Beaver Run (County Line Branch)
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Beaver Run (County Line Branch)
Beaver Run is a tributary of County Line Branch in Northumberland County and Montour County, in Pennsylvania, in the United States. It is approximately long and flows through Lewis Township in Northumberland County and Anthony Township in Montour County. The watershed of the stream mostly consists of agricultural land. The watershed lies over rock of the Onondaga and Old Port Formation, the Keyser and Tonoloway Formation, and the Hamilton Group. It lies over soil of the Chanango-Pope-Holly series, the Hagerstown-Edom-Washington series, and the Watson-Berks-Alvira series. The stream experiences siltation and organic enrichment. A. Joseph Armstrong described Beaver Run as "small and overgrown" in his book ''Trout Unlimited's Guide to Pennsylvania Limestone Streams''. Course Beaver Run begins in eastern Lewis Township, Northumberland County. It flows southeast for a short distance before turning southwest and then south. The stream then crosses Pennsylvania Route 44 and Pennsylvan ...
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West Branch Chillisquaque Creek
West Branch Chillisquaque Creek is a tributary of Chillisquaque Creek. Its watershed spans parts of Northumberland, Montour, Lycoming, and Columbia counties in Pennsylvania. West Branch Chillisquaque Creek is about five miles long. The creek is home to a number of tree species and herb species. There are also five main types of rock formations and four main types of soil in the creek's watershed. Course West Branch Chillisquaque Creek is long. It starts slightly east of Anthony Township and flows west. It flows southwest for some distance before turning nearly due south and passing under Pennsylvania Route 44 on its way through the community of Exchange. West Branch Chillisquaque Creek picks up its only named tributary, County Line Branch, right at its confluence with Chillisquaque Creek. The creek empties into Chillisquaque Creek above Washingtonville. Geology West Branch Chillisquaque Creek is situated in the Ridge-and-Valley province. The creek's headwaters are high ...
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Limestone Township, Montour County, Pennsylvania
Limestone Township is a township in Montour County, Pennsylvania, United States. Geography According to the United States Census Bureau, the township has a total area of 13.4 square miles (34.7 km2), all of it land. Demographics As of the census of 2000, there were 1,004 people, 335 households, and 277 families residing in the township. The population density was . There were 346 housing units at an average density of . The racial makeup of the township was 98.31% White, 0.50% African American, 0.20% from other races, and 1.00% from two or more races. Hispanic or Latino of any race were 0.30% of the population. There were 335 households, out of which 37.0% had children under the age of eighteen living with them; 74.0% were married couples living together, 4.8% had a female householder with no husband present, and 17.3% were non-families. 14.6% of all households were made up of individuals, and 7.8% had someone living alone who was sixty-five years of age or older. ...
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Native Species
In biogeography, a native species is indigenous to a given region or ecosystem if its presence in that region is the result of only local natural evolution (though often popularised as "with no human intervention") during history. The term is equivalent to the concept of indigenous or autochthonous species. Every wild organism (as opposed to a domesticated organism) is known as an introduced species within the regions where it was anthropogenically introduced. If an introduced species causes substantial ecological, environmental, and/or economic damage, it may be regarded more specifically as an invasive species. The notion of nativity is often a blurred concept, as it is a function of both time and political boundaries. Over long periods of time, local conditions and migratory patterns are constantly changing as tectonic plates move, join, and split. Natural climate change (which is much slower than human-caused climate change) changes sea level, ice cover, temperature, and r ...
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Turbotville, Pennsylvania
Turbotville Borough is a borough in Northumberland County, Pennsylvania, United States. The population was 705 at the 2010 census. Geography Turbotville is located at (41.102454, –76.771188). According to the United States Census Bureau, the borough has a total area of 0.4 square mile (1.2 km2), all land. Turbotville is located along the Upper Susquehanna River in the north-central part of Pennsylvania. Turbotville is the northernmost town in Northumberland County, and is surrounded on all sides by Lewis Township. History The greater part of the site of the borough was once owned by Jacob Sechler and wife Catherine, who had received a land grant from Governor Thomas Penn, son of William Penn. Sechler named his land "Green Lawn"; it included the area of present-day Main Street, Church Street, and the Turbotville Cemetery, and extended into present-day Lewis Township. The settlement was originally called Snydertown, after Philip Reifsnyder, believed to be one of the fi ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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Hydric Soil
Hydric soil is soil which is permanently or seasonally saturated by water, resulting in anaerobic conditions, as found in wetlands. Overview Most soils are aerobic. This is important because plant roots respire (that is, they consume oxygen and carbohydrates while releasing carbon dioxide) and there must be sufficient air—especially oxygen—in the soil to support most forms of soil life. Air normally moves through interconnected pores by forces such as changes in atmospheric pressure, the flushing action of rainwater, and by simple diffusion. In addition to plant roots, most forms of soil microorganisms need oxygen to survive. This is true of the more well-known soil animals as well, such as ants, earthworms and moles. But soils can often become saturated with water due to rainfall and flooding. Gas diffusion in soil slows (some 10,000 times slower) when soil becomes saturated with water because there are no open passageways for air to travel. When oxygen levels becom ...
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Soil Series
Soil series as established by the National Cooperative Soil Survey of the United States Department of Agriculture (USDA) Natural Resources Conservation Service are a level of classification in the USDA Soil Taxonomy classification system hierarchy. The actual object of classification is the so-called soil individual, or pedon. Soil series consist of pedons that are grouped together because of their similar pedogenesis, soil chemistry, and physical properties. More specifically, each series consists of pedons having soil horizons that are similar in soil color, soil texture, soil structure, soil pH, consistence, mineral and chemical composition, and arrangement in the soil profile. These result in soils which perform similarly for land use purposes. The soil series concept was originally introduced in 1903. Soil series were originally intended to consist of groups of soils which were thought to be the same in origin but different in texture. Soils were thought to be alike in orig ...
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Hamilton Group
The Hamilton Group is a Devonian-age geological group in the Appalachian region of the United States. It is present in New York, Pennsylvania, Maryland, Ohio, West Virginia, northwestern Virginia and Ontario, Canada. It is mainly composed of marine shale with some sandstone. There are two main formations encompassed by the group: the Mahantango Formation and the Marcellus Shale. In southwestern Virginia, where the two sub-units are not easily distinguishable, the Hamilton Group is broadly equivalent to the Millboro Shale or Millboro Formation. The group is named for the village of Hamilton, New York. These rocks are the oldest strata of the Devonian gas shale sequence. Stratigraphic Setting The Hamilton Group consists of the Mahantango Formation, a gray, dark gray, brown, and olive laminated shale; siltstone; and very fine-grained sandstone or claystone containing marine fossils. The uppermost clay layers of the Mahantango Formation are particularly rich in fossils. It overlie ...
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Ridge And Valley
The Ridge-and-Valley Appalachians, also called the Ridge and Valley Province or the Valley and Ridge Appalachians, are a physiographic province of the larger Appalachian division and are also a belt within the Appalachian Mountains extending from southeastern New York in the north through northwestern New Jersey, westward into Pennsylvania through the Lehigh Valley, and southward into Maryland, West Virginia, Virginia, Kentucky, Tennessee, Georgia, and Alabama. They form a broad arc between the Blue Ridge Mountains and the Appalachian Plateau physiographic province (the Allegheny and Cumberland plateaus). They are characterized by long, even ridges, with long, continuous valleys in between. The river valleys were areas of indigenous settlements for thousands of years. In the historic period, the Cherokee people had towns along many of the rivers in western South Carolina and North Carolina, as well as on the western side of the Appalachian Mountains in present-day Tennessee. ...
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Dissolved Oxygen
Oxygen saturation (symbol SO2) is a relative measure of the concentration of oxygen that is dissolved or carried in a given medium as a proportion of the maximal concentration that can be dissolved in that medium at the given temperature. It can be measured with a dissolved oxygen probe such as an oxygen sensor or an optode in liquid media, usually water. The standard unit of oxygen saturation is percent (%). Oxygen saturation can be measured regionally and noninvasively. Arterial oxygen saturation (SaO2) is commonly measured using pulse oximetry. Tissue saturation at peripheral scale can be measured using NIRS. This technique can be applied on both muscle and brain. In medicine In medicine, oxygen saturation refers to ''oxygenation'', or when oxygen molecules () enter the tissues of the body. In this case blood is oxygenated in the lungs, where oxygen molecules travel from the air into the blood. Oxygen saturation (() sats) measures the percentage of hemoglobin binding s ...
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Pennsylvania Department Of Environmental Protection
The Pennsylvania Department of Environmental Protection (DEP) is the agency in the U.S. state of Pennsylvania responsible for protecting and preserving the land, air, water, and public health through enforcement of the state's environmental laws. It was created by Act 18 of 1995, which split the Department of Environmental Resources into the Department of Environmental Protection and the Department of Conservation and Natural Resources. Its current acting secretary is Ramez Ziadeh. The Department of Environmental Resources was created by Act 275 of 1970, which abolished the Department of Forest and Waters. The Department of Forest and Waters was created by the General Assembly in 1901. The Department of Environmental Protection is charged with the responsibility for development of a balanced ecological system incorporating social, cultural, and economic needs of the commonwealth through development and protection. The department is responsible for the state's land, air, and water ...
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Agriculture
Agriculture or farming is the practice of cultivating plants and livestock. Agriculture was the key development in the rise of sedentary human civilization, whereby farming of domesticated species created food surpluses that enabled people to live in cities. The history of agriculture began thousands of years ago. After gathering wild grains beginning at least 105,000 years ago, nascent farmers began to plant them around 11,500 years ago. Sheep, goats, pigs and cattle were domesticated over 10,000 years ago. Plants were independently cultivated in at least 11 regions of the world. Industrial agriculture based on large-scale monoculture in the twentieth century came to dominate agricultural output, though about 2 billion people still depended on subsistence agriculture. The major agricultural products can be broadly grouped into foods, fibers, fuels, and raw materials (such as rubber). Food classes include cereals (grains), vegetables, fruits, cooking oils, meat, milk, ...
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