Description
The Needmore Formation was originally described by Willard and Cleaves in 1939 as a dark- to medium-gray limy shale, based on exposures in southern Fulton County, Pennsylvania. They considered it part of the Onondaga Group. DeWitt and Colton (1964) described the Needmore as "soft calcareous medium dark-brownish-gray and greenish-gray shale and mudrock...and soft, slightly calcareous very fissile brownish-black shale" that is not resistant to weathering. They estimated its thickness in their study area (southern Bedford County, Pennsylvania, and most of Allegany County, Maryland) as approximately 150 feet.deWitt, W. Jr., and Colton, G. W., 1964, Bedrock geology of the Evitts Creek and Pattersons Creek Quadrangles, Maryland, Pennsylvania, and West Virginia: U.S. Geological Surveys Bull. 1179, pl 1 and 2Fossils
DeWitt and Colton (1964) identified brachiopods (''Coelospira acutiplicata'', ''Eodevonaria arcuata''),Notable Exposures
Type locality is between Needmore and Warfordsburg in southern Fulton County, Pennsylvania.Age
Relative age dating places the Needmore in the middleReferences
Geologic formations of Pennsylvania Geologic formations of Maryland Geologic formations of Virginia Geologic formations of West Virginia Devonian System of North America Devonian geology of Pennsylvania Devonian Maryland Devonian geology of Virginia Devonian West Virginia Emsian Stage Limestone formations of the United States {{Maryland-geologic-formation-stub