The following tables list the global geological sites where tracks of theropod dinosaurs have been found, together with the proper names of the rock formations ( stratigraphic units ) that contain them.
Name | Age | Location | Description |
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Pliensbachian | Up to 1350 tracks, most of them currently undescribed. Includes small, medium and large theropods. [2] | ||
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An isolated, 14 cm long tridactyl footprint of a coelophysoid theropod dinosaur, late Triassic age. | |||
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Time | Description | ||
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Callovian [30] | Description | ||
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Early Jurassic | Tracks of Prosauropoda indet., Theropoda indet., Tetrapodium elmenhorsti , Saurichnium anserinum , S. damarense, S. parallelum & S. tetractis in an aeolian environment | ||
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Middle Norian [48] | Description | ||
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Late Berriasian to Valanginian [60] | Description | ||
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Early Maastrichtian [63] | Description | ||
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Sinemurian to Pliensbachian | Description | ||
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Late Maastrichtian [76] | Description | ||
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Time | Description | ||
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Pliensbachian to Toarcian [86] | Description | ||
Early Maastrichtian [87] | - has a few alternate spellings | ||
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Carnian [91] | Description | ||
Pliensbachian to Toarcian [92] | Description | ||
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Middle Norian [102] | Description | ||
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Cenomanian [106] | |||
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Magister militum was a top-level military command used in the late Roman Empire, dating from the reign of Constantine the Great. The term referred to the senior military officer of the empire. In Greek sources, the term is translated either as strategos or as stratelates.
Area codes 705, 249, and 683 are telephone area codes in the North American Numbering Plan (NANP) for most of northeastern and central Ontario in Canada. Area code 705 was created in a 1956 area code split from portions of the 613 and 519 numbering plan areas. After a reduction in geographic coverage in 1962, the numbering plan area was assigned a second area code, 249, in 2011 to form an overlay numbering plan. A third area code, 683, was added in June 2022.
Area codes 905, 289, 365, and 742 are telephone area codes in the North American Numbering Plan (NANP) for the Golden Horseshoe region that surrounds Lake Ontario in Southern Ontario, Canada. The numbering plan area (NPA) comprises (clockwise) the Niagara Peninsula, the city of Hamilton, the regional municipalities of Halton, Peel, York, Durham, and parts of Northumberland County, but excludes the City of Toronto.
Area codes 519, 226, 548, and 382 are overlay telephone area codes in the North American Numbering Plan (NANP) for most of southwestern Ontario.
Area code 701 is a telephone area code in the North American Numbering Plan (NANP) for the U.S. State of North Dakota. It is one of the 86 original North American area codes created by AT&T in 1947, and continues to be the only area code in North Dakota, one of eleven states with only one area code.
Area codes 208 and 986 are telephone area codes in the North American Numbering Plan for all of Idaho. Area code 208 is one of the 86 original area codes created by the American Telephone and Telegraph Company (AT&T) in 1947, and was Idaho's sole area code for seventy years. In 2017, 986 was added as a second area code to the same numbering plan area by creating an overlay complex.
The following is a complete list of cases decided by the United States Supreme Court organized by volume of the United States Reports in which they appear. This is a list of volumes of U.S. Reports, and the links point to the contents of each individual volume. Each volume was edited by one of the Reporters of Decisions of the Supreme Court. As of the beginning of the October 2019 Term, there were 574 bound volumes of the U.S. Reports. There were another 14 volumes worth of opinions available as "slip opinions", which are preliminary versions of the opinion published on the Supreme Court's website.
The Löwenstein Formation is a lithostratigraphic formation of the Keuper in Germany. It is underlain by the Mainhardt Formation and overlain by the Trossingen Formation. It dates back to the middle Norian.
The Guettioua Formation is a geological formation in Morocco. It dates back to the Middle Jurassic. It largely consists of sandstone, and is of continental origin. It is the lateral equivalent of the marine El Mers Formation.