Jim Thorpe is a borough and the county seat of Carbon County in the U.S. state of Pennsylvania.
Swatara Creek is a 72-mile-long (116 km) tributary of the Susquehanna River in east-central Pennsylvania in the United States. It rises in the Appalachian Mountains in central Schuylkill County and passes through northwest Lebanon County before draining into the Susquehanna at Middletown in Dauphin County.
The West Branch Susquehanna River is one of the two principal branches, along with the North Branch, of the Susquehanna River in the northeastern United States. The North Branch, which rises in upstate New York, is generally regarded as the extension of the main branch, with the shorter West Branch being its principal tributary. The West Branch, which is 243 miles (391 km) long, is entirely within the state of Pennsylvania, draining a large mountainous area within the Allegheny Plateau in the western part of the state. Along most of its course it meanders past mountain ridges and through water gaps, forming a large zigzag arc through central Pennsylvania around the north end of the Allegheny Mountains. In colonial times the river valley provided an important route to the Ohio River valley. In the 19th century, its lower valley became a significant industrial heartland of Pennsylvania. In the 20th century, the upper reaches of the West Branch turned a yellow/orange color due to sulfurous drainage from nearby and abandoned deep bituminous coal mines.
The Union Canal was a towpath canal that existed in southeastern Pennsylvania in the United States during the 19th century. First proposed in 1690 to connect Philadelphia with the Susquehanna River, it ran approximately 82 mi from Middletown on the Susquehanna below Harrisburg to Reading on the Schuylkill River.
The Endless Mountains are a geographical, geological, and cultural region in Northeastern Pennsylvania, United States. The Endless Mountains region includes Bradford, Sullivan, Susquehanna, and Wyoming counties. The highest peak in the region is the North Knob of Elk Mountain at 2693 feet.
Blue Mountain, Blue Mountain Ridge, or the Blue Mountains of Pennsylvania is a ridge of the Appalachian Mountains in eastern Pennsylvania. Forming the southern and eastern edge of the Ridge-and-Valley Appalachians physiographic province in Pennsylvania, Blue Mountain extends 150 miles (240 km) from the Delaware Water Gap on the New Jersey border in the east to Big Gap in Franklin County in south-central Pennsylvania at its southwestern end.
Yellow Breeches Creek, also known as Callapatscink Creek, Callapatschink Creek or Shawnee Creek is a 56.1-mile-long (90.3 km) tributary of the Susquehanna River in central Pennsylvania, USA. There is no agreed upon explanation for the name Yellow Breeches Creek, which is found in land warrants as early as 1736.
Meshoppen Creek is a tributary of the Susquehanna River in Susquehanna and Wyoming counties, Pennsylvania, in the United States. It is approximately 30.6 miles (49.2 km) long and flows through Bridgewater Township, Dimock Township, and Springville Township in Susquehanna County and Lemon Township, Washington Township, Meshoppen Township, and Meshoppen in Wyoming County. The watershed of the creek has an area of 114 square miles (300 km2). It is possible to canoe on 17.0 miles (27.4 km) of Meshoppen Creek.
Geographic regions of the Commonwealth of Pennsylvania, United States of America.
The Geology of Pennsylvania consists of six distinct physiographic provinces, three of which are subdivided into different sections. Each province has its own economic advantages and geologic hazards and plays an important role in shaping everyday life in the state. They are: the Atlantic Coastal Plain Province, the Piedmont Province, the New England Province, the Ridge and Valley Province, the Appalachian Plateau Province, and the Central Lowlands Province.
Pisgah Mountain or Pisgah Ridge is a ridgeline running 12.5 miles (20.1 km) from Tamaqua to Jim Thorpe, Pennsylvania. It is oriented north-northeast to south-southwest, and its north-side valley is followed by U.S. Route 209 from river gap to river gap. The ridge is a succession of peaks exceeding 1,440 feet (438.9 m) rising 300 to 540 feet above the boroughs of Lansford, Coaldale, and Tamaqua in the Panther Creek valley. The highest point on Pisgah Mountain is at 1,611 feet (491 m) in the borough of Summit Hill, which sits atop the ridge. Near Summit Hill was the "Sharpe Mountain" (peak) where in 1791 Phillip Ginter is documented as having discovered anthracite, leading to the formation of the Lehigh Coal Mine Company. In 1818 the Lehigh Coal Company took over the mines, and the mining camp gradually became a settlement and grew into Summit Hill.
Nesquehoning Mountain or Nesquehoning Ridge is a 15–17-mile-long (24–27 km) coal bearing ridge dividing the waters of Lehigh Valley to the north from the Schuylkill River valley and the several near parallel ridgelines of the Ridge-and-valley Appalachians barrier range all local members of which run generally WSW-ENE in the greater overall area.
Mountain Top yard or Penobscot yard is a rail yard in Mountain Top, Pennsylvania. It was built by the Lehigh Coal & Navigation Company (LC&N) in response to an 1837 bill authorizing a right of way and was established by 1840, at least as a construction camp for the Ashley Planes, in support of the construction of the Lehigh and Susquehanna Railroad trackage and operations to join the northern Anthracite Coal Region from barge loading docks along the Susquehanna in Pittston, in the Wyoming Valley, with the Lehigh Canal.
Mauch Chunk Ridge or Mauch Chunk Mountain is a historically important barrier ridgeline north of the Blue Mountain escarpment and 3rd parallel ridgeline south of the Nesquehoning Creek after Nesquehoning Mountain and Pisgah Ridge in the Ridge-and-Valley Appalachians of Northeastern Pennsylvania. The three lengthy ridges and two valley formations together are literally the first ridges and valleys just south of the Poconos on the opposite side of the Lehigh River—geological formations which contain some of the richest Anthracite coal bearing sedimentary rocks of Northeastern Pennsylvania. Historically, the first Anthracite mines in America were located atop Pisgah Mountain at Summit Hill and caravanned by pack mule through the Mauch Chunk Creek valley. Then the historic Mauch Chunk and Summit Hill Switchback Railroad, the second railway in North America was built along the Pisgah Mountain side of the same valley—and become quite a tourist attraction and is known as the world's first roller coaster, and would inspire others in purpose built amusement parks. The Mauch Chunk and Summit Hill Switchback Railroad became only a tourist road in the 1890s and thrilled riders until it was liquidated in the 1930s, a casualty of the Great depression.
Nescopeck Mountain is a ridge in Columbia County and Luzerne County, in Pennsylvania, in the United States. Its elevation is 1,594 feet (486 m) above sea level. The ridge is a forested ridge, with at least two types of forest and two systems of vernal pools. It is a very long and unbroken ridge with two water gaps: one carved by Catawissa Creek and one carved by Nescopeck Creek. This later gap was exploited as a transportation corridor with the construction of the Lehigh & Susquehanna Turnpike between the respective frontier communities at Lausanne Landing and Nescopeck in 1805 connecting the newly developing Wyoming Valley with Philadelphia and the Delaware River valley; cutting off over 100 miles between Philadelphia and Wilkes-Barre. Today's Route PA 93 derives from this historic pack mule road.
Pennsylvania State Game Lands Number 12 are Pennsylvania State Game Lands in Bradford County and Sullivan County, in Pennsylvania, in the United States. The game lands have an area of nearly 24,480 acres (9,910 ha) in Bradford County. The area is mainly mountainous and wooded and major streams in the area include Schrader Creek, Sugar Run, and Little Schrader Creek. Game animals within the game lands include black bear, gray squirrel, whitetail deer, and wild turkey. The main hardwood tree species include American basswood, American beech, black cherry, black birch, red maple, sugar maple, white ash, and aspen. The main conifer species include eastern hemlock, eastern larch, plantation Norway spruce, plantation red pine, and white pine.
Haystack Mountain (Pennsylvania), is an otherwise non-descript 1871 ft peak forming the steep southwestern faces of the Solomon Gap mountain pass's saddle connecting and dividing the Wyoming Valley from the Lehigh Valley.
Broad Mountain or Broad Ridge in the Ridge-and-Valley Appalachians in Carbon County and Schuylkill County in Eastern Pennsylvania is a steep-faced, anthracite-bearing barrier ridge just south of both Beaver Meadows and Weatherly, north of Nesquehoning and west and south of the Lehigh River basin west of the southwest border of the Poconos). The mountain ridge line is mostly flat and looks very similar to the man-made piles of culm in the region from the roads and towns looking up.
The gaps of the Allegheny, meaning gaps in the Allegheny Ridge in west-central Pennsylvania, is a series of escarpment eroding water gaps along the saddle between two higher barrier ridge-lines in the eastern face atop the Allegheny Ridge or Allegheny Front escarpment. The front extends south through Western Maryland and forms much of the border between Virginia and West Virginia, in part explaining the difference in cultures between those two post-Civil War states. While not totally impenetrable to daring and energetic travelers on foot, passing the front outside of the water gaps with even sure footed mules was nearly impossible without navigating terrain where climbing was necessary on slopes even burros would find extremely difficult.
Little Meshoppen Creek is a tributary of Meshoppen Creek in Susquehanna County and Wyoming County, in Pennsylvania, in the United States. It is approximately 9.5 miles (15.3 km) long and flows through Auburn Township in Susquehanna County and Messhoppen Township and Messhoppen in Wyoming County. The watershed of the creek has an area of 13.8 square miles (36 km2). The creek is a Coldwater Fishery and Migratory Fishery and is not designated as an impaired waterbody. Numerous industries involved the creek in the 19th century, including a tannery, several mills, and a water company that constructed a dam on the creek.
