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Manasquan Formation
The Manasquan Formation is a geologic formation in New Jersey. It preserves fossils dating back to the Paleogene period Period may refer to: Common uses * Era, a length or span of time * Full stop (or period), a punctuation mark Arts, entertainment, and media * Period (music), a concept in musical composition * Periodic sentence (or rhetorical period), a concept .... See also * List of fossiliferous stratigraphic units in New Jersey * Paleontology in New Jersey References * Paleogene geology of New Jersey {{NewJersey-geologic-formation-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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Paleogene
The Paleogene ( ; British English, also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period, geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago (annum, Mya) to the beginning of the Neogene Period Mya. It is the beginning of the Cenozoic Era of the present Phanerozoic Eon. The earlier term Tertiary Period was used to define the span of time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognised as a formal stratigraphy, stratigraphic term, 'Tertiary' is still widely found in earth science literature and remains in informal use. Paleogene is often abbreviated "Pg" (but the United States Geological Survey uses the abbreviation PE for the Paleogene on the Survey's geologic maps). During the Paleogene, evolution of mammals, mammals diversified from relatively small, simple forms into a large group of diverse animals in the wake of ...
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Shark River Formation
The Shark River Formation is a geologic formation in Texas. It preserves fossils dating back to the Paleogene The Paleogene ( ; British English, also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period, geologic period and system that spans 43 million years from the end of the Cretaceous Period million yea ... period. See also * List of fossiliferous stratigraphic units in Texas * Paleontology in Texas References * Paleogene geology of Texas Paleogene geology of New Jersey {{Paleogene-stub ...
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Absecon Inlet Formation
Absecon may refer to: Geography * Absecon, New Jersey, a city in Atlantic County, New Jersey **Absecon (NJT station), a New Jersey Transit train station in Absecon, New Jersey *Absecon Highlands, New Jersey, an unincorporated community within Galloway Township *Absecon Inlet, an inlet north of Atlantic City, New Jersey *Absecon Island, on the coast of Atlantic County, New Jersey *Absecon Light, in Atlantic City, New Jersey *Absecon Public School District, in Atlantic County, New Jersey Ships *USCGC Absecon (WAVP-374) The second USS ''Absecon'' (AVP-23) was a United States Navy ''Barnegat''-class seaplane tender in commission from 1943 to 1947, converted during construction to serve as a catapult training ship during World War II. The ship was in commissio ..., later WHEC-374, a United States Coast Guard cutter in commission from 1949 to 1972 * USS Absecon, the name of more than one United States Navy ship {{Disambiguation, geo ...
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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 Wer ...
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New Jersey
New Jersey is a state in the Mid-Atlantic and Northeastern regions of the United States. It is bordered on the north and east by the state of New York; on the east, southeast, and south by the Atlantic Ocean; on the west by the Delaware River and Pennsylvania; and on the southwest by Delaware Bay and the state of Delaware. At , New Jersey is the fifth-smallest state in land area; but with close to 9.3 million residents, it ranks 11th in population and first in population density. The state capital is Trenton, and the most populous city is Newark. With the exception of Warren County, all of the state's 21 counties lie within the combined statistical areas of New York City or Philadelphia. New Jersey was first inhabited by Native Americans for at least 2,800 years, with the Lenape being the dominant group when Europeans arrived in the early 17th century. Dutch and Swedish colonists founded the first European settlements in the state. The British later seized control o ...
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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 New Jersey
This article contains a list of fossil-bearing stratigraphic units in the state of New Jersey, U.S. Sites See also * Paleontology in New Jersey References * {{DEFAULTSORT:Fossiliferous stratigraphic units in New Jersey New Jersey Stratigraphic units A stratigraphic unit is a volume of rock of identifiable origin and relative age range that is defined by the distinctive and dominant, easily mapped and recognizable petrographic, lithologic or paleontologic features (facies) that characterize ... Stratigraphy of New Jersey New Jersey geography-related lists United States geology-related lists ...
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Paleontology In New Jersey
The location of the state of New Jersey Paleontology in New Jersey refers to paleontological research in the US state of New Jersey. The state is especially rich in marine deposits. During the Precambrian, New Jersey was covered by a shallow sea that was home to stromatolite forming bacteria. During the early part of the Paleozoic, the state was still covered by the sea, which was home to creatures like brachiopods and trilobites. By the Silurian, the northern part of the state was home to a river system. Sea levels rose and fell throughout the remainder of the state's Paleozoic rock record. There are no local rocks of Carboniferous or Permian age. During the Triassic, the state was a terrestrial ecoregion. Local lakes were home to the crustacean ''Cyzicus'' and the coelacanth ''Diplurus''. On land, dinosaurs left behind footprints, and continued to do so into the Jurassic. A sea rose over southern New Jersey during the Cretaceous. Invertebrates, plesiosaurs and turtles li ...
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