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The geology of Virginia began to form at least 1.8 billion years ago. The oldest rocks in the state were metamorphosed during the Grenville orogeny , a mountain-building event beginning 1.2 billion years ago in the Proterozoic , which obscured older rocks.
The Boscobel complex (originally "Boscabel bowlder beds") is unit of interlayered granite and gneiss within Goochland and Powhatan Counties, Virginia. The area had been mapped as the Petersburg Granite in 1970 by B. K. Goodwin. [2] The complex is mapped in a single, fault-bound area approximately 9 km long.
Meanwhile, Rogers had published six "Reports of the Geological Survey of the State of Virginia" (Richmond, 1836–40), though there were few copies, and recognition of their significance was slow to develop. They were later compiled by Jed Hotchkiss and issued in one volume with a map as Papers on the Geology of Virginia (New York, 1884). [9]
Pages in category "Geology of Virginia" The following 11 pages are in this category, out of 11 total. This list may not reflect recent changes. ...
The Doswell Formation (also known as the Doswell Group) is a geologic unit of Upper Triassic age, part of the Newark Supergroup.The Doswell Formation was originally named to refer to a geological sequence which forms the lower part of the sedimentary fill of the Taylorsville Basin in Virginia and Maryland.
The Patapsco Formation is a geologic formation of varigated clays, sandy clays, and sand in Virginia, the District of Columbia, Maryland, Delaware, Pennsylvania, and in the subsurface of New Jersey. [ 1 ] [ 2 ] It preserves fossils such as plants and molluscs dating back to the Cretaceous period .
The Edinburg Formation is an Ordovician-age geological formation in Virginia. It is primarily composed of basinal (deep sea) limestone and shale, and is one of the younger units in the "Middle Ordovician" sequence of the Shenandoah Valley. However, fossils have shown that it actually was deposited in the early part of the Late Ordovician.
A part of Virginia's Western Piedmont Province, the uranium deposit is bounded by the Chatham fault to the east, where it borders the Triassic Danville basin. Uranium minerals are found in the footwall of the Chatham fault, in healed fractures where apatite crystallized from high-temperature hydrothermal water in the Leatherwood granite mylonite .