Basement Waterproofing Bethel Park, PA

Basement Waterproofing Bethel Park, PA

Foundation Repair and Basement Waterproofing

Everdry Pittsburgh is the areas basement waterproofing, crawlspace waterproofing and foundation repair company. In an area with an abundance of older homes, it is a good idea to have your home inspected and if needed waterproofed by a professional. Everdry Pittsburgh provides services in the metro area, as well as the surrounding suburbs. Contact Everdry Pittsburgh for a FREE consultation.

Facts About Bethel Park

The area that is now Bethel Park was originally settled around 1800 and was first established as Bethel Township, in 1886. Bethel Park was incorporated as a borough on March 17, 1949, and became a home rule municipality in 1978. The name was most likely named after a meeting house. The first armored car robbery in the U.S. occurred on March 11, 1927 when a Brinks truck, heading towards the Coverdale Mine about a mile away was attacked. Paul Jaworski and his ‘Flatheads” gang destroyed the road with dynamite to steal a mining payroll. According to the United States Census Bureau, the borough had a total area of 11.7 square miles (30 km2), all of it land. Its average elevation is 1,197 feet (365 m) above sea level. Bethel Park lies at the margin between the Pittsburgh Low Plateau and Waynesburg Hills Sections of the Allegheny Plateau physiographic province. The area is characterized as a maturely dissected region where the ephemeral minor tributaries converge into the tributaries of principal streams. The highest point in Bethel Park is Rocky Ridge, in the southwestern portion of the borough, 1,370 feet (420 m), and the lowest point is at the intersection of the Piney Fork and Alsip Run creeks, 980 feet (300 m), in the southeast corner.

Bethel Park has seven borders, including Castle Shannon to the north, Whitehall to the north-northeast, Baldwin to the northeast, South Park to the east and southeast, Peters Township in Washington County to the south, Upper St. Clair to the west, and Mt. Lebanon to the north-northwest. The exposed rocks in Bethel Park are mostly composed of sandstone, limestone, shale, and a few coal layers (Redstone, Waynesburg, Washington, etc.). The ages of the exposed rocks bracket the late Pennsylvanianepoch (Gzhelian age; approximately 303 million years ago) near the lowest elevations, and early Permian period (Asselian age; approximately 297 million years ago) near the highest parts of the southern part of Bethel Park (e.g. Rocky Ridge). These sedimentary rocks were deposited as the sea level rose and fell along an ancient coastline (with the region alternating between delta, shallow lake, and shallow sea), and finally being uplifted with the formation of the Appalachian Mountains.

Bethel Park is underlain by the Pennsylvania-age Monongahela Formation. The Monongahela Formation consists of the Uniontown member and the underlying Pittsburgh member, and the base is the Pittsburgh coal seam. Much of southern Allegheny County is undermined, and the PADEP indicates that all of Bethel Park was undermined. A portion of the area is underlain by the Pittsburgh Terminal No. 8 Mine (Cortis and others, 1975), which was commonly known as the “H” Mine and the Coverdale Mine. The mine opened around 1920. The historic operations of the Coverdale Mine are apparent on a Bridgeville 7.5-minute topographic map. A “Mine Dump” is shown adjacent to the Montour Railroad tracks and South Park Road. Coal was mined through vertical shafts accessing inclined slopes following the dip of the Pittsburgh coal seam. Mine voids in the inclined slope resulted from the practice of room and pillar mining during the early 20th century. The Coverdale Mine is closed and largely unflooded.

WHERE TO FIND US:
1568 Mars Evans City Road
Evans City, PA 16033
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(800) 388-3837