muschelkalk

The Muschelkalk in the other tunnel also required special care.

A part is built on lower and middle muschelkalk.

Not visible is muschelkalk in the interior of the summit block.

The region forms part of the larger Muschelkalk geological zone.

Creuzburg is in the area known as the Muschelkalk.

Once the middle series in the Triassic was known as the Muschelkalk.

Middle Muschelkalk is found in the transition areas.

The gau landscape is mainly characterised by heavy muschelkalk soils.

Species of orchid abound on the open Muschelkalk slopes.

In 1625, 13 families lived on the island, making a living from farming, fishing and the production of muschelkalk or shell-bearing limestone.

The kuppen and plateaux rest directly on a bedrock of muschelkalk.

Later, during the Zechstein and Muschelkalk the region was largely flooded by the sea.

The most striking feature is the muschelkalk which characterises the exterior façade.

The hill is largely formed of muschelkalk.

This specimen is from the Muschelkalk of Germany.

The specimen originated in the Muschelkalk, which was deposited in a shallow sea.

Stylolites are common in all the Muschelkalk limestones.

Furthermore, the Muschelkalk soil is not very fertile and is often used as pasture for cattle.

It was built on a rocket of Muschelkalk (Middle Trias).

Again the keuper escarpment is missing and even the muschelkalk only appears in islands around individual domes.

On the sometimes very steep hills alongside the Main river the soil mainly consists of Muschelkalk.

It is located in the Westerberg area of the city in a former Muschelkalk quarry.

Of course these rocks have little history in common with the central European Muschelkalk except for similarities in fossil content.

The lithostratigraphic status of the Muschelkalk differs regionally.

Due to its karstified muschelkalk bedrock, the Heckengäu is a dry, edaphic region.