Hierlatz Limestone | |
---|---|
Stratigraphic range: Jurassic | |
Type | Formation |
Lithology | |
Primary | Limestone |
Location | |
Country | Austria |
The Hierlatz Limestone is a geologic formation in Austria. It preserves fossils dated to the Jurassic period. [1] [2]
The Valtos Sandstone Formation is a Middle Jurassic (Bathonian) formation found in the Inner Hebrides of Scotland. It is the thickest member of the Great Estuarine Group. The lithology consists of sets of approximately 6 metre thick cross bedded sandstone, capped by thin shelly limestones containing bivalves of the genus Neomiodon Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.
The Twin Creek Limestone is a geologic formation in Wyoming. It preserves fossils dating back to the Jurassic period.
The Whiteaves Formation is a geologic formation in British Columbia. It preserves fossils dating back to the Jurassic period.
Gibraltar Limestone consists of greyish-white or pale-gray compact, and sometime finely crystalline, medium to thick bedded limestones and dolomites that locally contain chert seams. This formation comprises about three quarters of the Rock of Gibraltar near the southernmost tip of the Iberian peninsula. Geologists have found various poorly preserved and badly eroded and rolled marine fossils within it. The fossils found in the Gibraltar Limestone include various brachiopods, corals, echinoid fragments, gastropods, pelecypods, and stromatolites. These fossils indicate an Early Jurassic age for the deposition of the Gibraltar Limestone.
The Creully Limestone is a geologic formation in France. It preserves fossils dating back to the Jurassic period.
The Lithographic limestones Formation is a geologic formation in France. It preserves fossils dating back to the Jurassic period.
The Weißjura Formation is a Limestone geologic formation located in the Swabian Jura range, Baden-Württemberg, Germany.
The Impressamergel Formation is a geologic formation in Germany. It preserves fossils dating back to the Jurassic period.
The Weissbach Formation is a geologic formation in Austria. It preserves fossils dating back to the Jurassic period.
The Rotgefleckter Liaskalk is a geologic formation in Austria. It preserves fossils dated to the Jurassic period.
The Lärchberg Formation is a geologic formation in Austria. It preserves fossils dated to the Jurassic period.
The Neuburger Bank Formation is a geologic formation in Austria. It preserves fossils dated to the Jurassic period.
The Blassenstein Formation is a geologic formation in Austria. It preserves fossils dated to the Jurassic period.
The Dürrnberg Formation is a geologic formation in Austria. It preserves fossils dated to the Jurassic period.
The Ernstbrunn Formation is a geologic formation in Austria and the Czech Republic. It preserves fossils dated to the Jurassic period.
The Fonsjoch Formation is a geologic formation in Austria. It preserves fossils dated to the Jurassic period.
The Gresten Formation is a geologic formation in Austria. It preserves fossils dated to the Jurassic period.
The Schnöll Formation is a geologic formation of the Adnet Group in Austria. It preserves fossils dated to the Jurassic period.
The Steinalm Formation is a geologic formation in the Northern Limestone Alps, in Austria.
The Oberrhaet Formation, also known as the Oberrhaet Limestone, is a Late Triassic (Rhaetian-age) geological formation in Austria. It is a unit of massive dark grey bioclastic limestones, found within the Northern Calcareous Alps. The Oberrhaet Limestone was originally a series of reefs which developed on the northwest edge of the Eiberg Basin, a narrow marine waterway extending along the northwestern tip of the Neotethys Ocean. The center of the Eiberg Basin is nowadays preserved as the Eiberg Member of the Kössen Formation, which was deposited southeast of the Oberrhaet Limestone and interfingers with it in many areas. The Oberrhaet Limestone was very similar to the Dachstein Limestone, which represented carbonate platforms and reefs on the southeast edge of the Eiberg Basin. The most prominent components of the reefs were giant frond-like colonies of Retiophyllia, a scleractinian coral.
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