While not usually described as gorges the Philadelphia area contains numerous narrow stream and river valleys which for all practical purposes should be called gorges. Most Philadelphia area gorges are 350 feet or less in depth and have been eroded into erosion resistant metamorphic and sedimentary rocks. Some Philadelphia area gorges now serve as major […]
Category archives for East Brandywine Creek
This is the second essay in which Philadelphia area drainage systems and erosional landforms as seen on detailed topographic maps are viewed as pieces of a solvable puzzle. The puzzle solution assumes running water carved the landscape features and the puzzle problem is to determine how running water accomplished that task. Each essay presents one […]
The Paoli-Thorndale Regional Rail Line is unique among the SEPTA Regional Rail Lines in that between Ardmore and Malvern it follows the Schuylkill-Delaware River drainage divide and further west crosses the Schuylkill-Delaware River divide along the Chester Valley south wall. The Paoli-Thorndale Regional Rail Line, which was originally the Pennsylvania Railroad main line and which […]
The East and West Branches of Brandywine Creek both originate in the area east of Honey Brook and between Welsh Mountain and the Baron Hills. From their common headwaters area the two streams diverge to take completely different south oriented routes to cross the east-northeast oriented Chester Valley and to carve separate narrow and deep […]
Phillylandforms.info 