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Appalachian Bogs
Appalachian bogs are boreal or hemiboreal ecosystems, which occur in many places in the Appalachian Mountains, particularly the Allegheny and Blue Ridge subranges. Though popularly called bogs, many of them are technically fens. Natural history After the Pleistocene ice ages, species and ecosystems that had shifted southward often survived in local refugia. As a result, cold-adapted ecosystems, such as bogs, remain as far south as East Tennessee and Western North Carolina. Development of land has greatly reduced both the number and acreage of the bogs in North Carolina. Bog ecosystems evolved in humid cold temperate regions and are generally ombrotrophic which means the system is dependent on precipitation for moisture and nutrient inputs. Shady Valley bogs Situated between Holston Mountain and the Iron Mountains, the community of Shady Valley, Tennessee, once contained an estimated 10,000 acres (40 km²) of cranberry bogs. In recent years, The Nature Conservancy has ...
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Restoration Ecology
Restoration ecology is the scientific study supporting the practice of ecological restoration, which is the practice of renewing and restoring degraded, damaged, or destroyed ecosystems and habitats in the environment by active human interruption and action. Effective restoration requires an explicit goal or policy, preferably an unambiguous one that is articulated, accepted, and codified. Restoration goals reflect societal choices from among competing policy priorities, but extracting such goals is typically contentious and politically challenging. Natural ecosystems provide ecosystem services in the form of resources such as food, fuel, and timber; the purification of air and water; the detoxification and decomposition of wastes; the regulation of climate; the regeneration of soil fertility; and the pollination of crops. These ecosystem processes have been estimated to be worth trillions of dollars annually. There is consensus in the scientific community that the current en ...
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Outcropping
An outcrop or rocky outcrop is a visible exposure of bedrock or ancient superficial deposits on the surface of the Earth. Features Outcrops do not cover the majority of the Earth's land surface because in most places the bedrock or superficial deposits are covered by soil and vegetation and cannot be seen or examined closely. However, in places where the overlying cover is removed through erosion or tectonic uplift, the rock may be exposed, or ''crop out''. Such exposure will happen most frequently in areas where erosion is rapid and exceeds the weathering rate such as on steep hillsides, mountain ridges and tops, river banks, and tectonically active areas. In Finland, glacial erosion during the last glacial maximum (ca. 11000 BC), followed by scouring by sea waves, followed by isostatic uplift has produced many smooth coastal and littoral outcrops. Bedrock and superficial deposits may also be exposed at the Earth's surface due to human excavations such as quarrying and buildi ...
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Granite
Granite () is a coarse-grained ( phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or '' granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is near ...
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Northeastern Pennsylvania
Northeastern Pennsylvania (NEPA) is a geographic region of the U.S. state of Pennsylvania that includes the Pocono Mountains, the Endless Mountains, and the industrial cities of Scranton, Wilkes-Barre, Pittston, Hazleton, Nanticoke, and Carbondale. A portion of this region constitutes a part of the New York City metropolitan area. Unlike most parts of the Rust Belt, some of these communities are experiencing a modest population increase, and others, including Monroe and Pike counties, rank among the fastest growing areas of Pennsylvania. Northeastern Pennsylvania borders the Lehigh Valley to its south, Warren County, New Jersey to its east, and Broome County, New York to its north. Area Northeastern Pennsylvania comprises Bradford County, Carbon County, Columbia County, Lackawanna County, Luzerne County, Monroe County, Montour County, Northumberland County, Pike County, Schuylkill County, Sullivan County, Susquehanna County, Wayne County, and Wyoming County. ...
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Tannersville Cranberry Bog
The Tannersville Cranberry Bog or Cranberry Swamp is a sphagnum bog on the Cranberry Creek in Tannersville, Pennsylvania. It is the southernmost boreal bog east of the Mississippi River, containing many black spruce and tamarack trees at the southern limit of their ranges. Technically, it can be classed as an acid fen, as it receives some groundwater flow. The site was designated a National Natural Landmark in December 1974. It was purchased by The Nature Conservancy and the Conservation and Research Foundation in 1957. Like many bogs, its terrain presents an image of solidity, but a liquid mass of decaying peat lies beneath a six-inch (152 mm) layer of sphagnum and a network of supporting tree roots. However, this bog may be viewed from a floating walkway. History The bog began as a "kettle lake" formed approximately 10,000 years ago by a portion of the retreating Wisconsin Glacier ''(named according to geologic epoch, not location)'', which initially covered a de ...
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West Branch Susquehanna Valley
The West Branch Susquehanna Valley of central Pennsylvania, United States, in the Ridge-and-valley Appalachians, is the low-lying area draining into the West Branch Susquehanna River southeast of the Allegheny Front, northeast of the Bald Eagle Valley, southwest of the Wyoming Valley and north of the water gap formed between Shamokin Mountain and Montour Ridge. The river enters the valley after emerging from a deep gorge in the Allegheny Plateau above Lock Haven, then turns east entering a broad alluvial flood plain, where it receives the Bald Eagle Creek after passing the town. The flood plain lies at the foot of the Bald Eagle Mountain ridge, with large fertile farm fields in and around the river's meanders and islands. The valley above the flood plain is a series of knolls below the plateau. Further down the valley, the river receives Pine Creek which has also entered the valley from a deep gorge, Pine Creek Gorge (also known as the Grand Canyon of Pennsylvania). East of ...
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Tamarack Swamp
Tamarack Swamp is a boreal (non-glacial) bog in Sproul State Forest, in Clinton County, Pennsylvania, in the United States. It is named for the tamarack tree, which inhabits the wetland. Numerous other species of plants and animals also inhabit the wetland. The total area of the wetland is 4000 acres. The Tamarack Swamp Natural Area is located in the wetland. Location and description Tamarack Swamp is located in northern Clinton County, Pennsylvania. It is northeast of the community of Tamarack and north of the borough of Renovo and close to Pennsylvania Route 144, which is near the western edge of the wetland. The wetland has a total area of 4000 acres. Its elevation is above sea level. Tamarack Swamp serves as the headwaters of Drury Run. Kettle Creek is located to the north of the wetland. Biology Tamarack Swamp is home to the tamarack tree, which is the only deciduous conifer in Pennsylvania. Most of the trees in it are boreal conifers, though black spruce, and balsam ...
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Ashe County, North Carolina
Ashe County is a county located in the United States state of North Carolina. As of the 2020 census, the population was 26,577. Its county seat is Jefferson. History Historical evidence shows that Ashe County was inhabited by Native Americans, which included the Cherokee, Creek, and Shawnee tribes. Pieces of broken pottery, arrowheads, and other Native American artifacts have been found, indicating their presence. Most of these artifacts have been found in the Old Fields area of Ashe County. The earliest Europeans to explore Ashe County were Bishop August Gottlieb Spangenberg – head of the Moravian Church in America – and his associates, Timothy Horsefield, Joseph Mueller, Henry Antes, Johan Merck, and Herman Loesch. Bishop Spangenberg wrote about his journey in Ashe in a diary that has been preserved by the Moravian church. He was given in Virginia as a place for his fellow Moravians to settle. The only one of Spangenberg's group to return and permanently se ...
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Mountain Bogs National Wildlife Refuge
The Mountain Bogs National Wildlife Refuge is a federally protected wildlife refuge located within multiple western North Carolina counties, United States. The refuge has a total area of over consisting of fee title and conservation easements on privately owned property. In order to respect the wishes of the landowner, and protect sensitive habitat, the refuge is currently not open to the public. The refuge was established in 2015 to conserve Southern Appalachian Bogs in North Carolina and Tennessee, and the U.S. Fish and Wildlife Service plans to add more sites to the refuge, by working with willing landowners. The reserve protects habitat for multiple threatened and endangered species, migratory birds, and important game species. Mountain Bogs is managed by the Piedmont National Wildlife Refuge. See also List of largest National Wildlife Refuges Here is a list of the largest National Wildlife Refuges in the United States. It includes all that are larger than , but excl ...
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Garrett County, Maryland
Garrett County () is the westernmost county of the U.S. state of Maryland. As of the 2020 census, the population was 28,806, making it the third-least populous county in Maryland. Its county seat is Oakland. The county was named for John Work Garrett (1820–1884), president of the Baltimore and Ohio Railroad. Created from Allegany County, Maryland in 1872, it was the last Maryland county to be formed. Garrett County has long been part of the media market of Pittsburgh, Pennsylvania. It is considered to be a part of Western Maryland. The Commonwealth of Pennsylvania is to the north. The Maryland–Pennsylvania boundary is commonly known as the Mason–Dixon line. The eastern border with Allegany County was defined by the Bauer Report, submitted to Governor Lloyd Lowndes, Jr. on November 9, 1898. The Potomac River and State of West Virginia lie to the south and west. Garrett County lies in the Allegheny Mountains, which here form the western flank of the Appalachian ...
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Preston County, West Virginia
Preston County is a county located in the U.S. state of West Virginia. As of the 2020 Census, the population was 34,216. Its county seat is Kingwood. The county was formed from Monongalia County in 1818 and named for Virginia Governor James Patton Preston. Preston County is part of the Morgantown, WV Metropolitan Statistical Area, and is the southernmost county of the Pittsburgh media market. It is the home of The Buckwheat Festival, a county fair known for making buckwheat pancakes. History Native Americans lived in and traveled through what became Preston County as they crossed from the Ohio River watershed (which drains into the Mississippi River), into the Chesapeake Bay watershed. Although white traders and explorers also lived in the county after 1736, and one boundary stone (the Fairfax Stone marking the limits of the North Branch of the River) was laid in 1746, white settlers began arriving in 1766. Traveling by foot or horseback, settlers established log cabins a ...
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