Siljan Ring

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A satellite photograph of the Siljan Ring. Lake Siljan takes up a large part of the southwestern edge of the now much-eroded crater.

The Siljan Ring (Swedish: Siljansringen) is a prehistoric impact crater in Dalarna, central Sweden.[1] It is one of the 18 largest known impact craters on Earth and the largest in Europe, with a diameter of about 52 km (32 mi). The impact that created the Siljan Ring occurred when a meteorite collided with the Earth's surface during the Devonian period, about 377 million years ago.[2] The effects of the impact can clearly be seen in the bedrock in the area. The Cambrian, Ordovician and Silurian sedimentary rocks deformed by the impact are rich in fossils.

The area around the Siljan Ring has been the site of recent prospecting for oil and natural gas, though none of the projects has so far been commercially viable. There are large deposits of lead and zinc near Boda at the western edge of the Ring.

There are several lakes in the vicinity, the largest of which is Siljan on the south-southwestern edge of the crater, with the smaller Lake Orsa to the west and Skattungen and Ore on the northeastern margin.

Geology[edit]

The Siljan Ring consist of an annular outcrop of Lower Paleozoic sedimentary rocks within Proterozoic granites of the Dala series.[3]

Basement rocks[edit]

In Dalarna the basement rocks consist of granites dated as 1.6 billion years old, putting them at the boundary between the Paleoproterozoic and the Mesoproterozoic. They were emplaced shortly after the Sveckokarelian orogeny.[4]

Sedimentary rocks[edit]

The oldest sedimentary rocks that outcrop in the Siljan area are of Ordovician age. The sequence is dominated by limestone formations with one prominent black shale, the Fjäcka Shale, which is bituminous and has generated petroleum, sourcing the oil found in limestone cavities in the same area.[3] The Ordovician sequence is overlain by rocks of the Llandovery series (Lower Silurian) .[5]

Glaciation[edit]

During the last ice age the area was covered by a thick icesheet. The bedrock was sculpted by the ice, with the softer Palaeozoic sedimentary rocks being preferentially eroded. These erosional hollows are now occupied by lakes Siljan, Orsa, Skattungen and Ore.[3]

Oil and gas prospecting[edit]

In accordance with theories about abiogenic petroleum (that hydrocarbons can be created without involving material from dead plants and animals), astrophysicist Thomas Gold suggested that there might be major deposits of oil and natural gas in the area. Drilling was carried out in the late 1980s and early 1990s but proved unsuccessful.[1] Drilling for natural gas was resumed in the late 2000s and continue as of mid-2012. The scientific premise for prospecting of this sort is based on the work of physicist Vladimir Kutcherov, who is cooperating with Igrene, the company financing the drilling operations.[6]

Notes[edit]

  1. ^ a b Glasby (2006), Gold (1992)
  2. ^ "Siljan". Earth Impact Database. University of New Brunswick. Retrieved 2007-02-19. 
  3. ^ a b c Ebbestad, J.O.R.; Högström A.E.S. (2007). "Ordovician of the Siljan District, Sweden". IGCP503 Ordovician Palaeogeography and Palaeoclimate Regional Meeting 2007. Sveriges geologiska undersökning. pp. 7–22. Retrieved 12 July 2012. 
  4. ^ Kenkmann, T.; von Dalwigk I. (2000). "Radial transpression ridges: A new structural feature of complex impact craters". Meteoritics and Planetary Science (Meteoritical Society) 35: 1189–1201. Bibcode:2000M&PS...35.1189K. doi:10.1111/j.1945-5100.2000.tb01508.x. Retrieved 12 July 2012. 
  5. ^ Bergström, S.M.; Toprak F.Ö., Huff W.D. & Mundil R. (2008). "Implications of a new, biostratigraphically wellcontrolled, radio-isotopic age for the lower Telychian Stage of the Llandovery Series (Lower Silurian, Sweden)". Episodes 31 (3): 309–314. Retrieved 12 July 2012. 
  6. ^ Bo Joffer, "Igrene förlänger runt Siljansringen, DT.se, 26 June 2012 (in Swedish). Accessed 13 July 2012."

References[edit]

External links[edit]

Coordinates: 61°02′N 14°55′E / 61.04°N 14.92°E / 61.04; 14.92