Name/Title
S04.01.003Description
Field trip participants on the Central Peak of the Serpent Mound Impact Structure at the William V. Martin farm north of Peebles in Adams County, Ohio. This area has dolomite, shale, limestone, sandstone, and siltstone lithologies. Because of the geologic forces that have acted on the site of the impact crater, bedrock in the area is a mixture of uplifted, down dropped, faulted, folded and eroded rock from the Ordovician, Silurian, Devonian and Mississippian Geologic Periods. The photograph was taken by Gerald H. Newsom during the American Association of Petroleum Geologists Eastern Section Meeting Field Trip to the Plum Run Quarry and the Serpent Mound Disturbance on October 10, 1998.
The Serpent Mound Impact Structure is an approximately 9-mile-diameter area of highly disturbed and structurally deformed bedrock at the intersection of Adams, Highland and Pike counties. The deeply eroded crater is believed to have been formed by an asteroid or a comet impact approximately 250 to 300 million years ago. It is named the Serpent Mound Impact Structure after the prehistoric American Indian effigy earthwork located near the southwestern edge of the area. It is the single-most complex geologic structure exposed at the surface in Ohio. Investigation of the impact structure has been done using rock cores, seismic data, geophysical surveys and remote satellite imagery for the area.
This slide image included in the USGS National Digital Catalog for NGGDPP Grant G15AP00115 in FY2015.Context
Group of people holding tools and heading towards serpent-shaped mound. Central Peak of the Serpent Mound Impact Structure; north of Peebles, Ohio.