File:Caledonian orogeny fold in King Oscar Fjord.jpg

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English: Folding from the Caledonian orogeny on a small rocky island at the mouth of Segelselskapets Fjord into King Oscar Fjord (Jägmästarens Ø). The fold is an recumbent syncline within Upper Precambrian siliciclastic sedimentary rocks (Lyell Land Group, overlain by base of Ymer Ø Group at the rightmost end of the island).[1]
  1. ↑ cf. fig. 27 (p. 28) in Henrik Tirsgaard, Martin Sønderholm: Lithostratigraphy, sedimentary evolution and sequence stratigraphy of the Upper Proterozoic Lyell Land Group (Eleonore Bay Supergroup) of East and North-East Greenland. Geology of Greenland Survey Bulletin, 178, 1–60, doi:10.34194/ggub.v179.5076.
Date
Source D70s through airplane window
Author Håvard Berland
Object location72° 28′ 00.9″ N, 24° 41′ 55.44″ W  Heading=0° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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current14:04, 22 September 2007Thumbnail for version as of 14:04, 22 September 20072,936 × 992 (795 KB)Berland (talk | contribs){{Information |Description= Folding from the Caledonian orogeny where Segelselskapets Fjord mouths into King Oscar Fjord, at 72°28'0.90"N, 24°41'55.44"W |Source= D70s through airplane window |Date= A

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