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History Of Carbon County, Pennsylvania
Carbon County is a county in the Commonwealth of Pennsylvania. As of the 2020 census, the population was 64,749. The county is part of the Northeast region of the commonwealth. The county borders Lehigh and Northampton counties in the state's Lehigh Valley region to its south, Monroe County to its east, Luzerne County to its north, and Schuylkill County to its west. The county is approximately northwest of Allentown, the state's third-largest city, and west of New York City, the nation's largest city. The county seat is Jim Thorpe, which was founded in 1818 as Mauch Chunk. The Lehigh River, a tributary of the Delaware River, flows through Carbon County. History Moravian settlement In 1745, the first colonial settlement in Carbon County was established by a Moravian mission in Gnadenhutten, in present-day Lehighton. By 1752, increased hostility between colonialists and Native Americans put Gnadenhutten at risk for attack; in 1755, the community was attacked by Nati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beltzville State Park
Beltzville State Park is a Pennsylvania state park in Franklin and Towamensing townships, Carbon County, Pennsylvania in the United States. The park opened in 1972, and was developed around the U.S. Army Corps of Engineers flood control project Beltzville Dam on Pohopoco Creek. The village of Big Creek Valley was vacated in 1966 to make way for Beltzville Lake. Beltzville Lake is a with of shoreline. Beltzville State Park is east of Lehighton just off U.S. Route 209. The park is at an elevation of . Beltzville Lake is a popular fishing destination. Anglers can fish for striped bass, largemouth and smallmouth bass, trout, walleye, perch, and muskellunge. Pohopoco Creek is stocked with trout by the Pennsylvania Fish and Boat Commission. Hunting is permitted at Beltzville State Park. Hunters are expected to follow the rules and regulations of the Pennsylvania Game Commission. The common game species are ruffed grouse, squirrels, pheasant, waterfowl, white-tailed de ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New York City
New York, often called New York City (NYC), is the most populous city in the United States, located at the southern tip of New York State on one of the world's largest natural harbors. The city comprises five boroughs, each coextensive with a respective county. The city is the geographical and demographic center of both the Northeast megalopolis and the New York metropolitan area, the largest metropolitan area in the United States by both population and urban area. New York is a global center of finance and commerce, culture, technology, entertainment and media, academics, and scientific output, the arts and fashion, and, as home to the headquarters of the United Nations, international diplomacy. With an estimated population in 2024 of 8,478,072 distributed over , the city is the most densely populated major city in the United States. New York City has more than double the population of Los Angeles, the nation's second-most populous city. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coal
Coal is a combustible black or brownish-black sedimentary rock, formed as rock strata called coal seams. Coal is mostly carbon with variable amounts of other Chemical element, elements, chiefly hydrogen, sulfur, oxygen, and nitrogen. Coal is a type of fossil fuel, formed when dead plant matter decays into peat which is converted into coal by the heat and pressure of deep burial over millions of years. Vast deposits of coal originate in former wetlands called coal forests that covered much of the Earth's tropical land areas during the late Carboniferous (Pennsylvanian (geology), Pennsylvanian) and Permian times. Coal is used primarily as a fuel. While coal has been known and used for thousands of years, its usage was limited until the Industrial Revolution. With the invention of the steam engine, coal consumption increased. In 2020, coal supplied about a quarter of the world's primary energy and over a third of its Electricity generation, electricity. Some iron and steel-maki ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Summit Hill, Pennsylvania
Summit Hill is a borough in Carbon County, Pennsylvania, United States. It is part of Northeastern Pennsylvania. The population was 3,034 at the 2010 census. Summit Hill was the western terminus of the United States' second operational railway, the Mauch Chunk Switchback Railway. It was the site of some of the earliest coal mines developed in North America, where the Lehigh Coal & Navigation Company began mining in 1792, establishing the town initially as little more than a mining camp with stables and paddocks. History Anthracite coal was discovered on the ridgeline of Sharpe Mountain (now known as Pisgah Mountain) in 1791 by a hunter. News of the find led to the founding of the Lehigh Coal Mining Company, which in 1792 began exploring the area in earnest and buying up promising land. Coal was found in 1794 by Phillip Ginter [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Water Gap
A water gap is a gap that flowing water has carved through a mountain range or mountain ridge and that still carries water today. Such gaps that no longer carry water currents are called wind gaps. Water gaps and wind gaps often offer a practical route for road and rail transport to cross the mountain barrier. Geology A water gap is usually an indication of a river that is older than the current topography. The likely occurrence is that a river established its course when the landform was at a low elevation, or by a rift in a portion of the crust of the earth having a very low stream gradient and a thick layer of unconsolidated sediment. In a hypothetical example, a river would have established its channel without regard for the deeper layers of rock. A later period of uplift would cause increased erosion along the riverbed, exposing the underlying rock layers. As the uplift continued, the river, being large enough, would continue to erode the rising land, cutting thr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Schuylkill River
The Little Schuylkill River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed April 1, 2011 tributary of the Schuylkill River in Northeastern Pennsylvania. It rises south of McAdoo Heights near Haddock, Kline Township in Schuylkill County, Pennsylvania, on top of Broad Mountain. It flows south, then southwest passing through the communities of Tamaqua and New Ringgold. The river joins the Schuylkill River near Port Clinton west of Hawk Mountain. The Pennsylvania Fish and Boat Commission has designated several parts of the stream special trout stocking areas. History The Little Schuylkill River was known as the Tamauguay Creek or River in the 18th and early to mid-19th centuries. Its name is derived from the Lenape word for "beaver" (tëmakwe or tamaqua) and also the Lenape method for using "hunter’s hints,"Mahr, August C., PRACTICAL REASONS FOR ALGONKIAN INDIAN STREAM AND PLACE NAMES, THE OHIO JOURNAL OF SCIE ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pisgah Mountain
Pisgah Mountain, or Pisgah Ridge on older USGS maps, is a ridgeline running from Tamaqua to Jim Thorpe, Pennsylvania from the Little Schuylkill River water gap to the Lehigh River water gap. The mountain runs 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 rising above the boroughs of Lansford, Coaldale, and Tamaqua in the Panther Creek valley. The highest point on Pisgah Mountain is at 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. Pisgah Ridge forms the left bank drainage divide of Panther Creek to its south and the stream's ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lehigh Gap
The Lehigh Gap or Lehigh Water Gap is a water gap located in the townships of Lehigh Township, Northampton County, Pennsylvania, Lehigh, Washington Township, Lehigh County, Pennsylvania, Washington, Lower Towamensing Township, Pennsylvania, Lower Towamensing, and East Penn Township, Pennsylvania, East Penn in the Lehigh Valley and Coal Region regions of eastern Pennsylvania. It was formed by the Lehigh River, where it cuts through the Blue Mountain (Pennsylvania), Blue Mountain in Pennsylvania. The gap allows easy travel between Carbon County, Pennsylvania, Carbon County to the north and Lehigh County, Pennsylvania, Lehigh and Northampton County, Pennsylvania, Northampton counties to the south of the mountain. One of the gap's more distinctive features is Devil's Pulpit, a rock formation that reminds hikers of a pulpit, church pulpit. Lehigh Gap is also the name of a village once known as Weider's Crossing at the south end of the gap in Lehigh and Northampton Counties. Travel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
