molasse

The region where the molasse crops out is divided into two.

Most houses are built of the local molasse stone.

The total thickness of molasse deposits in the basin can be up to 6 kilometers.

The tower was originally built in wood, then in molasse and pebbles like the place.

During this phase the Molasse basin ceased to be an area of net sedimentation.

The municipality's area includes a part of the Swiss plateau's molasse uplands.

The thickness of the molasse increases from west to east (at the same distance from the Alps).

In the Stephanian age molasse occurs, also in basins between mountains.

In this environment the third formation, the Upper Marine Molasse, was formed.

The district encompasses an area that includes a part of the Molasse peaks in the Jorat.

These are known as molasse.

Lithostratigraphically, this molasse is treated as a group that is divided into four formations.

It is considered a classic orogenic molasse.

The river would likely flow as gentry through the molasse as the Sweet Afton.

The resulting erosion resulted in the distinctive molasse that remains of S. thailandicus have been found in.

The basin is eventually filled, and covered with fluvial and alluvial molasse (stage 4).

The resulting molasses are treated to become a sterilized molasse free of impurities, ready to be fermented.

The village is built on a Molasse stone outcropping in the Töss Valley.

The missing Old Red Sandstone mentioned above formed the molasse sediments of stage 4.

The molasse stone was used in Hellenistic Massalia for both the quays and the ramparts.

Patagonian Molasse.

At the end of the 11th century a tower made of light-colored limestone and molasse was erected on the western side of the building.

Coarse sediments from the continual uplift and erosion were later deposited in foreland areas as molasse.

Saar-Nahe Basin is a molasse basin in southwest Germany.

The Central Plateau is mainly composed of molasse, a sedimentary rock which formed at the bottom of the old ocean.