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Archbald Pothole State Park
Archbald Pothole State Park is a Pennsylvania state park in Archbald, Lackawanna County, Pennsylvania. The focal point of the park is Archbald Pothole. The pothole is a remnant of the Wisconsin Glacial Period, deep with a largest diameter of by . It has drawn tourists since just after it was discovered in 1884. Archbald Pothole State Park is on U.S. Route 6 Business in the borough of Archbald. The park is at an elevation of . History A coal miner, Patrick Mahon, discovered Archbald Pothole in 1884. Mahon was extending a mine shaft. When he set off a blast of explosives, water and stones came pouring into the mine shaft. He and the other miners fled the scene fearing for their lives. The manager of the mining company, Edward Jones, came to investigate. Jones ordered that the area be cleared of the fallen debris. Almost 1,000 tons of small rounded stones were removed and Jones soon realized that the vertical tunnel discovered by the coal miners was a large pothole. Af ...
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Archbald, Pennsylvania
Archbald is a borough in Lackawanna County, Pennsylvania, United States. It is part of Northeastern Pennsylvania and is named for James Archbald, the first mayor of Carbondale, Pennsylvania. Before being renamed in Archbald's honor, the name of the settlement was White Oak Run. Most of the original settlers were Irish Catholics, fleeing the Great Famine. The population was 7,348 at the 2021 census. The village of Eynon is incorporated into Archbald. Geography Archbald is located at . According to the United States Census Bureau, the borough has a total area of 17.10 sqmi (44.29 km2), of which 17.09 smi (44.26 km2) is land and 0.014 sqmi (0.036 km2) (0.06%) is water. Demographics 2010 census As of the 2010 United States Census there were 7,011 people, 2,802 households, and 1,948 families in the borough. The population density was 408.7/sqmi (157.9/km). There were 2,952 housing units at an average density of 173/sqmi (67.5/km). The racial makeup of the borough ...
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Diameter
In geometry, a diameter of a circle is any straight line segment that passes through the centre of the circle and whose endpoints lie on the circle. It can also be defined as the longest Chord (geometry), chord of the circle. Both definitions are also valid for the diameter of a sphere. In more modern usage, the length d of a diameter is also called the diameter. In this sense one speaks of diameter rather than diameter (which refers to the line segment itself), because all diameters of a circle or sphere have the same length, this being twice the radius r. :d = 2r \qquad\text\qquad r = \frac. The word "diameter" is derived from (), "diameter of a circle", from (), "across, through" and (), "measure". It is often abbreviated \text, \text, d, or \varnothing. Constructions With straightedge and compass, a diameter of a given circle can be constructed as the perpendicular bisector of an arbitrary chord. Drawing two diameters in this way can be used to locate the center of ...
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Wilkes-Barre, Pennsylvania
Wilkes-Barre ( , alternatively or ) is a city in Luzerne County, Pennsylvania, United States, and its county seat. Located at the center of the Wyoming Valley in Northeastern Pennsylvania, it had a population of 44,328 in the 2020 census. It is the second-largest city, after Scranton, Pennsylvania, Scranton, in the Wyoming Valley, Scranton–Wilkes-Barre–Hazleton, PA Metropolitan Statistical Area, which had a population of 567,559 as of the 2020 United States census, 2020 census, making it the fifth-largest metropolitan area in Pennsylvania after the Delaware Valley, Greater Pittsburgh, the Lehigh Valley, and Harrisburg–Carlisle metropolitan statistical area, Greater Harrisburg. The contiguous network of five City, cities and more than 40 boroughs all built in a straight line in Northeastern Pennsylvania's urban core act, culturally and logistically as one continuous city, so while the city of Wilkes-Barre itself is a mid-sized city, the larger Scranton/Wilkes-Barre Urban ...
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Seven Tubs Natural Area
Seven Tubs Recreation Area is a publicly accessible recreation area located in Luzerne County, Pennsylvania, and owned by the Pennsylvania Department of Conservation and Natural Resources. Continuously flowing glacial meltwater gouged a line of smooth tubs in gritty sandstone over 12,000 years ago. The tubs are potholes formed by the flowing water. The site is part of a recreation area in the Pennsylvania mountains about south of downtown Wilkes-Barre.Litchman , Lori. "Seven Tubs Natural Area, Luzerne County." Greentreks Network. 2006. 19 Mar 2008 . The site is popular among hikers for its easy accessibility and beginner-level hiking environment. Geology The glaciers of the Ice Age were instrumental in shaping the physical features of the natural world that we see today. They too are responsible for the formations of the tubs. As ice melts over long periods of time, its eroding capabilities become much more substantial. Glacial melting produced large volumes of flowing wate ...
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Moraine
A moraine is any accumulation of unconsolidated debris (regolith and Rock (geology), rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines are those formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French language, French , which in turn is derived from the Savoyard dialect, Savoyard Italian ('mound of e ...
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Pocono Mountains
The Pocono Mountains, commonly referred to as the Poconos (), 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 name Pocono is derived from the Munsee word Pokawachne, which means "Creek Between Two Hills". Much of the Poconos region lies within the Greater New York–Newark, NY–NJ–CT–PA Combined Statistical Area. The wooded hills and valleys have long been a popular recreation area, accessible within a two-hour drive to millions of metropolitan area residents, with many Pocono communities having resort hotels with fishing, hunting, skiing, and other sports facilities. Although referred to usually as a mountain range, the area is a dissected plateau, a sub-section of the larger Allegheny Plateau, forming a escarpment. The topological mountains are also ...
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Hickory Run State Park
Hickory Run State Park is a Pennsylvania state park in Kidder and Penn Forest Townships in Carbon County, Pennsylvania in the United States. The park is spread across the Pocono Mountains. The park is easily accessible from Interstate 476 and Interstate 80. Hickory Run State Park was chosen by the Pennsylvania Department of Conservation and Natural Resources (DCNR) and its Bureau of Parks as one of "25 Must-See Pennsylvania State Parks". Recreation The park supports many activities, some of which vary seasonally. During the summer months, swimming is available in Sand Spring Lake. Swimming is allowed only at one designated swimming area, which is a sand beach, of Sand Spring Lake. Furthermore, this swimming area is open for swimming only from late May to mid-September. Because there are no lifeguards, swimming is at your own risk. In winter, the frozen lake can be used for ice skating. Seasonal hunting is permitted in many areas of the park, with white-tailed deer, black b ...
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Wisconsin Glaciation
The Wisconsin glaciation, also called the Wisconsin glacial episode, was the most recent glacial period of the North American ice sheet complex, peaking more than 20,000 years ago. This advance included the Cordilleran Ice Sheet, which nucleated in the northern North American Cordillera; the Innuitian ice sheet, which extended across the Canadian Arctic Archipelago; the Greenland ice sheet; and the massive Laurentide Ice Sheet, which covered the high latitudes of central and eastern North America. This advance was synchronous with global glaciation during the last glacial period, including the North American Glacier#Classification_by_size,_shape_and_behavior, alpine glacier advance, known as the Pinedale glaciation. The Wisconsin glaciation extended from about 75,000 to 11,000 years ago, between the Sangamonian Stage and the current interglacial, the Holocene. The maximum ice extent occurred about 25,000–21,000 years ago during the last glacial maximum, also known as the ''Late W ...
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Glacier
A glacier (; or ) is a persistent body of dense ice, a form of rock, that is constantly moving downhill under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land“Glacier, N., Pronunciation.” Oxford English Dictionary, Oxford UP, June 2024, https://doi.org/10.1093/OED/7553486115. Accessed 25 Jan. 2025. and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on ever ...
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Waterfall
A waterfall is any point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several ways, but the most common method of formation is that a river courses over a top layer of resistant bedrock before falling onto softer rock, which erodes faster, leading to an increasingly high fall. Waterfalls have been studied for their impact on species living in and around them. Humans have had a distinct relationship with waterfalls since prehistory, travelling to see them, exploring and naming them. They can present formidable barriers to navigation along rivers. Waterfalls are religious sites in many cultures. Since the 18th century, they have received increased attention as tourist destinations, sources of hydropower, andparticularly since the mid-20th centuryas subjects of research. Definition and terminology A waterfal ...
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Rapids
Rapids are sections of a river where the river bed has a relatively steep stream gradient, gradient, causing an increase in water velocity and turbulence. Flow, gradient, constriction, and obstacles are four factors that are needed for a rapid to be created. Physical factors Rapids are hydrology, hydrological features between a ''run'' (a smoothly flowing part of a stream) and a ''waterfall#Types, cascade''. Rapids are characterized by the river becoming shallower with some Rock (geology), rocks exposed above the flow surface. As flowing water splashes over and around the rocks, air bubbles become mixed in with it and portions of the surface acquire a white color, forming what is called "whitewater". Rapids occur where the stream bed, bed material is highly resistant to the erosive power of the stream in comparison with the bed downstream of the rapids. Very young streams flowing across solid rock may be rapids for much of their length. Rapids cause water aeration of the stream ...
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Bedrock
In geology, bedrock is solid rock that lies under loose material ( regolith) within the crust of Earth or another terrestrial planet. Definition Bedrock is the solid rock that underlies looser surface material. An exposed portion of bedrock is often called an outcrop. The various kinds of broken and weathered rock material, such as soil and subsoil, that may overlie the bedrock are known as regolith. Engineering geology The surface of the bedrock beneath the soil cover (regolith) is also known as ''rockhead'' in engineering geology, and its identification by digging, drilling or geophysical methods is an important task in most civil engineering projects. Superficial deposits can be very thick, such that the bedrock lies hundreds of meters below the surface. Weathering of bedrock Exposed bedrock experiences weathering, which may be physical or chemical, and which alters the structure of the rock to leave it susceptible to erosion. Bedrock may also experience subsur ...
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