Jump to content

Bear Valley Strip Mine: Difference between revisions

From Wikipedia, the free encyclopedia
Content deleted Content added
added property owner
Gallery: added another image
Line 39: Line 39:
File:Bear Valley Slickensides.jpg|[[Slickensides]] on a fault plane, south wall. Lens cap 5.8cm wide.
File:Bear Valley Slickensides.jpg|[[Slickensides]] on a fault plane, south wall. Lens cap 5.8cm wide.
File:Stigmaria Bear Valley upright.jpg|Upright ''[[Stigmaria]]'' in dipping sandstone and shale beds of the north wall. A so-called "[[Polystrate fossil]]".
File:Stigmaria Bear Valley upright.jpg|Upright ''[[Stigmaria]]'' in dipping sandstone and shale beds of the north wall. A so-called "[[Polystrate fossil]]".
File:DCP 0776.JPG|Another image of the south wall and Whaleback
</gallery>
</gallery>



Revision as of 02:59, 23 April 2010

View of the Bear Valley Strip Mine from the north wall facing southeast, with the "Whaleback" in center

The Bear Valley Strip Mine is an abandoned strip mine located to the southwest of the town of Shamokin, Pennsylvania. It lies in the Western Middle Field of the Anthracite belt in the Ridge-and-Valley Appalachians, where the Pennsylvanian Llewellyn Formation is exposed. The property is owned by the Reading Anthracite Company. [1]

Due to the coal and other overlying rock being removed by mining down to a resistant sandstone bed, excellent three-dimensional structures of folding and faulting caused by the Alleghany Orogeny are clearly displayed. Students of geology have been visiting the location for decades due to the quality of exposures.

The central anticline in the valley is often called the "Whaleback".

The sequence of structural deformation is outlined as follows[1]:

Stage Deformation event
I Joint formation in coal
II Joint formation with quartz fiber fillings in sandstone and ironstone
III Pressure solution and primary crenulation cleavage
IV Conjugate wrench and wedge faults form
V Large-scale folding
VI Extensional jointing and faulting

References

  1. ^ a b Sequence of structural stages of the Alleghany orogeny at the Bear Valley Strip Mine, Shamokin, Pennsylvania. Nickelsen, R. P. (Dept. of Geology, Bucknell University) Geological Society of America Centennial Field Guide—Northeastern Section, 1987