Cambro-Silurian

Cambro-Silurian
кембро-силурийский

English-Russian dictionary of geology. 2011.

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  • Ordovician–Silurian extinction event — …   Wikipedia

  • Massif Central (geology) — The Massif Central forms together with the Armorican Massif (Brittany and Normandy) one of the two big basement massifs in France. Its geological evolution started in the late Neoproterozoic and continues to this day. It has been shaped mainly by …   Wikipedia

  • Baltic Shield — The Baltic Shield (sometimes referred to as the Fennoscandian Shield) is located in Fennoscandia (Norway, Sweden and Finland), northwest Russia and under the Baltic Sea. The Baltic Shield is defined as the exposed Precambrian northwest segment of …   Wikipedia

  • Malmøya — Winter picture from East side of Malmoya, showing the old steamship pier. Malmøya is an island situated only 3 kilometres outside Oslo the capital of Norway. The island is mostly known for its large quantities of fossils from the Cambro Silurian… …   Wikipedia

  • Hardangervidda — Infobox protected area | name = Hardangervidda National Park iucn category = II caption = Hardangervidda landscape locator x = locator y = location = Buskerud, Hordaland, and Telemark, Norway nearest city = Bergen lat degrees = 60 lat minutes = 3 …   Wikipedia

  • Marcellus Formation — Stratigraphic range: Middle Devonian …   Wikipedia

  • GEOGRAPHICAL SURVEY — Names The name Ereẓ Israel (the Land of Israel) designates the land which, according to the Bible was promised as an inheritance to the Israelite tribes. In the course of time it came to be regarded first by the Jews and then also by the… …   Encyclopedia of Judaism

  • Mulde event — Key events of the Silurian view • edit 445 …   Wikipedia

  • Extinction event — …   Wikipedia

  • Ireland — This article is about the island. For the sovereign state of the same name, see Republic of Ireland. For the constituent country of the United Kingdom, see Northern Ireland. For other uses, see Ireland (disambiguation). Coordinates …   Wikipedia

  • Windermere supergroup — The Windermere supergroup is a geological unit formed during the Ordovician to Silurian periods Ma|450, and exposed in the north west of England, including the Pennines and correlates along its strike, in the Isle of Man and Ireland, and down dip …   Wikipedia


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