Cabin Run, Columbia County, Pennsylvania
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Cabin Run, Columbia County, Pennsylvania
Cabin Run is a tributary of West Branch Briar Creek in Columbia County, Pennsylvania, in the United States. It is approximately long and flows through North Centre Township. The watershed of the stream has an area of . The waters of the stream are slightly acidic. Its watershed lies over shale and siltstone. Several early attempts at settlement on Cabin Run occurred in 1777 and 1778. Course Cabin Run begins in a valley on Summer Hill in North Centre Township. It flows southeast for a short distance before turning south and flowing parallel to Cabin Run Road for several tenths of a mile. Upon leaving the valley, the stream crosses Fowlersville Road and turns southeast for a short distance before turning south again. After another few tenths of a mile, it reaches its confluence with West Branch Briar Creek. Cabin Run reaches its confluence with West Branch Briar Creek upstream of its mouth. Hydrology The discharge of Cabin Run ranges from 0.17 to 15.7 cubic feet per second. Th ...
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Briar Creek (Susquehanna River)
Briar Creek is a tributary of the Susquehanna River in Columbia County, Pennsylvania, in the United States. It is in length. The stream has a watershed area of 33.0 square miles. It flows through Briar Creek Township and the borough of Briar Creek. The area near the creek was originally inhabited by the Lenni Lenape and the Shawanese. European settlers arrived in the 1770s. Briar Creek has two named tributaries: West Branch Briar Creek and East Branch Briar Creek. The discharge of Briar Creek ranges from 0.06 to 50 cubic feet per second. The water temperature of the creek ranges from to . The rock in the watershed mostly consists of sandstone, siltstone, mudstone, limestone, and shale. There are Pennsylvania State Game Lands in the watershed, as well as a lake known as the Briar Creek Reservoir. In the lake, the most common species of fish is yellow perch. Course Briar Creek begins where Knob Mountain, Huntington Mountain, and Lee Mountain meet in western Briar Creek ...
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Hill
A hill is a landform that extends above the surrounding terrain. It often has a distinct Summit (topography), summit. Terminology The distinction between a hill and a mountain is unclear and largely subjective, but a hill is universally considered to be not as tall, or as Grade (slope), steep as a mountain. Geographers historically regarded mountains as hills greater than above sea level, which formed the basis of the plot of the 1995 film ''The Englishman who Went up a Hill but Came down a Mountain''. In contrast, hillwalkers have tended to regard mountains as peaks above sea level. The ''Oxford English Dictionary'' also suggests a limit of and Whittow states "Some authorities regard eminences above as mountains, those below being referred to as hills." Today, a mountain is usually defined in the UK and Ireland as any summit at least high, while the official UK government's definition of a mountain is a summit of or higher. Some definitions include a topographical pro ...
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Watermill
A watermill or water mill is a mill that uses hydropower. It is a structure that uses a water wheel or water turbine to drive a mechanical process such as milling (grinding), rolling, or hammering. Such processes are needed in the production of many material goods, including flour, lumber, paper, textiles, and many metal products. These watermills may comprise gristmills, sawmills, paper mills, textile mills, hammermills, trip hammering mills, rolling mills, wire drawing mills. One major way to classify watermills is by wheel orientation (vertical or horizontal), one powered by a vertical waterwheel through a gear mechanism, and the other equipped with a horizontal waterwheel without such a mechanism. The former type can be further divided, depending on where the water hits the wheel paddles, into undershot, overshot, breastshot and pitchback (backshot or reverse shot) waterwheel mills. Another way to classify water mills is by an essential trait about their location: tide mills ...
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Fishing Creek (North Branch Susquehanna River)
Fishing Creek is a long tributary of the Susquehanna River in Columbia County, Pennsylvania, Columbia County, Pennsylvania, in the United States. It joins the Susquehanna River near the census-designated place of Rupert, Pennsylvania, Rupert and the town of Bloomsburg, Pennsylvania, Bloomsburg. The drainage basin, watershed has an area of . Nomadic Native Americans arrived in the lower reaches of Fishing Creek around 8000 BCE, and some were spending winters in the upper reaches of the valley by 3000 to 2000 BCE. In the past few centuries, the Fishing Creek area has been home to many industries, watermill, mills, and dams. It drains parts of five Pennsylvania counties: Columbia, Montour County, Pennsylvania, Montour, Sullivan County, Pennsylvania, Sullivan, Luzerne County, Pennsylvania, Luzerne, and Lycoming County, Pennsylvania, Lycoming. The creek's main tributaries include Hemlock Creek (Fishing Creek tributary), Hemlock Creek, Little Fishing Creek, Green Creek (Fishing Creek) ...
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Native Americans In The United States
Native Americans, also known as American Indians, First Americans, Indigenous Americans, and other terms, are the Indigenous peoples of the mainland United States ( Indigenous peoples of Hawaii, Alaska and territories of the United States are generally known by other terms). There are 574 federally recognized tribes living within the US, about half of which are associated with Indian reservations. As defined by the United States Census, "Native Americans" are Indigenous tribes that are originally from the contiguous United States, along with Alaska Natives. Indigenous peoples of the United States who are not listed as American Indian or Alaska Native include Native Hawaiians, Samoan Americans, and the Chamorro people. The US Census groups these peoples as " Native Hawaiian and other Pacific Islanders". European colonization of the Americas, which began in 1492, resulted in a precipitous decline in Native American population because of new diseases, wars, ethni ...
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Moses Van Campen
Major Moses Van Campen (1757–1849) was a soldier during the American Revolutionary War. He was a prominent figure in Pennsylvania and parts of New York. His primary involvement in the Revolutionary War was in fighting against hostile Native American tribes. He began work as a soldier in 1775 and retired from military service in 1783. Van Campen was familiar with Native American methods of warfare. He also participated in the Sullivan Expedition in 1779. Early life Van Campen was born in Hunterdon County, New Jersey on January 21, 1757. His father was a farmer named Cornelius Van Campen. He was of Dutch descent on his father's side and French descent on his mother's side. He was the oldest of six sons and four daughters, and was named after Moses Depue, his grandfather. Shortly following Moses Van Campen's birth, his family moved to Northampton County, Pennsylvania, near the Delaware Water Gap, where Van Campen spent most of his childhood. Van Campen was educated at home until t ...
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Log Cabin
A log cabin is a small log house, especially a less finished or less architecturally sophisticated structure. Log cabins have an ancient history in Europe, and in America are often associated with first generation home building by settlers. European history Construction with logs was described by Roman architect Vitruvius Pollio in his architectural treatise '' De Architectura''. He noted that in Pontus (modern-day northeastern Turkey), dwellings were constructed by laying logs horizontally overtop of each other and filling in the gaps with "chips and mud". Historically log cabin construction has its roots in Scandinavia and Eastern Europe. Although their origin is uncertain, the first log structures were probably being built in Northern Europe by the Bronze Age (about 3500 BC). C. A. Weslager describes Europeans as having: Nevertheless, a medieval log cabin was considered movable property (a chattel house), as evidenced by the relocation of Espåby village in 1557: the ...
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New Jersey
New Jersey is a state in the Mid-Atlantic and Northeastern regions of the United States. It is bordered on the north and east by the state of New York; on the east, southeast, and south by the Atlantic Ocean; on the west by the Delaware River and Pennsylvania; and on the southwest by Delaware Bay and the state of Delaware. At , New Jersey is the fifth-smallest state in land area; but with close to 9.3 million residents, it ranks 11th in population and first in population density. The state capital is Trenton, and the most populous city is Newark. With the exception of Warren County, all of the state's 21 counties lie within the combined statistical areas of New York City or Philadelphia. New Jersey was first inhabited by Native Americans for at least 2,800 years, with the Lenape being the dominant group when Europeans arrived in the early 17th century. Dutch and Swedish colonists founded the first European settlements in the state. The British later seized control o ...
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Middle Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating al ...
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Upper Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating al ...
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Trimmers Rock Formation
Trimmer may refer to: * Trimmer (construction), beam used in construction * Trimmer (electronics), small electrical component * Trimmer (gardening), gardening power tool * Trimmer (surname) * Trimmer, California, community in Fresno County * Laminate trimmer, wood-working tool * Trimmer - a book trimming machine * Coal trimmer, also known as a trimmer, a person who distributes coal on a steam ship * Hair clipper * George Savile, 1st Marquess of Halifax George Savile, 1st Marquess of Halifax, (11 November 1633 – 5 April 1695), was an English statesman, writer, and politician who sat in the House of Commons in 1660, and in the House of Lords after he was raised to the peerage in 1668. Backgr ..., author of ''The Character of a Trimmer'', which was and is often held to describe his own conduct - and therefore he has "the Trimmer" as a nickname See also * * * Trimer (other) * Trim (other) {{disambig ...
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Mahantango Formation
The Devonian Mahantango Formation is a mapped bedrock unit in Pennsylvania, West Virginia, and Maryland. It is named for the North branch of the Mahantango Creek in Perry and Juniata counties in Pennsylvania. It is a member of the Hamilton Group, along with the underlying the Marcellus Formation Shale. South of Tuscarora Mountain in south central Pennsylvania, the lower members of this unit were also mapped as the Montebello Formation. Details of the type section and of stratigraphic nomenclature for this unit as used by the U.S. Geological Survey are available on-line at the National Geologic Map Database. Description The Mahantango Formation is a gray, brown, and olive siltstone and shale, characterized by coarsening-upward cycles. Stratigraphic Setting The Mahantango Formation is typically found conformally overlying the Marcellus Formation, and underlying the Tully Limestone (where present). The Mahantango has been divided into four members: *Tully Limestone: a fossili ...
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