GLOSSARY ENTRY (DERIVED FROM QUESTION BELOW) | ||||||
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19:32 Oct 27, 2005 |
German to English translations [PRO] Art/Literary - History / History of the Saarland | |||||||
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| Selected response from: Eckhard Boehle Germany Local time: 05:01 | ||||||
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Summary of answers provided | ||||
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4 +1 | Middle Triassic |
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4 +1 | shell limestone soils |
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3 | shell marl or limestone |
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Muschelkalkböden Middle Triassic Explanation: "Muschelkalk" is correct in English. But you could use "middle triassic soils" as the two are synonymous. Another option may be lime soils or soils (based) on limestone bedrock or country rock. |
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Muschelkalkböden shell marl or limestone Explanation: shell[y] marl o. lime[stone] ... which is primarily a grayish-green, silty, sandy, shell marl with imbedded layers and lenses of sand, ... marl. and limestone, which alternate with beds of marine shell marl ... www.sfwmd.gov/org/exo/ftmyers/report-text/volb/ch_2_studyar... More pages from sfwmd.gov geology The formation of Big Cypress goes back through geologic time to when the Florida peninsula was covered by the ocean. As oceanic debris was deposited on the sea floor, limestone began to form. ... formations are dolomite overlaid with freshwater marl, limestone, shell marl. This shows how the land here ... |
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Muschelkalkböden shell limestone soils Explanation: ... is probably what you are looking for. http://www.schmitts-kinder.com/: The warm shell limestone soils of Randersacker give the wine its special characteristics. http://www.winesforfood.com/TheWine.asp?ID=61&C=A: Bright, refined, always tasteful, Little Baron Riesling has been raised on the same ancient shell limestone soils, schlepped upon by his estimable ancestors down through the mists of Mosellian history. At casual gatherings, the delightfully diminutive Little Baron displays all the freshness and wide-eyed promise of youth. http://en.wikipedia.org/wiki/Muschelkalk: Muschelkalk (German for "Mussel chalk") is the term in geology for the middle member of the German Triassic. It consists of a series of calcareous, many and dolomitic beds which lie conformably between the Bunter and Keuper formations. The name Muschelkalk (Fr., calcaire coquillier; concijylien, formation of D'Orbigny) indicates a characteristic feature in this series, viz, the frequent occurrence of lenticular banks composed of fossil shells, remarkable in the midst of a singularly barren group. In its typical form the Muschelkalk is practically restricted to the German region and its immediate neighborhood; it is found in Thuringia, Harz, Franconia, Hesse, Swabia, and the Saar and Alsace districts. Northward it extends into Silesia, Poland and Heligoland. Representatives are found in the Alps, west and south of the Vosges, in Moravia, near Toulon and Montpellier, in Spain and Sardinia; in Romania, Bosnia, Dalmatia, and beyond this into Asia in the Himalayas, China, Australia, California, and in North Africa (Constantine). HTH |
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