⇄ 

Übersetzung für 'muschelkalk' von Englisch nach Deutsch

muschelkalk

Muschelkalk {m} [geol. Formation]geol.

---

Muschelkalk Formation

Muschelkalkformation {f}geol.

• Muschelkalk {m} [geol. Formation] = muschelkalk
• Muschelkalk {m} = coquina
• Muschelkalk {m} = shell limestone

• On the southeastern boundary of the district, between Ohrdruf and Mühlberg, is the muschelkalk Ohrdrufer Plateau which sits at an average of about 450 meters (1,436 ft).
• The municipality is mainly built on red sandstone. A part is built on lower and middle muschelkalk.
• In the 9th century in the southeastern Odenwald near the now more thickly settled Bauland, settlements were established. The muschelkalk-new red sandstone mineral boundary was crossed.
• After emerging from the Black Forest, the Enz flows down to its mouth in the Neckar Gäu country in the muschelkalk beds of the South German Scarplands.
• Around Wollersheim is a geological and botanical feature: the muschelkalk "kuppen", which are home to numerous rare species of limestone pastures.

• The "Großalmerode Graben Zone" in the north lies on a narrow muschelkalk nappe.
• The lake, which only contains water when there is a high water table, lies in a hollow, a muschelkalk-karst basin.
• In these muschelkalk hills lies the Pyrmont Basin ("Pyrmonter Talkessel") on the fault lines of which mineral and brine springs rise, and to which the town of Bad Pyrmont owes its status as a spa town.
• The hill is largely formed of muschelkalk.
• As it was uplifted, the horizontal strata of the surrounding area, mainly consisting of muschelkalk, were tilted.

• Today the river forms the typically narrow valley shape of a gorge ("Klamm") in the area of the muschelkalk rocks, while the areas of softer Partnach strata to the north and south have a wider valley cross-section.
• A hiatus in the strata between the lias and the Lower Cretaceous and the discordant, overlapping layering of the Upper Cretaceous up to the muschelkalk indicate that activity took place at different times, particularly on the Northern Harz Boundary Fault.
• Clearly different from the aforementioned ridges is the eastern slope of the Long Rhön, which forms the transition zone from the High Rhön to the muschelkalk region of the Mellrichstadt Gäu ("Mellrichstädter Gäu"), the eastern part of the Werra Gäu Plateaux.
• The Franconian Keuper-Lias Plains are bounded to the north and west by the muschelkalk Gäu landscapes of the Main-Franconian Plateaux, to the southwest, of which, are the Gäu Plateaus.
• It is physically located on the Stromberg, where its loess-covered keuper and muschelkalk hills meet the flat and dry [...].