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An outcrop of the Allegheny Group along the Baltimore and Ohio Railroad Company cut northwest of Mineral City, Tuscarawas County, Ohio. The image shows removal of debris caused by highly fractured spalling rock at the location of the outcrop. This area has shale, siltstone, sandstone, conglomerate, limestone, coal, clay and flint lithologies. Bedrock is from the Pennsylvanian Geologic Period.
An outcrop with draped strata on the edge of massive sandstone of the Allegheny Group at Glen Ebon in York Township, Athens County, Ohio. This area has shale, siltstone, sandstone, conglomerate, limestone, coal, clay and flint lithologies. Bedrock is from the Pennsylvanian Geologic Period. The image was taken by Micheal C. Hansen in 1976.
An outcrop with the Freeport sandstone of the Allegheny and Pottsville Groups undivided along Interstate 77 near mile marker 63 in Tuscarawas County, Ohio. This area has shale, siltstone, sandstone, conglomerate, limestone, coal, clay and flint lithologies. Bedrock is from the Pennsylvanian Geologic Period. The photograph was taken by Michael C. Hansen in 1981.
Outcrop of the Cuyahoga Formation along State Route 16 west of Newark, Licking County, Ohio. This area has shale, siltstone, sandstone and conglomerate lithologies. Bedrock is from the Mississippian Geologic Period. The photograph was taken in 1976.
An outcrop of the Black Hand Sandstone Member of the Cuyahoga Formation behind Malabar Inn in Richland County, Ohio. The rock surface pictured here shows prominent crossbedding and honeycomb weathering. Bedrock is from the Mississippian Geologic Period. The location is approximate to Malabar Inn.
Outcrop of the Pottsville Group in Licking Township, Licking County, Ohio. This area has shale, siltstone, sandstone, conglomerate, limestone and coal lithologies. Bedrock is from the Pennsylvanian Geologic Period. The photograph was taken by Pauline Smyth on September 23, 1953.
The sandstone cliff site of Ohio's only fatal landslide on United States Highway 52, west of Hanging Rock, Lawrence County, Ohio. The landslide killed James A. Spence of Ironton on December 24, 1986. Joints in the sandstone are visible in the outcrop. The massive sandstone responsible for the main mass of rockfall ranges up to 60 feet thick and is stratigraphically below the Vanport limestone. The rocks involved in the fall are assigned to either the Upper Pottsville or the Lower Allegheny Group undivided. This area has shale, siltstone, sandstone, conglomerate, limestone, and coal lithologies. Bedrock is from the Pennsylvanian Geologic Period. The image comes from the files of the Ohio Department of Transportation.
An outcrop of the Newland (No. 4, Brookville) coal overlain by the Putnam Hill limestone of the Allegheny Group at a small quarry in Section 30 of Pike Township, Stark County, Ohio. This area has shale, siltstone, sandstone, conglomerate, limestone, coal, clay and flint lithologies. Bedrock is from the Pennsylvanian Geologic Period. The photograph was probably taken in 1958.
An outcrop of the Lower Kittanning (No. 5) coal of the Allegheny Group in New Albany, Mahoning County, Ohio. Bedrock is from the Pennsylvanian Geologic Period. This area has shale, siltstone, sandstone, conglomerate, limestone, coal, clay and flint lithologies. The photograph was taken by Myron T. Sturgeon in September 1941.
An outcrop of the Salem limestone of the Allegheny Group at Lisbon, Columbiana County, Ohio. Bedrock is from the Pennsylvanian Geologic Period. This area has shale, siltstone, sandstone, conglomerate, limestone, coal, clay and flint lithologies. The photograph was taken by Myron T. Sturgeon in March 1944. Location approximate to Columbiana County, Ohio.
Rock core sample showing the Pottsville Group-Sharon sandstone/conglomerate. The sample is from Core Record File No. 2541 in Raccoon Township, Gallia County, Ohio. This area has shale, siltstone, sandstone, conglomerate, limestone and coal lithologies. Bedrock is from the Pennsylvanian Geologic Period. The photograph was taken by Michael C. Hansen in 1982.
An outcrop of the Pottsville Group-Sharon sandstone/conglomerate at Thompson Ledges Township Park, Thompson Township, Geauga County, Ohio. Bedrock is from the Pennsylvanian Geologic Period. The photograph was taken by Michael C. Hansen in 1975.
A view of the broken slabs and boulders of Black Hand Sandstone of the Cuyahoga Formation at the base of Broken Rock Falls in the Old Man's Cave section of Hocking Hills State Park, Hocking County, Ohio. Below Old Man's Cave, about a 1/2 mile above the Lower Falls, a small creek enters the gorge from a narrow slot called Broken Rock Falls. The large piles of boulders that have accumulated beneath the falls are an example of the forces that affected the development of the Old Man's Cave gorge area. Bedrock is from the Mississippian Geologic Period. The photograph was taken Michael C. Hansen in June 1973.
Plant life growing on a boulder of Black Hand Sandstone of the Cuyahoga Formation at Broken Rock Falls in the Old Man's Cave section of Hocking Hills State Park, Hocking County, Ohio. Below Old Man's Cave, about a 1/2 mile above the Lower Falls, a small creek enters the gorge from a narrow slot called Broken Rock Falls. The large piles of boulders that have accumulated beneath the falls are an example of the forces that affected the development of the Old Man's Cave gorge area. Bedrock is from the Mississippian Geologic Period.
A view of the broken slabs and boulders of Black Hand Sandstone of the Cuyahoga Formation at the base of Broken Rock Falls in the Old Man's Cave section of Hocking Hills State Park, Hocking County, Ohio. Below Old Man's Cave, about a 1/2 mile above the Lower Falls, a small creek enters the gorge from a narrow slot called Broken Rock Falls. The large piles of boulders that have accumulated beneath the falls are an example of the forces that affected the development of the Old Man's Cave gorge area. Bedrock is from the Mississippian Geologic Period. The photograph was taken Michael C. Hansen in June 1973.
An outcrop of the Black Hand Sandstone Member of the Cuyahoga Formation at Big Spring Hollow. Big Spring Hollow is located in the Hocking State Forest, Hocking County, Ohio. It is part of the ninety-nine acres that have been set aside for rock climbing and rappelling. The area is managed by the Ohio Division of Forestry. Bedrock is from the Mississippian Geologic Period.
An outcrop of the Black Hand Sandstone Member of the Cuyahoga Formation at the Conkle's Hollow State Nature Preserve area in Hocking Hills State Park, Hocking County, Ohio. Conkle's Hollow is a deep rocky gorge. All three zones of the Black Hand Sandstone are visible in the steep cliffs of the valley walls. Crossbedding and honeycomb weathering are well displayed on the fretted surface of the Black Hand. The gorge at Conkle's Hollow follows a major joint trending N 60� W. Conkle's Hollow is named for an early visitor who inscribed his name, W. J. Conkle 1797, on the west wall of the gorge. Bedrock is from the Mississippian Geologic Period. The photograph was taken by Michael C. Hansen in 1973. The location is approximate...
A scenic view of Rockbridge with waterfall at Rockbridge State Nature Preserve in Hocking County, Ohio. The Natural Arch and Bridge Society defines a natural arch as �a rock exposure that has a hole completely through it formed by the natural, selective removal of rock, leaving a relatively intact frame.� At 92 feet Rockbridge is Ohio's longest natural bridge. The bridge originated as a typical Hocking Hills alcove carved into the soft middle layer of Black Hand Sandstone at the head of a short box canyon cut by a small tributary of the Hocking River. Three intersecting vertical fractures in the roof of the shelter were gradually enlarged until the block they surrounded was no longer supported and fell, creating...
An outcrop showing splits in the Putnam Hill limestone of the Allegheny Group at a small quarry in Section 30 of Pike Township, Stark County, Ohio. This area has shale, siltstone, sandstone, conglomerate, limestone, coal, clay and flint lithologies. Bedrock is from the Pennsylvanian Geologic Period. The photograph was probably taken around 1960 and includes Horace R. Collins for scale.
An outcrop of the Pottsville Group-Sharon sandstone/conglomerate west of Hartland, Huron County, Ohio. The area has shale, siltstone, sandstone and conglomerate lithologies. Bedrock is from the Pennsylvanian Geologic Period. The photograph was taken by Myron T. Sturgeon in August 1942.
map background search result map search result map Cuyahoga Formation, Licking County, Ohio 1976 Black Hand Sandstone, Malabar Inn, Richland County, Ohio Thompson Ledges, Geauga County, Ohio, 1975 Pottsville Group Outcrop, Licking County, Ohio, 1959 Sandstone Cliff at Hanging Rock, Lawrence County, Ohio, 1980s Core Sample of the Sharon Sandstone/Conglomerate, Raccoon Township, Gallia County, Ohio, 1982 Limestone Quarry, Pike Township, Stark County, Ohio, 1958 Roadcut along Interstate 77, Tuscarawas County, Ohio, 1981 Putnam Hill Limestone, Bethlehem Township, Stark County, Ohio, 1960 Lower Kittanning (No. 5) Coal at New Albany, Mahoning County, Ohio, 1941 Salem Limestone at Lisbon, Ohio, 1944 Baltimore and Ohio Railroad at Mineral City, Tuscarawas County, Ohio Strata at Glen Ebon, York Township, Athens County, Ohio, 1976 Pottsville Group-Sharon Sandstone/Conglomerate at Hartland, Huron County, Ohio, 1942 Broken Rock Falls, Hocking Hills State Park, Hocking County, Ohio, 1973 Broken Rock Falls, Hocking Hills State Park, Hocking County, Ohio Broken Rock Falls, Hocking Hills State Park, Hocking County, Ohio, 1973 Big Spring Hollow at the Hocking State Forest, Hocking County, Ohio Conkle's Hollow State Nature Preserve, Hocking Hills State Park, Hocking County, Ohio, 1973 Rockbridge State Nature Preserve, Hocking County, Ohio