Nordaustlandet's geology and landscape

Red Rijpfjord graniteThe red Rijpfjord granite dominates the inner part of Rijpfjorden, Wordieodden. In this picture the colour is particularly vivid due to the morning sun that also lights up Vestfonna in the background. (Image: Jørn Henriksen) View from Wordiebukta and northwards towards RijpfjordenView from Wordiebukta and northwards towards Rijpfjorden. On the opposite side of the fjord the mountain Båtkvelvet and the cape Kapp Lovén can be seen. On the far right is Nordkapp on the island of Chermsideøya. (Image: Arild Lyssand / The Governor of Svalbard) Cape Kapp Lejonhufvud in DuvefjordenThe cape Kapp Lejonhufvud in Duvefjorden consists of red granite. Parts of the Platenhalvøya peninsula can be seen in the background. (Image: Kit Kovacs & Christian Lydersen / The Norwegian Polar Institute) The landscape in the west of Duvefjorden.The landscape in the west of Duvefjorden. (Image: Kit Kovacs & Christian Lydersen / The Norwegian Polar Institute) A branch of the Austfonna ice capA branch of the Austfonna ice cap, the glacier Bråsvellbreen has a steep front towards the sea in the southern part of Nordaustlandet. (Image: Jørn Henriksen) The front of BråsvellbreenThe front of Bråsvellbreen. Meltwater rivers make waterfalls down into the sea. (Image: Jørn Henriksen) Rocks of migmatiteRocks of migmatite in Duvefjorden on Nordaustlandet. (Image: Rune Selbekk / Norwegian Polar Institute)

The rock types in Nordaustlandet stem from many different geological eras. The northern part consists of old crystalline basement, with rocks such as marble, quartzite, mica schist, gneiss and granite. East of Lady Franklinfjorden, on the peninsula Botniahalvøya and east of Duvefjorden there are volcanic rocks. In the east and south of Rijpfjorden the bedrock is made up of distinctive red-coloured granite... The Rijpfjord granite is medium grained, and contains two micas (muscovite and biotite) in addition to quartz, plagioclase and pink K-feldspar. It was emplaced in late Silurian times.

Layered gabbro and dolerite of Silurian age occur at Kapp Laura in easternmost Nordaustlandet, on the island of Storøya, and in the eastern part of the island of Kvitøya. On Andréeneset, in the southern part of Kvitøya, gneisses and granites are the most common rock types. Four generations of rocks: gneiss, amfibolite, and grey and pink granite are present on Isispynten, a headland east of Austfonna. South of Wahlenbergfjorden there is a large area with sedimentary rocks – mostly limestone and dolomite – from the Carboniferous and Permian. The youngest rocks in Nordaustlandet are Jurassic–Cretaceous dolerite dikes, which intrude the basement rocks on the island of Lågøya and in the outlet of Brennevinsfjorden.

Unconsolidated deposits in Nordaustlandet consist of scree slopes, block fields and raised shore deposits. There are only small amounts of river deposits. The largest strandflats on Nordaustlandet can be found in the north-west, around Murchisonfjorden and on the island of Lågøya. Another large strandflat is Svartknausflya in the south, just west of the glacier of Bråsvellbreen. Here, there are raised shore deposits up to 120 m.a.s.l., where ancient whale bones have been found 70 m above today’s sea level. Svartknausflya is also the largest moraine area in Nordaustlandet; it measures about 70 km².

Glacial activity has shaped the landscape in Nordaustlandet through several ice ages. Gentle plateaus and rounded mountains are the most common sight. The tallest and steepest mountains, up to 600 m.a.s.l., can be found in the north. The eastern part of Nordaustlandet is covered in glaciers, and there are few areas without ice. Between Vibebukta and Kapp Laura, the steep front of the Austfonna ice cap dominates. The glacier has retracted a bit during recent decades, revealing new areas of dry land on the few headlands that can be found around here (such as Isispynten). Austfonna, including Vegafonna, stretch across an area of 8450 km². Austfonna covers approximately 58% of Nordaustlandet. Vestfonna is 2445 km². The largest areas with no ice are between Austfonna and Vestfonna and on the peninsulas in the north and north-west of Nordaustlandet.

The glacier Bråsvellbreen is a branch of Vestfonna. In 1937-1938 it had one of the largest surges ever recorded in Svalbard. The 30-km wide glacier front 20 km forwards and into the ocean.

Updated June 2015

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