Main dolomite Hauptdolomit Stratigraphic range: Carnian & Norian ages, Late Triassic Epoch, Mesozoic Era |
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Main Dolomite Formation, exposed in the Northern Limestone Alps.
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Type | Geological formation |
Thickness | 0–2,200 metres (0–7,218 ft) |
Lithology | |
Primary | Dolomite (rock) |
Location | |
Region |
Limestone Alps and Apennines ranges, Central Europe |
Main dolomite (also Main Dolomite, German: Hauptdolomit, Italian: Dolomia Principale) is a lithostratigraphic unit in the Alps of Europe.
The formation is found in:
It is primarily made of dolomite rock, ranging 0–2,200 metres (0–7,218 ft) in thickness. The formation was deposited in shallow lagoons during the Late Carnian and Early Norian ages of the Late Triassic epoch in the Triassic Period, during the Mesozoic Era..
Fossil prosauropod tracks have been reported from the formation.