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List Of Fossiliferous Stratigraphic Units In Virginia
This article contains a list of fossil-bearing stratigraphic units in the state of Virginia, U.S. Sites See also * Paleontology in Virginia References * {{DEFAULTSORT:Fossiliferous stratigraphic units in Virginia Virginia 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 Virginia Virginia geography-related lists United States geology-related lists ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratigraphic Units
A stratigraphic unit is a volume of Rock (geology), rock of identifiable origin and relative age range that is defined by the distinctive and dominant, easily mapped and recognizable petrology, petrographic, lithology, lithologic or paleontology, paleontologic features (facies) that characterize it. Units must be ''mappable'' and ''distinct'' from one another, but the contact need not be particularly distinct. For instance, a unit may be defined by terms such as "when the sandstone component exceeds 75%". Lithostratigraphic units Sequences of sedimentary rock, sedimentary and volcanic rocks are subdivided the basis of their shared or associated lithology. Formally identified lithostratigraphic units are structured in a hierarchy of lithostratigraphic rank, higher rank units generally comprising two or more units of lower rank. Going from smaller to larger in rank, the main lithostratigraphic ranks are Bed, Member, Formation, Group and Supergroup. Formal names of lithostratigraph ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bowen Formation
The Bowen Formation is an Ordovician-age geological formation in the Appalachian region of the eastern United States. It occupies a thin stratigraphic range between the Wardell and Witten formations in some areas of southwest Virginia and northeast Tennessee. It is particularly well-exposed in Tazewell County, Virginia. Unlike its encompassing strata, the Bowen Formation is mostly calcareous sandstone and mudrock rather than limestone. The thicker upper part of the formation is composed of layered red mudrock which is replete with mudcracks. The thinner lower part, which is not always preserved, is a coarser unit of dark grey stratified sandstone which weathers to a rusty-brown color. Fossils are rare, restricted to stromatolites and ''Tetradium fibratum'' (a coral-like colonial organism). The Bowen Formation was probably formed by a small lobe of a delta flowing northeast onto the carbonate platforms of the area. Mudcracks indicate that the sediments were partially exposed to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Choptank Formation
The Choptank Formation is a geologic formation in Virginia and Maryland. It preserves fossils dating from the Miocene epoch of the Neogene period. Fossils The Choptank Formation is extremely fossiliferous. Some of the fossil species represented include the following: Sharks *''Otodus megalodon'' *''Carcharodon hastalis'' *'' Isurus oxyrhincus'' *Carcharomodus escheri *'' Physogaleus contortus'' *''Galeocerdo aduncus'' *''Carcharhinus'' *''Hemipristis serra'' *'' Squatina sp.'' *'' Notorhyncus cepedianus'' *''Carcharias'' *'' Isurus retroflexus'' *'' Parotodus benedeni'' *''Alopias vulpinus'' *'' Alopias grandis'' *''Cetorhinus'' *'' Negaprion brevirostris'' *''Rhizoprionodon'' *'' Sphryna laevissima'' Rays and Other Cartilaginous Fish *''Aetobatus arcuatus'' *'' Pteromyaleus sp.'' *''Dasyatis rugosa'' *''Dasyatis probsti'' *'' Pinthicus stenodon'' Fish *''Acipenseridae indet.'' *''Opsanus sp.'' *''Serranidae sp.'' *'' Pogonias sp.'' *''Sciaenops sp.'' *''Tautoga sp.'' *''Acanth ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calvert Formation
The Calvert Formation is a geologic formation in Maryland, Virginia, and Delaware. It preserves fossils dating back to the early to middle Miocene epoch of the Neogene period. The formation is a destination for amateur fossil hunters as well as professional paleontologists. It is one of the three formations which make up the Calvert Cliffs, all of which are part of the Chesapeake Group. Fossils The Calvert Formation is extremely fossiliferous. Some of the fossil species represented include the following: Sharks * ''Otodus megalodon'' * ''Otodus chubutensis'' * ''Carcharodon hastalis'' * '' Isurus oxyrhincus'' * '' Physogaleus contortus'' * '' Physogaleus hemmooriensis'' * ''Galeocerdo aduncus'' * '' Carcharhinus'' * ''Hemipristis serra'' * '' Squatina sp.'' * ''Squalus sp.'' * '' Echinorhinus blakei'' * '' Notorhyncus cepedianus'' * '' Hexanchus gigas'' * '' Carcharias'' * ''Carcharoides catticus'' * '' Isurus retroflexus'' * '' Parotodus benedeni'' * ''Alopias vulpinus'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chepultepec Formation
The Chepultepec Formation, is an Early Ordovician-age geological formation in the Appalachian regions of Eastern North America. Also known as the Chepultepec Dolomite, it is a unit of the Upper Knox Group, overlying the Copper Ridge Dolomite and underlying the Longview- Kingsport-Mascot sequence. The Chepultepec Formation is a primarily limestone and dolomite formation, the earliest formation of the Ordovician period in its area. Further north, it is equivalent to the Stonehenge Formation of the Beekmantown Group. The formation was first described from Allgood, Alabama, and has also been found in Tennessee and Virginia. Allgood was originally named "Chepultepec", providing its name to the formation as well. In Virginia, the Chepultepec Formation has a habit of forming large natural arches, including Natural Tunnel in Scott County and Natural Bridge in Rockbridge County. See also * List of fossiliferous stratigraphic units in Virginia * Paleontology in Virginia * Carbonate-ho ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chemung Formation
The Devonian Foreknobs Formation is a mapped bedrock unit in Pennsylvania, Maryland, Virginia, and West Virginia. Description The Foreknobs Formation contains massive sandstones; siltstone; "redbeds" of brownish-gray sandstone, siltstone, and shale containing scattered marine fossils; and occasional quartz-pebble conglomerate or conglomeratic sandstone beds. Stratigraphy Dennison (1970) renamed the old Chemung Formation the Greenland Gap Group and divided it into the lower Scherr Formation and the upper Foreknobs Formation. De Witt (1974) extended the Scherr and Foreknobs into Pennsylvania, but did not use the term Greenland Gap Group. Boswell, et al. (1987), does not recognize the Scherr and Foreknobs Formations in the subsurface of West Virginia and thus these formations are reduced from "group" to "formation" as the Greenland Gap Formation. Rossbach and Dennison (1994) extended the Foreknobs into the Catawba syncline of southwestern Virginia.Rossbach, T.J., and Dennison, J. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Manassas Sandstone
The Manassas Sandstone is a Carnian Stage sandstone geological formation in Virginia, United States. The Carnian Stage is part of the Triassic System of the Mesozoic. Fossil theropod tracks have been reported from the formation.Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607. See also * List of dinosaur-bearing rock formations ** List of stratigraphic units with theropod tracks 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. Non-avian theropods Avialans See also *L ... References Bibliography * {{ISBN, 0-520-24209-2 Triassic System of North America Carnian Stage Triassic geology of Virginia Sandstone formations of the United States Fluvial deposits Ichnofossiliferous formations ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bull Run Formation
The Bull Run Formation is a Late Triassic ( Norian) stratigraphic unit in the eastern United States.Bull Run Formation at Fossilworks.org Fossil fish bones and scales have been found in outcrops of the formation's Groveton Member in .Hunt et al., 2006, p.64 Indeterminate fossil tracks have been reported from the formati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Charleston Sandstone
The Charleston Sandstone is a geologic formation in West Virginia. It preserves fossils dating back to the Carboniferous period. See also * List of fossiliferous stratigraphic units in West Virginia This article contains a list of fossil-bearing stratigraphic units in the state of West Virginia, U.S. Sites See also * Paleontology in West Virginia References * {{DEFAULTSORT:Fossiliferous stratigraphic units in West Virginia West V ... References * Carboniferous West Virginia Carboniferous geology of Virginia Carboniferous southern paleotropical deposits {{Carboniferous-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chambersburg Formation
The Chambersburg Formation is a geologic formation in Virginia. It preserves fossils dating back to the Ordovician period. See also * List of fossiliferous stratigraphic units in Virginia * Paleontology in Virginia Paleontology in Virginia refers to paleontological research occurring within or conducted by people from the U.S. state of Virginia. The geologic column in Virginia spans from the Cambrian to the Quaternary. During the early part of the Paleozoic ... References * Ordovician geology of Virginia Ordovician southern paleotemperate deposits {{Virginia-geologic-formation-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Permian
The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Paleozoic Era; the following Triassic Period belongs to the Mesozoic Era. The concept of the Permian was introduced in 1841 by geologist Sir Roderick Murchison, who named it after the region of Perm in Russia. The Permian witnessed the diversification of the two groups of amniotes, the synapsids and the sauropsids ( reptiles). The world at the time was dominated by the supercontinent Pangaea, which had formed due to the collision of Euramerica and Gondwana during the Carboniferous. Pangaea was surrounded by the superocean Panthalassa. The Carboniferous rainforest collapse left behind vast regions of desert within the continental interior. Amniotes, which could better cope with these drier conditions, rose to dominance in place of their am ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
