as well as an improved opportunities to get to know the area. National parks are amongst Iceland's finest assets and everyone is free to explore them.The Snæfellsjökull glacier lies within the national park, and the park is the only Icelandic national park that stretches to the sea. The geology of Snæfellsnes national park is diverse with formations from almost every era of Iceland’s past. The more prominent formations in and around the National Park mainly date from geologically “modern” times back to the last ice age. The hills to the north of the glacier, around Bárðarkista, are of volcanic palagonite tuff, formed during eruptions under the glacier or below the surface of the sea. Svalþúfa is most likely the eastern section of a crater that erupted under the sea, while Lóndrangar is a volcanic plug.
DJUPALONSSANDUR & DRITVIK
Djupalonssandur is a beautiful pebbled beach, with a series of rocks of mysterious form emerging from the ocean.
It is one of the few areas that lead down to the sea along this coast with its high dramatic cliffs. Watch out for the famous ghosts roaming the place!
The rests of a shipwreck can be seen on the beach. On the beach there are also big stones which people tried to lift and test their strength in the days of the fishing stations: Fully Strong 154 kg, Half-Strong 100 kg, Weakling 54 kg and Bungler 23 kg. Weakling marked the frontier of wimphood, any man who couldn't lift it was deemed unsuitable for a life as a fisherman.
LONDRANGAR BASALT CLIFFS
Uniquely-formed remnants of ancient basalt volcanic dikes sticking out from the sea.
Londrangar and the hill Svalthufa are the remains of a crater, which has been eroded to its present form by the sea.
The farmers in the area never made or make hay on the hill, because it is said to belong to the elves living in the area.
Younger lava fields surround this old crater ruin. The higher pillar (75m) was first climbed in 1735 and the lower (61 m) in 1938.
Below the hill you may find Thufubjarg cliff where according to a folktale the poet Kolbeinn Joklaskald had an encounter with the Devil.
On these cliffs, puffins and fulmars have their nests.
GRUNDARFJÖRÐUR
Home to Mt Kirkjufell
Though Grundarfjörður is not the most well-known town in Snæfellsnes, its mountain is certainly one of the most famous mountains in Iceland, if not the world. It is not unusual for photographers from all over the world to make their way to Grundarfjörður for the sole purpose of photographing this unique landmark which has even starred in a number of films, most recently The Secret Life of Walter Mitty.
Once the increasing number of visitors have had their fill of Kirkjufell, they quickly discover that there is a lot more on offer in Grundarfjörður than merely magnificent mountains. Nature abounds, with vibrant birdlife, spectacular waterfalls, great hiking trails and exciting marine visitors such as seals and whales putting in an appearance every now and then. During the long summer days, there are daily boat trips where visitors can go deep sea fishing, see puffins and other beautiful birds and perhaps even catch sight of a whale or two.
Grundarfjörður is conveniently located in the middle of Snæfellsnes and provides easy access to Stykkishólmur, Snæfellsbær and the Snæfellsnes National Park. There is a great selection of accommodation available, with a high quality hotel and hostel, two guesthouses, a farm holiday guesthouse and a campsite by the swimming pool.
The swimming pool with its hot tubs is just one of a number of exciting services around the town. There is also a golf course, a family restaurant, a hotel restaurant, a coffee shop in the culture and heritage centre (where the information centre is also located), horse rentals, a pharmacy, a liquor store, a dry cleaning and laundry service and a well-stocked grocery store.
Though most visitors to Grundarfjörður arrive by road, there are also thousands that come by sea. Grundarfjörður Harbour makes every effort to make a cruise ship's visit comfortable and memorable for passengers and crew alike and as a result the number of cruise ships visits have increased from 2 in 2001 to no fewer than 18 scheduled for this summer.
During summer the town truly comes alive in a number of different ways. The local Viking Association are building up a Viking "village" in the centre of town and Viking-age re-enactments are often the highlight of the day for cruise ship passengers.
During the town festival, Á góðri stund, which is held the last weekend in July, the town literally changes colour when inhabitants and their guests decorate their houses in red, blue, yellow and green and indulge in a range of activities for all the family, from art exhibitions to fighting Vikings to concerts on the pier.
From Mt Kirkjufell to the sea, Grundarfjörður welcomes all its visitors equally.
Kirkjubæjarklaustur - Skaftárhreppur
Kirkjubæjarklaustur was known in olden times as "Kirkjubær" (Church Farm) and was an important farming estate. It is one of the most tongue-twisting words to pronounce of any location in Iceland. Kirkjubæjarklaustur has developed into a village, the only centre of population in the district, with about 150 inhabitants. Kirkjubæjarklaustur, often abbreviated to "Klaustur", is centrally located in the district. Roads radiate from Klaustur in many different directions and the Ring Road runs through the district. The Laki road, just west of Kirkjubæjarklaustur, leads into the highlands. The circular Landbrot / Meðalland road serves the southern part of the district. The Fjallabak roads (north and south) lead from the Ring Road into the interior via Skaftártunga. The Álftaver road is a circular route serving Álftaver on Mýrdalssandur.
Kirkjubæjarklaustur is the only place between Vík and Höfn which offers services, including a fuel station, a bank, a post office and a supermarket. Nearby tourist attractions include the Laki craters, the Eldgjá and Skaftafell. An attraction close to the village is Kirkjugólf (Church Floor), a natural pavement of basalt. These are basalt columns down in the earth, eroded and shaped by wind and waves, but only the top can be seen, and they, as the name suggests, have the appearance of a paved church floor. It is a protected natural monument. This lava formation has similar origins as the Giant's Causeway in Ireland. All these attractions contribute to the popularity of Kirkjubæjarklaustur as a stopping point for tourists.
Skaftárhreppur
Skaftárhreppur district is the centre of the south of Iceland and the perfect location to stay while taking daytours to see many of Iceland's bestt known natural treasures, Skaftafell, Jökulsárlón glacier lagoon, Langisjór lake, Eldgjá fissure, Laki craters and Reynisfjara black beach to name but a few. This is an area where saga meets lava and is easily accessible all year round. Through the app Locatify Smartguide you can find two audio-guides "The Laki eruption 1783-1784" and "Klaustur trail" and learn about more about the history of the area. The district is part of Katla geopark and the gateway to the western part of Vatnajökull National Park.
中文
