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Published: August 28th 2019
We're moving around the island in a counterclockwise direction, so we are at the south part of the island. The storms hit from the south and the wind picks up alot of moisture. As the air rises over the mountains it drop the precipitation as snow which is why the largest glaciers are on the south side of the island. Then volcanoes erupt and push through the glaciers which causes massive floods. We drove by massive lava fields; some had moss all over them and some looked like they happened yesterday. We also went by areas that massive glacier floods had brought tons of debris, boulders, and ice. The shoreline was actually pushed out by debris from glacier outflow.
From GuidetoIceland website: "The vast Eldhraun lava field (“Fire Lava“), in the south of the Icelandic highlands, was created in one of the greatest eruptions in recorded history and is of the largest of its kind in the world. The Lakagigar craters were also created during this eruption.
This eruption lasted from 1783 to 1784 and is known as the Skaftáreldar (The Skaftá River Fires). This was a cataclysmic event for Iceland and beyond. In Iceland, it lead to disease,
crop failure and disasters.
The eruption affected Europe as well. In Great Britain, that summer is known as the Sand-Summer in Great Britain due to the fallout of ash and it is believed that the airborne haze and blocking of sunlight may have contributed to the French Revolution.
Despite the abysmal effect the eruption had, this lava field of 565 km2 is today one of the most stunningly attractive ones in Iceland.
The area features one of the most magnificent lava tube systems in the country, located north of the Lake Laufbalavatn. More than 200 caves have been found there, extending for more than five kilometers and 14 cu. meters."
We went to Skaftafell National Park. From Wikipedia:
Skaftafell National Park Skaftafell National Park
was a national park, situated between Kirkjubæjarklaustur
, typically referred to as Klaustur, and Höfn
in the south of Iceland
. On 7 June 2008, it became a part of the larger Vatnajökull National Park
It was founded on September 15, 1967, and enlarged twice afterwards. Before its inclusion into Vatnajökull National Park, it measured about 4807 km2
), making it Iceland's second largest national park. It contains the valley Morsárdalur
the mountain Kristínartindar
and the glacier Skaftafellsjökull
(a spur of the Vatnajökull
Skaftafellsjökull glacier as seen from the sky
The landscape is very similar to some of the Alps, but it has been formed over thousands of years by different influences of fire (volcanic eruptions of Öræfajökull
) and water (the glaciers Skeiðarájökull
), the rivers Skeiðará
. Volcanic eruptions under the ice-cap can give rise to jökulhlaups
(glacial floods) which swell the Skeiðará river massively. The sandy wasteland between the glacier and the sea caused by jökulhlaups
is called Skeiðarársandur
, and is a typical outwash plain
known locally as a sandur. The last large jökulhlaup occurred in 1996.
We went for a glacier hike on one of the glacier tongues of the Vatnajokull, the largest glacier in Europe.
With an area of 7,900 km²,
Vatnajökull is the largest ice cap
in Europe by volume (about 3,000 km³)
and area (not counting the still larger Severny Island ice cap
of Novaya Zemlya
, Russia, which may be regarded as in the extreme northeast of Europe).
On 7 June 2008, it became a part of the Vatnajökull National Park
The average thickness
of the ice is 380 m (1,250 ft),
with a maximum thickness of 950 m (3,120 ft). Iceland
's highest peak, Hvannadalshnúkur
(2,109.6 m (6,921 ft)), is in the southern periphery of Vatnajökull, near Skaftafell National Park
Vatnajökull Glacier in Iceland.
Under the ice cap, as under many of the glaciers
of Iceland, there are several volcanoes
Eruptions from these volcanoes have led to the development of large pockets of water beneath the ice, which may burst the weakened ice and cause a jökulhlaup
(glacial lake outburst flood
During the last ice age
, numerous volcanic eruptions occurred under Vatnajökull, creating many subglacial eruptions
In more modern times, the volcanoes continue to erupt beneath the glaciers, resulting in many documented floods. One jökulhlaup in 1934 caused the release of 15 km3
(3.6 cu mi) of water over the course of several days.
The volcanic lake Grímsvötn
was the source of a large jökulhlaup in 1996.
There was also a considerable but short-lived eruption of the volcano under these lakes at the beginning of November 2004.
On 21 May 2011 a volcanic eruption started in Grímsvötn in Vatnajökull National Park at
around 7 p.m.
The plume reached as up to 17 kilometres (11 mi).
Since it has been raining for 3 days, the crust snow on top of the hard, blue ice has been washed away, which means we were hiking, with crampons, on hard, blue ice. Took getting used to, especially going downhill. It was a great experience. I've never been up close and personal with a glacier like that. Lots of meltwater running off the glacier and moulins.
(or glacier mill
) is a roughly circular, vertical (or nearly vertical) well-like shaft within a glacier
or ice sheet
which water enters from the surface. The term is derived from the French word for mill.
They can be up to 10 meters wide and are typically found on ice sheets and flat areas of a glacier in a region of transverse crevasses.
Moulins can reach the bottom of the glacier, hundreds of meters deep, or may only reach the depth of common crevasse formation (about 10–40 m) where the stream flows englacially.
They are the most typical cause for the formation of a glacier cave
Note Rivers coming off the glacier.
This is where alot of the glacier floods occur.
parts of the internal structure of glaciers, that carry meltwater
from the surface down to wherever it may go.
Water from a moulin often exits the glacier at base level, sometimes into the sea, and occasionally the lower end of a moulin may be exposed in the face of a glacier or at the edge of a stagnant block of ice
Water from moulins may help lubricate the base of the glacier, affecting glacial motion
. Given an appropriate relationship between an ice sheet and the terrain, the head of water in a moulin can provide the power and medium with which a tunnel valley
may be formed. The role of this water in lubricating the base of ice sheets and glaciers is complex and it is implicated in accelerating the speed of glaciers
and thus the rate of glacial calving
We lucked out with the weather too. It rained hard before and after our hike to the glacier.
Next we went to the Jökulsárlón
Glacier Lagoon and Diamond Beach. It is called Diamond Beach because the small clear pieces of ice from the glacier on the black sand look like diamonds.
From Wikipedia: Jökulsárlón
); literally "glacial
river lagoon") is a large glacial lake
in southeast Iceland
, on the edge of Vatnajökull National Park
. Situated at the head of the Breiðamerkurjökull
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 248 m (814 ft), as glacial retreat
extended its boundaries.
The size of the lake has increased fourfold since the 1970s.
It is considered as one of the natural wonders of Iceland.
The lake can be seen from Route 1
. It appears as "a ghostly procession of luminous blue icebergs".
Jökulsárlón 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 Amazing Race
In 1991, Iceland issued a postage stamp, with a face value of 26 kronur
, depicting Jökulsárlón.<sup id="cite_ref-Jokul_2-1"
The tongue of the Breiðamerkurjökull glacier is a major attraction for tourists.
The Jökulsárlón 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 Vatnajökull. Vatnajökull 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.
Check out the weather report.
We were lucky, we didn't have much rain during the glacier walk.
Jökulsárlón 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 Vatnajökull 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.
An iceberg with Vatnajökull in the background: The icebergs in Jökulsárlón, as well as this iceberg, fell off Vatnajökull.
An isolated iceberg on the beach
Given the current retreat rate of Vatnajökull, likely a deep fjord
will develop where Jökulsárlón 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 Höfn 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.
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