Aquia Formation | |
---|---|
Stratigraphic range: Late Paleocene ~ | |
Type | Geological formation |
Unit of | Pamunkey Group |
Sub-units | Paspotansa & Piscataway Members |
Underlies | Nanjemoy Formation |
Overlies | Brightseat Formation |
Thickness | up to 100 feet (30 m) |
Lithology | |
Primary | Sandstone |
Location | |
Location | Hopewell, Virginia |
Coordinates | 38°18′N77°18′W / 38.3°N 77.3°W |
Approximate paleocoordinates | 39°00′N58°54′W / 39.0°N 58.9°W |
Region | Maryland, New Jersey, Virginia |
Country | United States |
Extent | Upper Chesapeake Bay-James River |
Type section | |
Named for | Aquia Creek |
The Aquia Formation is a geologic sandstone formation that extends from the upper Chesapeake Bay to the James River near Hopewell, Virginia. [1] It consists of clayey, silty, very shelly, glauconitic sand. [1] Fossil records indicate that this stratigraphic unit was created during the Paleocene. [1]
The Aquia formation was named for Aquia Creek where it is exposed in cliff faces along the banks. [2]
When uncovered, it appears dark green to gray-green, argillaceous, with well sorted fine- to medium-grained sand and locally indurated shell beds. [3] It is between 0 and 100 feet thick in Maryland. [3] Quartz and phosphatic pebbles and/or very coarse glauconitic quartz sand mark the base of the unit. [4] A few hard streaks of shells or thin "rock" layers are often reported but appear to be more abundant in the sections south of the James River. [4]
The Aquia formation is overlain by the Nanjemoy Formation and overlies the Brightseat Formation. [5]
The Aquia formation is broken down into two members: the lower Piscataway member and upper Paspotansa member. [2]
The Aquia Formation is thought to be 59.0-55.5 million years old. [2] The Piscataway member is 59–56.25 million years old, and the Paspotansa member is 56–55.5 million years old. [2] This is the Paleocene period.
Older publications describe the Aquia as being of Eocene age. [6]
Mammal fossils are extremely rare. [2]
Bird fossils are extremely rare. [2]
The Ripley Formation is a geological formation in North America found in the U.S. states of Alabama, Georgia, Mississippi, Missouri, and Tennessee. The lithology is consistent throughout the layer. It consists mainly of glauconitic sandstone. It was formed by sediments deposited during the Maastrichtian stage of the Late Cretaceous. It is a unit of the Selma Group and consists of the Cusseta Sand Member, McNairy Sand Member and an unnamed lower member. It has not been extensively studied by vertebrate paleontologists, due to a lack of accessible exposures. However, fossils have been unearthed including crocodile, hadrosaur, nodosaur, tyrannosaur, ornithomimid, dromaeosaur, and mosasaur remains have been recovered from the Ripley Formation.
The Yorktown Formation is a mapped bedrock unit in the Coastal Plain of Maryland, Virginia, North Carolina and South Carolina. It is overconsolidated and highly fossiliferous.
The Brightseat Formation is an exposure of marine sedimentary rock beds of Upper Cretaceous/Lower Paleocene age, in Landover, Maryland. The exposure is located at Brightseat Road between Sheriff and Landover Roads. The site is currently owned by the Maryland-National Capital Park and Planning Commission. It was given its name by R.R. Bennett and G.G. Collins in 1952.
The Choptank Formation is a geologic formation in Virginia and Maryland. It preserves fossils dating from the Miocene epoch of the Neogene period.
The Nanjemoy Formation is a geologic formation pertaining to both the Wilcox Group and the Pamunkey Group of the eastern United States, stretching across the states of Virginia, Maryland, and District of Columbia. The formation crops out east of the Appalachians and dates back to the Paleogene period. Specifically to the Ypresian stage of the Eocene epoch, about 55 to 50 Ma or Wasatchian in the NALMA classification, defined by the contemporaneous Wasatch Formation of the Pacific US coast.
The Piney Point Formation is a geologic formation in Virginia. It preserves fossils dating back to the Lutetian Stage of the Eocene Epoch of the Paleogene period.
The Williamsburg Formation is a geologic formation in South Carolina consisting of sandy shale and clayey sand. It is a member of the Black Mingo Group and overlays the Rhems Formation. It preserves fossils, among others coprolites, dating back to the Paleogene period.
The Bashi Formation is a geologic formation in Alabama and Mississippi. It is named for Bashi Creek in northern Clarke County, Alabama, which cuts through some of its exposures. It preserves fossils dating back to the Eocene period, or Wasatchian in the NALMA classification.
The Dawson Arkose is a geologic formation in the Denver Basin that underlies the Denver area in Colorado. It is characterized by alternating beds of arkosic sandstone and mudstone. The Dawson Arkose contains plant remains and other nonmarine fossils, and hosts aquifers that are important sources of water for the area.
The Muleros Formation is a geologic formation in New Mexico, which is particularly well exposed at Cerro de Cristo Rey near El Paso, Texas. It preserves fossils dating back to the early Cretaceous period.
Cucullaea gigantea is an extinct species of false ark shell found in the United States, in the Aquia Formation in Maryland and Virginia along the Potomac River and its tributaries, and in Alabama. They flourished in marine environments during the Paleocene, ranging from 58.7 to 55.8 million years ago.
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. It is one of the three formations which make up the Calvert Cliffs, all of which are part of the Chesapeake Group.
fossils of the aquia formation.