Attractions: 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.
DYRHOLAEY
Dyrhólaey is a 120-metre high promontory, not far from Vík. The place got its name from the massive arch that the sea has eroded from the headland. (The name literally means "door-hole"). When the sea is calm, big boats can sail through it. There has even been a maniacal daredevil pilot that flew through the arch with a small-craft airplane! From the top of Dyrhólaey there is a great view. The headland is thought to have been made in an underwater volcanic eruption late in the glacial period, not unlike the eruption of Surtsey. Several outcrops are in the sea, the highest one called Háidrangur ("High column") is 56 m. high. Dyrhólaey has been a natural reserve since 1978. The promontory is widely known among sailors as "Portland", and English trawler fishermen ubeach where one can climb (at your own risk). According to legend the Reynisdrangar needles were formed when two trolls were trying to drag a three-masted ship to land. When daylight broke they turned to stone. The Needles can be seen clearly from the village of Vík and are 66 meters above sea level at their highest. In one of the many caves here - there is a local legend about a monster having lived here for many centuries. The monster seems to have disappeared after a landslide over 100 years ago…sed to call it "Blow hole". There are also amazing rock formations all along the Birdlife here is abundant, with puffins and eider ducks being the most common species in the area. The lighthouse on the top of the cliff stands impressive and stoic in this often very windy area. Be careful not to go too close to the ledge of this dramatic cliff.
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.
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.
Scenic landscape, favorable weather conditions and a selection of hiking trails make Skaftafell an ideal destination for those who like to enjoy outdoor activities in Icelandic nature.
Short and easy trails lead to waterfall Svartifoss and glacier Skaftafellsjökull, but for those who want to reach further out, the Morsárdalur valley and Kristínartindar mountain peaks are perfect in terms of distance and labour. Skaftfell is also the perfect base camp for those who seek to climb Iceland‘s highest mountain peak, Hvannadalshnjúkur.
In 1967, Skaftafell National Park was established, but in 2008 it became a part of the newly established Vatnajökull National Park.
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.
Svartifoss (Black Falls) is a waterfall in Skaftafell in Vatnajökull National Park in Iceland, and is one of the most popular sights in the park. It is surrounded by dark lava columns, which gave rise to its name. Other well-known columnar jointing formations are seen at the Giant's Causeway in Northern Ireland, Devil's Tower in Wyoming, United States and on the island of Staffa in Scotland. There are also similar formations throughout Iceland, including a small cave on the beach of Reynisdrangar.
The base of this waterfall is noteworthy for its sharp rocks. New hexagonal column sections break off faster than the falling water wears down the edges.
These basalt columns have provided inspiration for Icelandic architects, most visibly in the Hallgrímskirkja church in Reykjavík, and also the National Theatre.
FJAÐRÁRGLJÚFUR
Fjaðrárgljúfur is a magnificent and massive canyon, about 100 meters deep and about two kilometres long. The canyon has sheer walls, and is somewhat serpentine and narrow. The bedrock in Fjaðrárgljúfur is mostly palagonite from cold periods of the Ice Age and is thought to be about two million years old. The river Fjaðrá has its source in the mountain Geirlandshraun and falls off the heath edge in this stunning canyon until it makes it down into Skaftá river. Fjaðrá has changed a lot in the course of time. Today Fjaðrá is often rather low in water and therefore hikers can safely choose to walk inside the canyon. However, wading is necessary fairly often. Deep in the canyon there are waterfalls so one needs to walk the same way back. Most people choose to walk along a walking path up on the canyon's edge while simultaneously enjoying the view above the canyon.
Formation of the Fjaðrárgljúfur canyon
It is believed that Fjaðrárgljúfur formed at the end of the last Ice Age, about nine thousand years ago. When the glacier retreated, a lake formed in the valley behind a hard resistant rock. The run-off from the lake flowed to where Fjaðrárgljúfur is today. Glacial rivers from the glacier's edge carried a lot of sediment into the lake and the river which ran from it dug itself down into the rock and down onto the palagonite in front of it. Because the cascade has been so large, it was powerful in digging out the canyon. Eventually the lake filled with sediments and the river's strength dwindled. When the lake filled up completely, the river began to dig itself into the sediment layers which it had previously left in the valley. Fluvial terraces on both sides in the valley give an indication about the original height and location of the lake while a deep channel in the palagonite serves as a silent reminder to the power of nature.
