Laacher Lake: Basalt lava flow - Places of Geologic Significance on Waymarking.com

Before the eruption of the pumice vulcano and the collapse of the Laacher caldera a valley has existed into that the lava stream here already donw-flowed. The material of the rocks is Leucite-Nepheline. The liquefied material was not so gassy than lava flows from other eruptions in this area. For this reason the rock is more compact and tough than other basaltic lava. A lava flow is a moving outpouring of lava, which is created during a non-explosive effusive eruption. When it has stopped moving, lava solidifies to form igneous rock.

Waymark is confirmed to be publicly accessible: yes Parking Coordinates: N 50° 24.192 W 007° 15.276 Access fee (In local currency): .00 Requires a high clearance vehicle to visit.: no Requires 4x4 vehicle to visit.: no Public Transport available: yes Website reference: [Web Link]

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