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Cass Fjord Formation
The Cass Fjord Formation is a geologic formation in Greenland. It preserves fossils dating back to the Ordovician period. The Cass Fjord is a geographic feature at the northern end of Peabody Bay on the eastern side of the Kane Basin in northwestern Greenland. 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 ... References Ordovician Greenland {{Ordovician-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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Ordovician
The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era, and the second of twelve periods of the Phanerozoic Eon (geology), Eon. The Ordovician spans 41.6 million years from the end of the Cambrian Period Megaannum, Ma (million years ago) to the start of the Silurian Period Ma. The Ordovician, named after the Celtic Britons, Welsh tribe of the Ordovices, was defined by Charles Lapworth in 1879 to resolve a dispute between followers of Adam Sedgwick and Roderick Murchison, who were placing the same Rock (geology), rock beds in North Wales in the Cambrian and Silurian systems, respectively. Lapworth recognized that the fossil fauna in the disputed Stratum, strata were different from those of either the Cambrian or the Silurian systems, and placed them in a system of their own. The Ordovician received international approval in 1960 (forty years after Lapworth's death), when it was adopted as an official per ...
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Cass Fjord
Cass Fjord is a fjord in northern Greenland. To the southwest, the fjord opens into the Kane Basin of the Nares Strait. Geography The Cass Fjord opens to the SW at the northern end of Peabody Bay, north of Cape Clay. Cass Fjord forms Washington Land's southeastern coastline and the facing shore is part of Daugaard-Jensen Land.GoogleEarth The Washington Land shore is fringed by high cliffs, known as ''Poulsens Klint''.''Prostar Sailing Directions 2005 Greenland and Iceland Enroute,'' p. 92 See also *List of fjords of Greenland This is a list of the most important fjords of Greenland:In Greenland, Northern Greenland, a large area made up entirely of fjords; therefore Peary Land above not a fjord but a fjord area.In Greenland, Northeastern Greenland, a large area made ... * Cass Fjord Formation References External linksStratigraphy of the Cass Fjord Formation (Middle and Upper Cambrian), North Greenland Fjords of Greenland {{Greenland-fjord-stub ...
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Greenland
Greenland is an autonomous territory in the Danish Realm, Kingdom of Denmark. It is by far the largest geographically of three constituent parts of the kingdom; the other two are metropolitan Denmark and the Faroe Islands. Citizens of Greenland are full Danish nationality law, citizens of Denmark and European Union citizenship, of the European Union. Greenland is one of the Special territories of members of the European Economic Area#Overseas countries and territories, Overseas Countries and Territories of the European Union and is part of the Council of Europe. It is the List of islands by area, world's largest island, and lies between the Arctic Ocean, Arctic and Atlantic oceans, east of the Arctic Archipelago, Canadian Arctic Archipelago. It is the location of the northernmost point of land in the world; Kaffeklubben Island off the northern coast is the world's Northernmost point of land, northernmost undisputed point of land—Cape Morris Jesup on the mainland was thought to ...
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Formation (geology)
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 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 Abraham Gottlob ...
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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''. Though the fossil record is incomplete, numerous studies have demonstrated that there is enough information available to give a good understanding of the pattern of diversification of life on Earth. In addition, the record can predict and fill gaps such as the discovery of '' Tiktaalik'' in the arctic of Canada. Paleontology includes the study of fossils: their age, method of formation, and evolutionary significance. Specimens are sometimes considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years to 4.1 billion years old. Early edition, published online before print. ...
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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 (a 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 standardised international units of geological 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 ...
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Peabody Bay
Peabody Bay () is a large bay in northwestern Greenland. Administratively it is part of Avannaata municipality. Geography Peabody Bay is located on the eastern side of the Kane Basin off the western end of the Humboldt Glacier. Cape Forbes and the Cass Fjord Cass Fjord is a fjord in northern Greenland. To the southwest, the fjord opens into the Kane Basin of the Nares Strait. Geography The Cass Fjord opens to the SW at the northern end of Peabody Bay, north of Cape Clay. Cass Fjord forms Washingt ... lie at the northern end of the roughly 80 km wide bay. The McGary Islands lie at the southern end of the bay and the Bonsall Islands lie between that end and Dallas Bay to the SW. Elisha Kane —whose Arctic venture in search of the lost Franklin expedition crossed the area in 1854— had named the Kane Basin itself "Peabody Bay," in honor of philanthropist George Peabody, the major funder of Kane's expedition. Currently, however, Peabody Bay is this smaller bay at the ...
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Kane Basin
Kane Basin (; ) is an Arctic waterway lying between Greenland and Ellesmere Island, Canada's northernmost. It links Smith Sound to Kennedy Channel and forms part of Nares Strait. It is approximately in length and at its widest. It is named after the American explorer Elisha Kent Kane, whose expedition in search of Franklin's lost expedition crossed it in 1854. Kane himself had named it "Peabody Bay," in honor of philanthropist George Peabody, the major funder of Kane's expedition. Currently Peabody Bay is a bay at the eastern side of the basin, off the southwestern end of the Humboldt Glacier Humboldt Glacier () is one of the major glaciers in northern Greenland. The glacier is named after German naturalist Alexander von Humboldt and is the widest tidewater glacier in the Northern Hemisphere. Geography The Humboldt Glacier borders ... in northern Greenland. Further reading * Cold Regions Research and Engineering Laboratory (U.S.). ''Radar Imagery of Arctic Pack Ice Ka ...
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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 Pos ...
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