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Transcript
OUTSTANDING GEOLOGIC FEATURES OF PENNSYLVANIA
BILGERS ROCKS
CLEARFIELD COUNTY
Location
Bilgers Rocks park, Clearfield Co., Bloom Twp., lat: 40.9941, lon: 78.5920; Curwensville 7.5-minute quadrangle
Geology
Bilgers Rocks is a classic “rock city” made of large sandstone
blocks. The rocks have been split by vertical fractures called
joints that have widened over time. Today, the sandstone blocks
are separated by narrow passageways to wide “streets” and
“rooms.” The large rocks were not deposited by glaciers, but
the freezing and thawing of water infiltrating along fracture and
bedding planes detaching the blocks from the parent rock mass.
Movement of the blocks was probably much more substantial
during glacial times when the ground thawed to a shallow depth
during brief summers. The thawed material would have had a
high water content, which would allow blocks of rock to slowly
move down any slope, however slight. Frost wedging during
the movement phase broke and shifted the blocks. Additional
fracturing and shifting of the rocks occurred along horizontal
bedding planes.
The rocks unit is the crossbedded “Homewood” sandstone of the Pottsville Formation. The sediment is fluvial
in origin, deposited in the Pennsylvanian period over 300 million years ago. The sandstone is typically 20-25
feet thick. Joint separations vary from a few inches to as much as 15-20 feet. As a result, chambers and
passageways may be found throughout the rocks. Chamber rooms have vertical walls 15-25 feet in height
connected by narrow passageways of the same height and from 15 inches to 3 feet in width. Some of these
narrow passageways ways can be up to 50 feet long.
Rooms and passageways at Bilgers Rocks. Center photo shows cross-bedded nature of sandstone, where layers lie at an angle to
other layers. Here, these patterns were produced by stream action as sand was deposited on a migrating, inclined plane, followed by
another layer of cross bedding above.
For information regarding outstanding geologic features, contact the Pennsylvania Geological Survey:
Bureau of Topographic and Geologic Survey, 3240 Schoolhouse Rd., Middletown, PA 17057
717-702-2017 www.dcnr.state.pa.us/topogeo
S. Reese, 2012