- Geology of Bedford County, Pennsylvania
Pennsylvaniais situated along the western border of the Ridge and Valleyphysiographic province, which is characterized by folded and faulted sedimentary rocks of early to middle Paleozoicage. The northwestern border of the county is approximately at the Allegheny Front, a geological boundary between the Ridge and Valley Province and the Allegheny Plateau(characterized by relatively flat-lying sedimentary rocks of late Paleozoicage). ( [http://www.dcnr.state.pa.us/topogeo/maps/map13.pdf PA Geologic Survey Map 13] )
The stratigraphic record of sedimentary rocks within the county spans from the
CambrianWarrior Formation to the PennsylvanianConemaugh Group (in the Broad Top area). No igneous or metamorphic rocks of any kind exist within the county.
The primary mountains within the county (From west to east: Wills, Evitts, Dunning, and Tussey mountains) extend from the southern border with
Marylandto the northeast into Blair County, and are held up by the Silurian Tuscarora Formation, made of quartz sandstoneand conglomerate. Chestnut Ridge is a broad anticlineheld up by the DevonianRidgeley Member of the Old Port Formation, also made of sandstoneand conglomerate. Broad Top, located north of Breezewood, is a plateau of relatively flat-lying rocks that are stratigraphically higher, and thus younger ( Mississippianand Pennsylvanian), than most of the other rocks within the county ( Cambrianthrough Devonian). Broad Top extends into Huntingdon County to the north and Fulton County to the east.
The Raystown Branch of the
Juniata Riveris the main drainage in the northern two-thirds of the county. The river flows to the east through the mountains within the county through several water gaps caused by a group of faults trending east-west through the central part of the county. The river then turns north and flows into Raystown Lakein Huntingdon County. The southern third of the county is drained by several tributaries of the Potomac River. Both the Potomac and Juniata rivers are part of the Chesapeake BayWatershed.
All of Bedford County lies far to the south of the
glacial boundary, and thus it was never glaciated ( [http://www.dcnr.state.pa.us/topogeo/maps/map59.pdf PA Geologic Survey Map 59] ). However, during the Pleistoceneepoch, or "Ice Age," periglacial(meaning "around glacier" or simply "cold") processes dominated. Most of the county was most likely a tundraat this time. The many boulder fields obvious as rocky and often treeless areas on mountainsides within the county formed as a result of seasonal freeze-thaw cycles during the Pleistocene.
Several limestone quarries exist in Bedford County, most of which are owned and operated by New Enterprise Stone and Lime Company. Quarry locations include Ashcom, New Paris, Kilcoin, and Sproul. [http://www.nesl.com/Default.aspx?tabid=280&portalid=2000&Pageid=Blair-Bedford] .
Two coal fields exist within Bedford County. One is the Broad Top Field in the northeastern corner of the county, and the other is the Georges Creek Field along the southwestern border ( [http://www.dcnr.state.pa.us/topogeo/maps/map11.pdf PA Geologic Survey Map 11] ). Both fields contain bituminous coal. There are abandoned mines in both areas and
acid mine drainageis an environmental problem in the Broad Top area, where several fishless streams exist as a result of the discharge from the abandoned mines. [http://bedford.pacounties.org/bedford/lib/bedford/AcidMineDrainage.pdf] . Natural gasfields and storage areas exist in southeastern Bedford County, primarily within folded Devonianrocks south of Breezewood. Another deep gas field exists in the vicinity of Blue Knobon the border with Blair County to the north. ( [http://www.dcnr.state.pa.us/topogeo/maps/map10.pdf PA Geologic Survey Map 10] )
Interesting geologic features within Bedford County include some of the following:
* New Enterprise New Paris quarry, where fossil
coralsand bryozoansmay be found within the DevonianKeyser Limestone.
* Coral Caverns [http://www.coralcaverns.com/] in Manns Choice.
* The roadcut through Warrior Ridge on Rt. 30 (Everett Bypass), where an exposure of
Silurianand Devonianrocks from limestoneto shaleto conglomerate can be seen.
* The roadcut on the north side of the
Pennsylvania Turnpikeat the Narrows water gap(where the Raystown Branch cuts through Evitts Mountain) exposes a continuous section of the Bald Eagle Formation, Juniata Formation, and the Tuscarora Formation. The beds of the Bald Eagle are overturned, folded, and faulted. The Tuscarora and Juniata are also exposed on the south side of the gap along Rt. 30.
* Sweet Root Natural Area, within
Buchanan State Forestand located near Chaneysville, where periglacialprocesses have created a bouldery landscape by eroding the Tuscarora Formationof Tussey Mountain.
* Blue Knob, a notable ski resort and recreational area, is also the state's second highest point at 3146 feet/959 m (after Mount Davis in Somerset County to the west).
* A transpression structure is located on the northern border of the county (shared with Blair County), about three miles east of the town of Woodbury. This structure is an up-thrust block of
Cambrianand Ordovicianrocks bounded on all sides by north-trending faults. The southern tip of the structure is approximately at Pulpit Hill.
* An outcrop on the north side of Rt. 30 about three miles west of the village of Juniata Crossing shows an excellent example of a
thrust faultwithin the Devonian Catskill Formation.
* The Raystown Branch of the
Juniata Riverbetween Breezewood and Raystown Laketo the north is an example of a river with incised (or entrenched) meanders.
* Bedford County
Geology of Pennsylvania
* [http://bedford.pacounties.org/bedford/site/default.asp Bedford County home page]
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