Muschelkalk
Sign in to saveThe Muschelkalk (German for "shell-bearing limestone", ) is a sequence of sedimentary rock strata (a lithostratigraphic unit) in the geology of central and western Europe. It has a Middle Triassic (240 to 230 million years) age and forms the middle part of the three-part Germanic Trias (that gives the Triassic its name) lying above the older Buntsandstein and below the younger Keuper. The Muschelkalk ("mussel-chalk") consists of a sequence of limestone and dolomite beds.
In the Vinony graph
Within Vinony's link graph, Muschelkalk is referenced by 249 other articles, and connects out to halite, Tethys Ocean and bed.
Vinony files it under Geology of Germany, Limestone and Lithostratigraphy.
Its subject is documented across 15 Wikipedia language editions.
Wikidata facts
- Instance of
- lithostratigraphic unit
- Named after
- shelly limestone
- Country
- Netherlands
- Material used
- shelly limestone
- Image
- Muschelkalk am Simmelsberg 2.JPG
Show 4 more facts
- Commons category
- Muschelkalk
- overlies
- Buntsandstein
- underlies
- Keuper Group
- described by source
- Encyclopædia Britannica 11th edition
Sources (1)
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Encyclopedic overview
7 sectionsContents
- Occurrence
- Stratigraphy
- Germany
- Fossil content
- Exploration
- See also
- References
The Muschelkalk (German for "shell-bearing limestone", ) is a sequence of sedimentary rock strata (a lithostratigraphic unit) in the geology of central and western Europe. It has a Middle Triassic (240 to 230 million years) age and forms the middle part of the three-part Germanic Trias (that gives the Triassic its name) lying above the older Buntsandstein and below the younger Keuper. The Muschelkalk ("mussel-chalk") consists of a sequence of limestone and dolomite beds.
In the past, the time span in which the Muschelkalk was deposited could also be called "Muschelkalk". In modern stratigraphy, however, the name only applies to the layers of rock.
Excerpted from Wikipedia’s “Muschelkalk” article, available under the CC BY-SA 4.0 licence.
Gallery (3)
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