Geology Of Svalbard
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The geology of Svalbard encompasses the geological description of rock types found in
Svalbard Svalbard ( , ), also known as Spitsbergen, or Spitzbergen, is a Norwegian archipelago in the Arctic Ocean. North of mainland Europe, it is about midway between the northern coast of Norway and the North Pole. The islands of the group range ...
, and the associated
tectonics Tectonics (; ) are the processes that control the structure and properties of the Earth's crust and its evolution through time. These include the processes of mountain building, the growth and behavior of the strong, old cores of continents k ...
and
sedimentological Sedimentology encompasses the study of modern sediments such as sand, silt, and clay, and the processes that result in their formation (erosion and weathering), transport, deposition and diagenesis. Sedimentologists apply their understanding of mo ...
history of soils and rocks. The geological exploration of Svalbard is an ongoing activity, and recent understandings may differ from earlier interpretations.


Geological Basement

Geological basement dated from
Precambrian The Precambrian (or Pre-Cambrian, sometimes abbreviated pêž’, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the ...
,
Cambrian The Cambrian Period ( ; sometimes symbolized C with bar, êž’) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million ...
,
Ordovician The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period million years ago (Mya) to the start ...
and
Silurian The Silurian ( ) is a geologic period and system spanning 24.6 million years from the end of the Ordovician Period, at million years ago ( Mya), to the beginning of the Devonian Period, Mya. The Silurian is the shortest period of the Paleozo ...
, originally termed ''Hecla Hoek'', is found in three different provinces. The southwestern terrain comprises
Prins Karls Forland Prins Karls Forland or Forlandet, occasionally anglicized as Prince Charles Foreland, is an island off the west coast of Oscar II Land on Spitsbergen in the Arctic archipelago of Svalbard, Norway. The entire island and the surrounding sea area c ...
,
Oscar II Land Oscar II Land is the land area between Isfjorden and Kongsfjorden on Spitsbergen, Svalbard. The long glacier Sveabreen divides Oscar II Land from James I Land. The area is named after Oscar II of Sweden Oscar II (Oscar Fredrik; 21 January ...
,
Nordenskiöld Land Nordenskiöld Land is the land area between Isfjorden and Van Mijenfjorden on Spitsbergen, Svalbard. The area is named after Finnish-Swedish explorer and geologist Nils Adolf Erik Nordenskiöld. The coastal region of Nordenskiöld Land (Norde ...
west of
Grønfjorden Grønfjorden (English: Green Fjord or Green Harbour) is a 16 km long fjord, separated from Isfjorden to the north by Festningsodden in the west and Heerodden in the east. It lies within the western portion of Nordenskiöld Land. On its eas ...
and
Wedel Jarlsberg Land Wedel Jarlsberg Land is the land area between Van Keulenfjorden and Hornsund on the southwestern part of Spitsbergen, Svalbard. The area is largely covered with glaciers, and is completely within the Sør-Spitsbergen National Park. Named aft ...
. The northwestern terrain includes
Haakon VII Land Haakon VII Land is a land area at the northwestern part of Spitsbergen, Svalbard, between Woodfjorden and Kongsfjorden Kongsfjorden as seen from Blomstrandhalvøya Kongsfjorden (Kongs Fjord or Kings Bay) is an inlet on the west coast of ...
and
Albert I Land Albert I Land is the land area of the northwestern part of Spitsbergen, Svalbard. It is bordered by Haakon VII Land to the southeast. To the northeast lies Raudfjorden and its inner branch, Klinckowströmfjorden, to the southeast Krossfjor ...
. The northeastern terrain comprises
Nordaustlandet Nordaustlandet (sometimes translated as North East Land) is the second-largest island in the archipelago of Svalbard, Norway, with an area of . It lies north east of Spitsbergen, separated by Hinlopen Strait. Much of Nordaustlandet lies under la ...
and the northeastern parts of
Spitsbergen Spitsbergen (; formerly known as West Spitsbergen; Norwegian: ''Vest Spitsbergen'' or ''Vestspitsbergen'' , also sometimes spelled Spitzbergen) is the largest and the only permanently populated island of the Svalbard archipelago in northern Norw ...
.


Devonian

Devonian The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, whe ...
age sediments are exposed in Andrée Land,
James I Land James I Land is a land area on the northwestern part of Spitsbergen, Svalbard. It is named after King James I of England and Scotland. The 30 kilometer long glacier Sveabreen divides James I Land from Oscar II Land Oscar II Land is the land area ...
and
Dickson Land Dickson Land is a land area between Isfjorden and Wijdefjorden Wijdefjord is the longest fjord in Norway's Svalbard archipelago. Wijdefjord is located in the northern portion of the island of Spitsbergen, which lies in the Arctic Ocean about ...
.
Orogeny Orogeny is a mountain building process. An orogeny is an event that takes place at a convergent plate margin when plate motion compresses the margin. An ''orogenic belt'' or ''orogen'' develops as the compressed plate crumples and is uplifted t ...
took place in late Devon.


Carboniferous and Permian

During
Carboniferous The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carbonifero ...
and
Permian The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Paleoz ...
, rift basins were formed. Carboniferous strata are found along
Billefjorden Billefjorden is the central fjord of the three branching from the innermost part of the Isfjorden to the northeast, in Svalbard, Norway. It is 30 km long and 5–8 km wide. Billefjorden lies between Dickson Land to the northwest and Bà ...
, and Permian formations dominate Billefjorden,
Tempelfjorden Tempelfjorden is a fjord branch at the inner end of Sassenfjorden, a part of Isfjorden at Spitsbergen, Svalbard. It is located between Sabine Land and Bünsow Land. The fjord is named after the mountain Templet, which resembles a temple ...
and
Lomfjorden Lomfjorden ( en, The Loon Fjord) is a fjord In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark ...
.


Triassic

Triassic The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period ...
rocks are found at the southern part of
Spitsbergen Spitsbergen (; formerly known as West Spitsbergen; Norwegian: ''Vest Spitsbergen'' or ''Vestspitsbergen'' , also sometimes spelled Spitzbergen) is the largest and the only permanently populated island of the Svalbard archipelago in northern Norw ...
, at
Edgeøya Edgeøya (), occasionally anglicised as Edge Island, is a Norwegian island located in southeast of the Svalbard archipelago; with an area of , it is the third-largest island in this archipelago. An Arctic island, it forms part of the Søraust-S ...
,
Barentsøya Barentsøya, sometimes anglicized as Barents Island, is an island in the Svalbard archipelago of Norway, lying between Edgeøya and Spitsbergen. Barents Island has no permanent human inhabitants. Named for the Dutch explorer Willem Barents (who ...
and
Kong Karls Land Kong Karls Land or King Charles Land is an island group in the Svalbard archipelago, in the Arctic Ocean. The island group covers an area of and is made up of the islands of Kongsøya, Svenskøya, Abel Island, Helgoland Island, and Tirpitzøy ...
. It is particularly visible at Edgeøya, Barentsøya and in eastern part of
Olav V Land Olav V Land is a peninsula in eastern Spitsbergen Island, Svalbard named after Olav V of Norway. It is covered by the Olav V Icefield, measuring about .''Glacier Atlas of Svalbard and Jan Mayen''. 1993. Oslo: Norsk polarinstitutt, p. 32. The o ...
. Triassic outcrops are exposed in a long and narrow belt between pre-Triassic sediments along the west coast and the post-Triassic sediments of the central basin. The Triassic rock units are divided into the Sassendalen Group, dating from Early Triassic to Late Middle Triassic, and the succeeding Kapp Toscana Group.


Jurassic, Cretaceous and Cenozoic

Jurassic The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The J ...
,
Cretaceous The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of th ...
and
Cenozoic The Cenozoic ( ; ) is Earth's current geological era, representing the last 66million years of Earth's history. It is characterised by the dominance of mammals, birds and flowering plants, a cooling and drying climate, and the current configura ...
rocks are exposed in the middle southern part of Spitsbergen. Coal deposits from
Paleogene The Paleogene ( ; British English, also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period, geologic period and system that spans 43 million years from the end of the Cretaceous Period million yea ...
are exploited in Longyearbyen (including
Svea Svea may refer to: Name * Svea (name), Swedish female given name meaning "Swede" * Mother Svea, personification of Sweden * Svea (singer) (Svea Virginia KÃ¥gemark, born 1999), a Swedish singer Places * United States ** Svea, Florida, unincorpor ...
) and
Barentsburg Barentsburg (russian: Баренцбург) is the second-largest settlement in Svalbard, Norway, with about 455 inhabitants (). A coal mining town, the settlement is almost entirely made up of ethnic Russians and Ukrainians. History Rijpsburg ...
. The
post-glacial rebound Post-glacial rebound (also called isostatic rebound or crustal rebound) is the rise of land masses after the removal of the huge weight of ice sheets during the last glacial period, which had caused isostatic depression. Post-glacial rebound a ...
is estimated to be up to three kilometers in central Spitsbergen, while only a few hundred meters at
Kong Karls Land Kong Karls Land or King Charles Land is an island group in the Svalbard archipelago, in the Arctic Ocean. The island group covers an area of and is made up of the islands of Kongsøya, Svenskøya, Abel Island, Helgoland Island, and Tirpitzøy ...
.Ramberg 2006: pp. 476–477


References


Bibliography

* * * *
Svalbard Svalbard ( , ), also known as Spitsbergen, or Spitzbergen, is a Norwegian archipelago in the Arctic Ocean. North of mainland Europe, it is about midway between the northern coast of Norway and the North Pole. The islands of the group range ...
Svalbard {{svalbard-stub