| Fairview Cave | contact: Jim Reger, (jreger@mgs.md.gov ) |
| Fairview Cave | |||
| Geology: | (click on an image for a larger view) | ||
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Fairview cave is
developed in a thrust sheet of the Chambersburg Limestone, very close
to a contact with the Martinsburg Shale. The passages are found along
a series of major north-south oriented joints in beds which dip 10º
east and strike due north. |
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| Description | |||
| The entrance
passage is four feet square and leads to a small, low room out of which
leads a low crawlway. The crawlway is actually the top of a vertical fissure
or channel which is nearly filled by stream alluvium. This passage trends
south for 100 feet and then swings to the west where it opens up into walking
passage. This passage parallels the first and leads out of the central room
as a narrow fissure for forty feet to the north. At the southern end of
the room there is a nearly vertical mud slide which joins a more southerly
trending passage for 160 feet. Intermittent sections of a slightly lower
level with a stream bed opens up into walk can be observed along the eastern
flank of the passage, which is narrow and high and inclined at right angles
to the dip of the beds. A few flowstone and drapery formations exist here;
however, most of the cave is devoid of speleothems and is exceedingly muddy
and wet.
(from ES3 -Caves of Maryland) |
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| updated
3/7/05
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