zechstein वाक्य
उदाहरण वाक्य
मोबाइल
- The bulging of the saddle occurred as a result of the movement of Malm Salt ( not Zechstein Salt ) deep underground that forced the overlying, younger layers of solid rock upwards.
- These are the Rotliegend, Zechstein ( both of Permian age ), Buntsandstein, Muschelkalk, Keuper ( Triassic in age ), ICS does not contain any of these names any longer.
- The nature park covers parts of the southern foothills of the Lower Harz, the gypsum karst landscape of the adjacent Zechstein belt and the transition region with the North Thuringian bunter sandstone country.
- The Taognathus lived in South Africa during the Tatarian Age, Lopingian Subepoch, Zechstein Epoch, in the Late Permian, and was named by Scottish South African doctor and paleontologist Robert Broom in 1911.
- The cutting exposes a section of late Permian Ford Formation ( Zechstein ) dolomite in which the transition from the flat to the crest of the shelf-edge of an ancient reef is clearly visible.
- Just above the base of the Zechstein formation is a fairly thin layer of shale, or slate, where it has been metamorphized, known as the " kupferschiefer " for its high copper content.
- At that time the edges of the Rhine Graben were uplifted and the layers of bunter sandstone and, in places also older rocks ( Zechstein, Rotliegendes ) were exposed after the overlying rock was eroded away.
- He also noted the large labyrinthodonts of the Keuper ( a unit of rocks that dates to the Late Triassic ) were younger than more advanced reptiles in the Magnesian and Zechstein, which are Late Permian in age.
- Under the serial number 340 were included the open high plateaus made of Zechstein and Bunter sandstone of the Waldeck Plain ( 340 1 ) and the adjacent thickly wooded Bunter sandstone ridge of the Waldeck Forest ( 340 2 ).
- It is oriented roughly parallel to the Thuringian Forest and, while a separate structure, is geologically very similar to the latter, as it consists of the same rock types such as granite, hornfels, porphyrites, Rotliegend and Zechstein sediments, and thus forms part of the Variscan chain.
- Mineral layers that do not reach the surface here are the Lower Bunter, running from a depth of some 90 m underneath the town ( about 110 m above sea level ) down to some 390 m farther down, and, following at yet greater depths, Upper and Lower Zechstein from the Permian.
- The Hessian Highlands correspond to the geological structural unit known as the Hessian Depression ( " Hessischen Senke " ) in its broader sense, because here geologically young layers of Zechstein and Bunter sandstone, and in places even younger rocks like Muschelkalk, of the Jurassic, Paleogene and Neogene periods, have been preserved.
- The West and East Hesse Highlands together form the " Hesse Highlands " and correspond to the geological unit of the " Hesse Depression " in its wider sense, because geologically recent layers of Zechstein and Bunter sandstone, and in places even younger Muschelkalk rocks, from the lower Jurassic and Tertiary periods have been preserved here.
- The West and East Hesse Highlands or " Hesse Highlands " correspond to the geological unit known as the Hesse Depression ( " Hessischen Senke " ), in its wider sense, because here geologically young layers of Zechstein and Bunter sandstone, and in places even younger rocks like Muschelkalk, of the Jurassic, Paleogene and Neogene periods, have been preserved.
- The outcropping Mesozoic platform at the surface comprises Zechstein ( Middle / Late Permian ) marine gypsum rocks and limestones, Buntsandstein ( Early Triassic ) siliciclastic rocks, Muschelkalk ( Middle Triassic ) marine limestones, Keuper ( Middle and Late Triassic ) mixed evaporite-carbonate-siliciclastic deposits, Early Jurassic ( Lias / Schwarzjura ) marine black shales, Dogger / Braunjura ( Middle Jurassic ) marine, often iron-bearing, siliciclastic rocks, White Jurassic / Malm ( Late Jurassic ) marine limestones, Early Cretaceous ( Wealden ) continental siliciclastic rocks and Late Cretaceous marine limestones, sandstones and gaizes.
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