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The Pocono Mountains, commonly referred to as the Poconos (/ ˈ p oʊ k ə n oʊ z /), are a geographical, geological, and cultural region in Northeastern Pennsylvania.They overlook the Delaware River and Delaware Water Gap to the east, Lake Wallenpaupack to the north, Wyoming Valley and the Coal Region to the west, and the Lehigh Valley to the south.
The Mississippian Pocono Formation is a mapped bedrock unit in Pennsylvania, Maryland, and West Virginia, in the United States. It is also known as the Pocono Group in Maryland and West Virginia, [ 2 ] and the upper part of the Pocono Formation is sometimes called the Burgoon Formation or Burgoon Sandstone in Pennsylvania.
Penobscot Knob, also Penobscot Mountain, is a summit that is located in the western fringe of the Poconos nearest to Mountain Top, Pennsylvania. The Solomon Gap pass below it contains an important multi-modal transportation corridor.
Mount Pocono is located at (41.123012, −75.359574), [4] and is nearly centered in Monroe County—the most southerly and centered county of the five counties containing portions of the Pocono Mountains of Northeastern Pennsylvania.
Hence Blue Mountain is not to be confused with the Blue Ridge Mountains but instead, represents the sharp escarpment, a step in elevation separating the Appalachian Mountains from the pastoral basin famous as the landscape associated with the Pennsylvania Dutch in southern Pennsylvania called the Great Valley A physiographic province, as are ...
The Pocono Mountain Range runs throughout northeastern Pennsylvania. The Allegheny and Pocono mountains are the two largest subranges in Pennsylvania. Other mountain ranges in Pennsylvania include the Bear Pond Mountains, the Blue Ridge Mountains, the Conewago Mountains, Music Mountains, Town Hill Mountain Range, and the Endless Mountains. [5 ...
Pocono Mountains (2 C, 120 P) R. Ridges of Pennsylvania (4 C, 42 P) S. South Mountain Range (Maryland−Pennsylvania) (37 P) Pages in category "Mountain ranges of ...
Erosion brought sediment from the mountain westwards into the sea, forming the deltas. Eventually, the Delta formation was buried and transformed into sandstone, which was then revealed in places when the Catskill and Appalachian Mountains were formed at a later date. This transformation and uncovering is the primary reason why the Catskill ...