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Hauge Bjerge Formation
The Hauge Bjerge Formation is a formation of the Peary Land Group in Greenland. It preserves fossils dating back to the Silurian period. See also * List of fossiliferous stratigraphic units in Greenland * Haug Range The Haug Range ( da, Hauge Bjerge) is a mountain range in far northwestern Greenland. Administratively this range is part of Avannaata municipality. The range is located in Hall Land, one of the coldest places in Greenland. This mountain chain w ... References * Silurian Greenland {{Silurian-stub ...
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Formation (stratigraphy)
A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics (lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock exposed in a geographical region (the stratigraphic column). It is the fundamental unit of lithostratigraphy, the study of strata or rock layers. A formation must be large enough that it can be mapped at the surface or traced in the subsurface. Formations are otherwise not defined by the thickness (geology), thickness of their rock strata, which can vary widely. They are usually, but not universally, tabular in form. They may consist of a single lithology (rock type), or of alternating beds of two or more lithologies, or even a heterogeneous mixture of lithologies, so long as this distinguishes them from adjacent bodies of rock. The concept of a geologic formation goes back to the beginnings of modern scientific geology. The term was used by ...
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Silurian
The Silurian ( ) is a geologic period and system spanning 24.6 million years from the end of the Ordovician Period, at million years ago ( Mya), to the beginning of the Devonian Period, Mya. The Silurian is the shortest period of the Paleozoic Era. As with other geologic periods, the rock beds that define the period's start and end are well identified, but the exact dates are uncertain by a few million years. The base of the Silurian is set at a series of major Ordovician–Silurian extinction events when up to 60% of marine genera were wiped out. One important event in this period was the initial establishment of terrestrial life in what is known as the Silurian-Devonian Terrestrial Revolution: vascular plants emerged from more primitive land plants, dikaryan fungi started expanding and diversifying along with glomeromycotan fungi, and three groups of arthropods (myriapods, arachnids and hexapods) became fully terrestrialized. A significant evolutionary milestone during ...
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Haug Range
The Haug Range ( da, Hauge Bjerge) is a mountain range in far northwestern Greenland. Administratively this range is part of Avannaata municipality. The range is located in Hall Land, one of the coldest places in Greenland. This mountain chain was named after Ivar Haug, who compiled the first Gazetteer of Greenland. The area of the range is characterized by Tundra climate. Geography The Haug Range is an up to almost 1,100 m high little glaciated mountain range in Hall Land. It runs roughly from east to west across the peninsula, from the shores of the Nares Strait to the shores of the Newman Bay, separating the unglaciated Polaris Foreland in the north from the southern part of Hall Land. high Kayser Mountain, the highest elevation of the range, is located at its northeastern end. The area of the Haug Range is uninhabited. Google Earth Pentamerus fossils dating back to the Lower Silurian have been found in this mountain range. They belong to the Hauge Bjerge Formation. Se ...
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Greenland
Greenland ( kl, Kalaallit Nunaat, ; da, Grønland, ) is an island country in North America that is part of the Kingdom of Denmark. It is located between the Arctic and Atlantic oceans, east of the Canadian Arctic Archipelago. Greenland is the world's largest island. It is one of three constituent countries that form the Kingdom of Denmark, along with Denmark and the Faroe Islands; the citizens of these countries are all citizens of Denmark and the European Union. Greenland's capital is Nuuk. Though a part of the continent of North America, Greenland has been politically and culturally associated with Europe (specifically Norway and Denmark, the colonial powers) for more than a millennium, beginning in 986.The Fate of Greenland's Vikings
, by Dale Mackenzie Brown, ''Archaeological Institute of America'', ...
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Peary Land Group
The Peary Land Group is a geologic group in Greenland. It preserves fossils dating back to the Silurian period. Formations The following formations are included in the Peary Land Group: * Adams Bjerg Formation * Cape Schuchert Formation *Pentamerus Bjerge Formation * Lafayette Bugt Formation * Hauge Bjerge Formation * Lauge Koch Land Formation * Wulff Land Formation * Merqujoq Formation * Nordkronen Formation * Nyeboe Land Formation * Chester Bjerg Formation * Sydgletscher Formation See also * List of fossiliferous stratigraphic units in Greenland This is a list of fossiliferous stratigraphic units in Greenland. List of fossiliferous stratigraphic units See also * List of fossiliferous stratigraphic units in Antarctica * Lists of fossiliferous stratigraphic units in North America * ... * Pentamerus Bjerge References Geologic groups of Europe Geologic groups of North America Geologic formations of Greenland Silurian Greenland {{Silurian-stub ...
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Fossils
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the absolute ...
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Period (geology)
The geologic time scale, or geological time scale, (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochronology (scientific branch of geology that aims to determine the age of rocks). It is used primarily by Earth scientists (including geologists, paleontologists, geophysicists, geochemists, and paleoclimatologists) to describe the timing and relationships of events in geologic history. The time scale has been developed through the study of rock layers and the observation of their relationships and identifying features such as lithologies, paleomagnetic properties, and fossils. The definition of standardized international units of geologic time is the responsibility of the International Commission on Stratigraphy (ICS), a constituent body of the International Union of Geological Sciences (IUGS), whose primary objective is to precisely define ...
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List Of Fossiliferous Stratigraphic Units In Greenland
This is a list of fossiliferous stratigraphic units in Greenland. List of fossiliferous stratigraphic units See also * List of fossiliferous stratigraphic units in Antarctica * Lists of fossiliferous stratigraphic units in North America ** List of fossiliferous stratigraphic units in the Northwest Territories ** List of fossiliferous stratigraphic units in Nunavut ** List of fossiliferous stratigraphic units in Newfoundland and Labrador * Lists of fossiliferous stratigraphic units in Europe ** List of fossiliferous stratigraphic units in Iceland ** List of fossiliferous stratigraphic units in Norway ** List of fossiliferous stratigraphic units in Russia ** List of fossiliferous stratigraphic units in Svalbard References Bibliography * * * * Further reading * C. B. Skovsted and J. S. Peel. 2011. ''Hyolithellus'' in life position from the Lower Cambrian of north Greenland. Journal of Paleontology 85(1):37-47 * A. C. Daley and J. S. Peel. 2010. A Possible Ano ...
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