description Strohn Maar Overview
Strohn Maar is a dry volcanic crater located near the village of Strohn in the Eifel region of western Germany, an area known for its Pleistocene-era volcanic features including numerous maars. The maar was formed by a phreatomagmatic eruption and is now dry rather than containing a lake, unlike some other Eifel maars such as the nearby Meerfelder Maar. The surrounding area features pyroclastic deposits characteristic of maar-forming eruptions. Strohn is also known for a large volcanic bomb, estimated at over 100 tons, found nearby and displayed as a geological landmark.
help Strohn Maar FAQ
Where is Strohn Maar located?
Strohn Maar is near the village of Strohn in western Germany's Eifel region. The Eifel is known for its many volcanic landforms.
How was Strohn Maar formed?
Strohn Maar formed through a phreatomagmatic eruption. It is a volcanic crater rather than a cave or an ordinary depression.
Is Strohn Maar a lake?
No. Strohn Maar is a dry volcanic crater, so it does not contain a lake today.
What is the connection between Strohn Maar and Pleistocene volcanism?
The crater lies in the Eifel, an area known for Pleistocene-era volcanic features including numerous maars. Strohn Maar is one of the region's dry maar formations.
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