Image Credit: by Sebastian Schellbach-Kragh from Pixabay
Iceland is truly a geologically rich land. The Jokulsarlon (Icelandic for glacial river lagoon) holds great charm for visitors. This lagoon is populated by icebergs that originate from the Breioamerkurjokull glacier, an arm of the massive Vatnajokull Ice Cap, the largest ice cap in Europe. In 1935 increasing amounts of silt began to build the lagoon which then grew quickly. Today, erosion continues to increase the area of the lagoon. Breioamerkurjokull was formed during the Little Ice Age (c 1300 -1850). When I saw the iceberg pictured above, I was amazed by the colors that stood out like a diamond on a gray day. Standing there looking at it for a while I began to feel a very strong connection with nature.
Jokulsarlon, Iceland Coordinates: 64.070278, -16.211667
Situated at the head of the Breioamerkurjokull glacier, it developed into a lake after the glacier started receding from the edge of the Atlantic Ocean. The lake has grown since then at varying rates because of melting of the glaciers. It is now 1.5 km (0.93 mi) away from the ocean's edge and covers an area of about 18 km2 (6.9 sq mi). In 2009 it was reported to be the deepest lake in Iceland, at over 284 m (932 ft), as glacial retreat extended its boundaries. The size of the lake has increased fourfold since the 1970s.
The lake can be seen from Route 1 between Hofn and Skaftafell. It appears as "a ghostly procession of luminous blue icebergs".
Jokulsarlon has been a setting for four Hollywood movies: A View to a Kill, Die Another Day, Lara Croft: Tomb Raider, and Batman Begins, as well as the reality TV series The Amazing Race. In 1991, Iceland issued a postage stamp, with a face value of 26 kronur, depicting Jokulsarlon.
The tongue of the Breioamerkurjokull glacier is a major attraction for tourists.
The Jokulsarlon lake provides outstanding views of the ice cap, a vast dome of ice that rises to a height of 3,000 ft (910 m). It spills to the lagoon 12 mi (19 km) away from the jagged glacier hill to the edge of the water line. The lake developed only about 60 years ago (1948 is mentioned), when the entire area was less than 100 ft (30 m) of glacier, which was only 250 yd (230 m) from the Atlantic Ocean, and 2 mi (3.2 km) away from Vatnajokull. Vatnajokull was at the shore line of the ocean and dropped icebergs into the ocean.
However, it started drifting inland rapidly every year, leaving deep gorges en route, which got filled with melted water and large chunks of ice. These icebergs gather at the mouth of the lake's shallow exit, melt down into smaller ice blocks, and roll out into the sea. In summer, icebergs melt and roll down the channel into the sea. The lake does not freeze in winter. Ice water and soil make a unique ecological phenomenon. Jokulsarlon Lake, the "glacier lake", is now reported to have doubled in size in the recent 15-year period. The huge blocks of ice that calve from the edge of Vatnajokull are about 30 m (98 ft) high, which fills the lagoon stocked with icebergs. Some icebergs appear naturally sculpted on account volcanic ash from ancient eruptions that partly covers them.
Jokulsarlon, Iceland Coordinates: 64.070278, -16.211667
Icebergs:
The icebergs that calve from the glacier edge move towards the river mouth and get entrenched at the bottom. The movement of the icebergs fluctuates with the tide currents, as well as being affected by wind. However, they start floating as icebergs when their size is small enough to drift to the sea. These icebergs are seen in two shades: milky white and bright blue, which depends on the air trapped within the ice and is an interplay of light and ice crystals.
Glacier - Breioamerkurjokull
The outlet glacier that feeds the lagoon is called Breioamerkurjokull. This outlet glacier is the only place in Iceland where a glacier meets the sea.
Out-wash plains - Breioamerkursandur
The glacier is responsible for the formation of a large outwash plain called Breioamerkursandur. It has a breadth of around 25 km and serves as bird habitat in the summer month. This outwash plain is constantly changing. The shoreline of the glacial lagoon used to be advancing, but is now retreating as there is a decrease in glacial rivers depositing material. However, as the glaciers melt, the land rises around 2-4 cm each year somewhat balancing out the retreating shoreline.
Fauna - Grey seals on the Jokulsarlon lake
The lake is filled with fish that drift in from the sea along with the tides. Seals gather in large numbers at the mouth of the lake to catch fish during the winter. Large numbers of seabirds, particularly Arctic terns, which nest nearby, gather to catch herring, trout, salmon, krill and other fish. Breioamerkursandur (the large sand deposits in the area) is the main habitat of the Arctic skua (Stercorarius parasiticus). During the summer season, the gull-like skuas have their nests on the lake's shores.
The skuas, fat and dark in colour with white wingtips, are said to be aggressive "pirates of the seas", which harass other birds as big as gannets. They also kill and eat smaller birds such as puffins. Great skuas are not afraid of human beings and also do not tolerate human beings close to their nests. These birds are reported to migrate from their wintering grounds off the coasts of Spain and Africa. Seals are seen either swimming in the lagoon or lying on icebergs. Many times, the tides carry shoals of herring or capelan into the lagoon by the tide and the birds feast on them.
Land Settlement and Farms
The first settlers arrived in Iceland around AD 870, when the edge of the tongue of Breioamerkurjokull glacier was about 20 km (12 mi) further north of its present location. During the Little Ice Age between 1600 and 1900, with lower temperatures prevailing in these latitudes, the glacier had grown by up to about 1 km (0.62 mi) from the coast at Jokulsa River, by about 1890. When the temperatures rose between 1920 and 1965, the Breioamerkurjokull glacier tongue rapidly retreated, continually creating icebergs of varying size, thus creating a lagoon in its wake around 1934-35. The lake is over 200 m (660 ft) deep where the glacier snout originally existed. Glacial moraines became exposed on both sides of the lake. In 1975, the lake was about 8 km2 (3.1 sq mi) in area and now it reportedly stands at 18 km2 (6.9 sq mi) at the edge of the glacier tongue.
Current Ownership
In 2017 the Icelandic State bought the farm Fell which includes Jokulsarlon. Later that same year Fell and other public land surrounding Jokulsarlon got protected as a part of Vatnajokull National Park.
The Jokulsarlon Landowners Association represented the owners of the land property Fell. This property was leased out for filming or any other commercial activity as required.
Einar Bjorn Einarsson is the operator of the boat trips on Jokulsarlon. The Landowners Association leased out the site at the lagoon front to this operator to ply the boats on the lagoon.
Nature Protection
Jokulsarlon and the surrounding area became a park of Vatnajokull National on 7 June 2008. The size of the park is 14,707 km2 Which is approximately 14% of Iceland, making it Europe's second largest national park in terms of area after Yugyd Va in Russia. On 5 July 2019, Vatnajokull National Park was inscribed as a UNESCO World Heritage Site. The unique qualities of Vatnajokull National Park are primarily its great variety of landscape features, created by the combined forces of rivers, glacial ice, and volcanic and geothermal activity. The National Park aims to preserve unimpaired the natural beauty of the park for the enjoyment, education, and inspiration of this and future generations.
An iceberg with Oraefajokull (southernmost part of Vatnajokull) in the background: The icebergs in Jokulsarlon, as well as this iceberg, fell off Vatnajokull.
Protective measures for the bridge
A coffer dam was constructed near the Glacial River Bridge that spans Jokulsarlon to build a row of protective measures of stone boulders to prevent any erosion of the foundation of the pillars of the bridge. This coffer dam enabled the Icelandic road administration to create workable access for the power shovel digger to place the row of stone protective measures, which would also divert the icebergs from hitting the bridge pillars, thus avoiding damage to the structure.
Given the current retreat rate of Vatnajokull, likely a deep fjord will develop where Jokulsarlon is now. This retreat is also posing a threat to the National Highway Route 1 of Iceland. The lagoon is 75 km (47 mi) to the west of Hofn town and 60 km (37 mi) east of Skaftafell. It is accessible by the ring road, Route 1, that goes across the lake, and where parking facilities have been provided for visitors. It is also known as the "tourist conveyor belt". Isolated large blocks of icebergs can be seen on the black sand beach, sometimes called "diamond beach" because of ice chunks scattered on the sand.
