Nanjemoy Formation
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 about thin formation crops out in a narrow irregular band and only in certain of the many creeks  of the Maryland peninsula and on the southern side of the Potomac River in Virginia. The two members the formation was divided into by Clark and Martin in 1901; Potapaco and Woodstock, represent different phases in the basin history. The lower Potapaco Member is much more clayey, described as marl, than the upper Woodstock Member, probably characteristic of less storm influences in the shallow shelf sediments. The formation has provided a wealth of fossils of mainly fish, but also mammals, reptiles, birds and flora. The presence of the sharks "Otodus obliquus" and "Carcharocles aksuaticus", as well as various other shark  and ray species are notable. Crocodylian, snake, turtle, mammal, and bird remains have all been found in the Nanjemoy Formation. Etymology. Nanjemoy is probably an Ojibwe word, meaning "one goes downward", representing the many rivers and creeks in the wet watershed of Chesapeake Bay, an area originally inhabited by the Algonquin-speaking Nanticoke and Powhatan. The formation is named after Nanjemoy Creek, a left tributary of the Potomac River. Wicomico is the name of two separate rivers, one on Maryland's Eastern Shore, Wicomico River (Maryland eastern shore), and another in Southern Maryland, Wicomico River (Potomac River tributary), and is  the name of a small thoroughfare in southeastern Charles County. The reason this term appears in three different places in the state simply means that the people living there when the English barged in were trying to tell them it was a nice place to live. "Wigh" or "wik", representing "pleasant" and "accomico" "dwelling, village" was the native's way of telling the Europeans they liked living there. Potapaco was an early name for Port Tobacco Creek, that was named after the people, also known as the Piscataway. Nanjemoy, which may contain elements of Ojibwa, by contrast means "one goes  downward." Mattawoman, found in Charles, Prince George's and on the Eastern Shore, has remnants of not only Algonquin, but Fox and Ojibwa as well, and translates to "where one goes pleasantly." Definition. The Nanjemoy Formation was defined by Clark and Martin in 1901, as part of the mapping by the Maryland Geological Survey. The Nanjemoy Formation was divided into two members, the lower or Potapaco, and the upper or Woodstock. The main lithologic distinction is that the lower part of the Nanjemoy is much clayey than the upper part. In the subsurface, the distinction between the members is less  evident than in outcrops, especially in Maryland, so the formation has been left undivided. In the outcrops along the Potomac River near Popes Creek, the contact between the Woodstock and Potapaco at about above the water level. Extent. The Nanjemoy Formation, represented as Tn on the geologic map of the Washington West 30' × 60' Quadrangle, Maryland, Virginia, and Washington D.C., restricted to the southeastern side of the Potomac Basin represented in the quadrangle. Scott (2005) in his thesis included a map showing the thin bands of outcrops of both the underlying Marlboro Clay and the Nanjemoy Formation, restricted to  the many creeks feeding the Chesapeake Bay. The Nanjemoy Formation (Eocene), the Marlboro Clay (Paleocene), and the Aquia Formation (Paleocene) are present in the westernmost part of the Potomac channel. The outcrop area of the formation is designated Nanjemoy Wildlife Management Area. Geology. Geologically, the area of deposition of the Nanjemoy Formation is part of the Atlantic coastal plain province. Potomac Basin. The Potomac Basin represents the central part of the Atlantic coastal plain that stretches along the Atlantic coast of Canada and the United States. The basin stretches across parts of four states (Maryland, Pennsylvania, Virginia and West Virginia ), as well as the District of Columbia. This area is also called the Potomac watershed. It includes all of the land area where water drains towards the mouth of the Potomac – the point where the river spills into the Chesapeake Bay. The Potomac River basin is the 2nd largest watershed in the Chesapeake Bay watershed. The drainage area of the Potomac includes 14,670 square miles in four states: Virginia (5,723 sq. mi.), Maryland (3,818 sq. mi.), West Virginia (3,490 sq. mi.), Pennsylvania (1,570 sq. mi.), and the District of Columbia (69 sq. mi.). The basin’s total area varies depending  on map projection used. The basin lies in five geological provinces: the Appalachian Plateau, the Ridge and Valley, Blue Ridge, Piedmont Plateau, and Coastal Plain. The Potomac meanders over 383 miles from Fairfax Stone, West Virginia to Point Lookout, Maryland. The river’s distance will vary with map projection and location of measuring tool in the river (ie. middle of the river, Maryland shoreline, Virginia shoreline). Based on information from the NLCD 2011 database, the majority of the basin’s land area is covered by forests at 54.6 percent of the land area. Developed land makes up 14.1 percent of  the basin’s land area, while agriculture covers 26.0 percent. Water and wetlands make up 5.9 percent of the basin’s land area. The Potomac's major tributaries include: the Anacostia River, Antietam Creek, the Cacapon River, Catoctin Creek, Conococheague Creek, the Monocacy River, the North Branch, the South Branch, the Occoquan River, the Savage River, the Seneca Creek, and the Shenandoah River. The population of the basin is approximately 6.11 million (2010 estimated census). The population has increased by about five percent since 2005. The following information is based on 2010 estimated census data. Stratigraphy. The Nanjemoy Formation belongs  to two geologic groups; the Wilcox Group of the Gulf of Mexico Basin in the southernmost surface expression of the formation and the Pamunkey Group in the northern and central portions from Maryland in the north through Virginia and the Carolinas. Both geologic groups have been dated to the early Paleogene; the Paleocene and Eocene periods, or in the commonly used NALMA classification; Wasatchian, defined by the age-equivalent Wasatch Formation of Wyoming. The third-oldest unit in the Pamunkey Group is the Nanjemoy Formation that overlies the Marlboro Clay and is partly overlain by the Piney Point Formation and  in many areas covered by the Miocene Calvert Formation, separated by an unconformity representing about 34 Ma. The upper surface reaches an elevation of about and is overlain in most places by the Calvert Formation (Tc). The unit is present only in the southeastern part of the map area of Washington D.C., and it reaches a maximum thickness of about . Petrology. The formation comprises glauconitic quartz sand, dark-grayish-green to olive-black (tan to orange where weathered), fine to medium-grained; and dark-greenish-gray silty clay. In places, the sand is very muddy or contains many small quartz  pebbles, and the clay is silty or sandy. Both lithologies contain richly fossiliferous beds including abundant mollusk shells. Robert E. Weems and Gary J. Grimsley (1999) described the geology of the Fisher/Sullivan site in Virginia as: Paleogeography. Climate. The climate of the Early Eocene and Late Paleocene was very hot and rich in CO. Based on the fossils of the terrifyingly large "Titanoboa cerrejonensis", dating to the latest Paleocene, a body mass of for the snake was estimated. This enormous size could only have been possible under the most ideal conditions for such large species, around 6 to 8  Ma after the extinction of the previous megafauna; the dinosaurs. The climate of the Neotropical biome was estimated at average yearly temperatures and 2000 ppm atmospheric CO. Depositional environment. The depositional environment of the Nanjemoy Formation is mostly shallow shelf. The more clayey beds suggest an area or time of quiet water, not affected by waves, tides, or current activity; intercalated sandier zones may reflect the higher energy of waves or currents during episodic storms. Its regional dip is eastward at 15–20 ft per mile (3-3.5 m/km). Paleontology. The floral and faunal assemblage of the Nanjemoy Formation is  very varied and provides an insight into the paleobiological and paleoclimatological environment of the early Eocene. Fossils of bivalves, sharks, rays, actinopterygian fishes, reptiles, birds and mammals, and of fruits and seeds are common in the Potapaco Member. More than 2000 vertebrate coprolites from the Potapaco Member at the Fisher/Sullivan Site in Virginia were analyzed by Dentzien Dias et al. (2019). The chemical composition (phosphatic), inclusions and morphology suggest that only carnivorous scats were preserved. All Nanjemoy coprolites were produced by fishes; chondrichthyans, Carcharhiniformes, and lamniform sharks, probably the genus "Carcharias". Other morphotypes were produced by actinopterygian fishes. The  surface marks and the lack of flatness on most coprolites suggests early lithification of the Potapaco Member. Main fossil sites of the Nanjemoy Formation are Fisher/Sullivan site, VA. In October 1990, Mr. Richard Brezina of the Maryland Geological Society discovered an important fossil site east of Fredericksburg, in eastern Stafford County, Virginia. This locality, along an unnamed tributary of Muddy Creek, became known as the Fisher/Sullivan site in recognition of its principle landowners. Mr. Brezina immediately realized that the site was exceptional, because it yielded numerous shark teeth and other vertebrate remains from the sands and gravels in  the unnamed tributary. Mr. Brezina notified other members of the Maryland Geological Society, and together members of the MGS began to screen stream sediments at the site for more shark teeth and other remains. It soon became apparent, from the types of teeth that were being found and from the color and texture of the sediments in the banks of the creek, that the fossils were being reworked from glauconitic ("greensand") horizons of the Lower Tertiary (Paleocene-Eocene) Pamunkey Group. Because the Pamunkey Group previously had yielded only sparse vertebrate remains, it seemed reasonable to suspect that this locality was  scientifically important. Fossil content. Among many invertebrates (gastropods, bivalves, corals, bryozoans), the following fossils have been reported from the Nanjemoy Formation: Contemporaneous fossiliferous units. Ypresian, Wasatchian and Casamayoran formations: