Category:Fur Formation

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<nowiki>Formazione di Fur; Formation de Fur; Furformationen; Fur Formation; Moler; 富尔组; Fur Formation; formation; 55 millioner år gammelt & 60 m tykt lerlag i den centrale del af Limfjordśområdet; Fur Formation; Fur-Formation; Fur Formationen</nowiki>
Fur Formation 
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LocationNorth Denmark Region, Denmark
Map56° 50′ 16″ N, 8° 57′ 43″ E
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English: The Fur Formation is a marine geological formation of Ypresian (Lower Eocene Epoch, c. 56.0-54.5 Ma) age which crops out in the Limfjord region of Denmark from Silstrup via Mors and Fur (island) to Ertebølle, and can be seen in many cliffs and quarries in the area. The Diatomite Cliffs (moler in Danish) is on the Danish list of tentative candidates for World Heritage and may become a world Heritage site.[1]

The Fur Formation is a unit of diatomitic sediment approximately 60 meters thick consisting of diatoms and clay minerals with up to 180 layers of volcanic ash.[2] In Danish literature the formation has informally been referred to as the moler (Ler means clay). The diatomite comprises 2/3 opal tests of diatoms and 1/3 clay, interbedded with layers of volcanic ash and a few limestone horizons (‘cementstones’), and has exceptionally complete fossil preservation.

It is known for its abundant fossil fish, insects, reptiles, birds and plants. The Fur Formation was deposited just above the Palaeocene-Eocene boundary, about 55 million years ago, and its tropical or sub-tropical flora indicate that the climate after the Paleocene-Eocene Thermal Maximum was moderately warm (approximately 4-8 degrees warmer than today).

Glacial activity has moved and folded all exposed moler in a complicated pattern which permits very precise mapping of glacial movement at the end of the last ice age, and has, due to the ash layers, created an extraordinary pedagogical case for studying tectonics.

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This category has the following 10 subcategories, out of 10 total.

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Media in category "Fur Formation"

The following 45 files are in this category, out of 45 total.