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Viewed in a map today these plutons make up about 15% the Sudetes. [12] [15] Granites are of S-type. [13] The granites and grantic-gneisses of Izera in the west Sudetes are disassociated from orogeny and thought to have formed during rifting along a passive continental margin. [17]
The Western Sudetes (Polish: Sudety Zachodnie; Czech: Krkonošská oblast; German: Westsudeten) are a geomorphological macroregion, the western part of the Sudetes subprovince on the borders of the Czech Republic, Poland and Germany.
Download QR code; Print/export Download as PDF; Printable version; ... Pages in category "Sudetes" The following 56 pages are in this category, out of 56 total.
The Central Sudetes (Czech: Orlická oblast or Střední Sudety, Polish: Sudety Środkowe, German: Mittelsudeten) are the central part of the Sudetes mountain range on the border of the Czech Republic and Poland. They stretch from the Nysa Kłodzka River and the Kłodzko Valley in the east to the upper Bóbr in the west.
The native German-speaking regions in 1930, within the borders of the current Czech Republic, which in the interwar period were referred to as the Sudetenland. The Sudetenland (/ s uː ˈ d eɪ t ən l æ n d / ⓘ soo-DAY-tən-land, German: [zuˈdeːtn̩ˌlant]; Czech and Slovak: Sudety) is a German name for the northern, southern, and western areas of former Czechoslovakia which were ...
The Eastern Sudetes (Polish: Sudety Wschodnie, Czech: Východní Sudety or Jesenická oblast) are the eastern part of the Sudetes mountains on the border of the Czech Republic and Poland. [1] They stretch from the Kłodzko Valley and the Eastern Neisse River in the west down to the Moravian Gate in the east, [ 2 ] [ 3 ] leading to the Outer ...
The Tadeusz Hołdys High-Mountain Meteorological Observatory on Śnieżka [1] (previously used name: Tadeusz Hołdys High-Mountain Observatory on Śnieżka) [2] - an institution of the Institute of Meteorology and Water Management, located on Śnieżka - the highest summit of the Karkonosze and the whole Sudetes, at an altitude of 1602 m.
Sudetes Foothills or Sudeten Foreland [1] (Przedgórze Sudeckie, Czech: Krkonošsko-jesenické podhůří, Sudetské podhůří, Silesian: Przednio ziymia Sudeten, German: Sudetenvorland) is an area (macroregion) located north of the Sudetes proper, being connected with them, but separated from the Sudetes by a distinct tectonic line (Sudetic marginal fault).