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Briar Creek (Susquehanna River Tributary)
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 (Pennsylvania), Knob Mountain, Huntington Mountain, and Lee Mountain me ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brier Creek (Susquehanna River Tributary)
Brier Creek is a river in Otsego County, New York. It converges with the Susquehanna River west-southwest of Otego (village), New York, Otego. References Rivers of New York (state) Rivers of Otsego County, New York {{NewYork-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Briar Creek Township, Columbia County, Pennsylvania
Briar Creek Township is a township in Columbia County, Pennsylvania. It is part of Northeastern Pennsylvania. The population was 2,992 at the 2020 census. Geography Briar Creek Township is in eastern Columbia County, bordered to the east by Luzerne County, to the north by Fishing Creek Township, to the west by North Centre Township, and to the south by the boroughs of Briar Creek and Berwick. The unincorporated community of Foundryville is in the southeastern corner of the township, adjacent to Berwick. The northern boundary of the township follows the ridgecrest of Huntington Mountain, while Lee Mountain is south of it, running nearly parallel to it. The two ridges converge to form Knob Mountain, which is primarily west of the township. According to the United States Census Bureau, the township has a total area of , of which is land and , or 1.04%, is water. Demographics As of the census of 2000, there were 3,061 people, 1,225 households, and 911 families residing in th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Centre Township, Columbia County, Pennsylvania
North Centre Township is a township in Columbia County, Pennsylvania. It is part of Northeastern Pennsylvania. The population was 2,039 at the 2020 census. History The Fowlersville Covered Bridge was listed on the National Register of Historic Places in 1979. Geography The township is located slightly northeast of the center of Columbia County. Knob Mountain forms the northern boundary. Unincorporated communities include North Centre in the northwestern part of the township, and Fowlersville and Dennis Mills in the east. According to the United States Census Bureau, the township has a total area of , of which , or 0.30%, is water. Demographics As of the census of 2000, there were 2,009 people, 735 households, and 580 families residing in the township. The population density was . There were 792 housing units at an average density of . The racial makeup of the township was 98.26% White, 0.85% African American, 0.05% Native American, 0.25% Asian, 0.10% Pacific Islander, 0. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Luzerne County, Pennsylvania
Luzerne County is a county in the U.S. state of Pennsylvania. According to the U.S. Census Bureau, the county has a total area of , of which is land and is water. It is Northeastern Pennsylvania's second-largest county by total area. As of the 2020 census, the population was 325,594, making it the most populous county in the northeastern part of the state. The county seat and largest city is Wilkes-Barre. Other populous communities include Hazleton, Kingston, Nanticoke, and Pittston. Luzerne County is included in the Scranton–Wilkes-Barre–Hazleton Metropolitan Statistical Area, which has a total population of 555,426 as of 2017. On September 25, 1786, Luzerne County was formed from part of Northumberland County. It was named after Chevalier de la Luzerne, a French soldier and diplomat during the 18th century. When it was founded, Luzerne County occupied a large portion of Northeastern Pennsylvania. From 1810 to 1878, it was divided into several smaller counties. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Briar Creek Lake In August
Briar, Briars, Brier, or Briers may refer to: * Briar, or brier, common name for a number of unrelated thorny plants that form thicket People * Brier (surname) * Briers, a surname * Briars (surname) Places * Briar, Missouri, U.S. * Briar, Texas, U.S. * Briars Historic Park, Mount Martha, Victoria, Australia * The Briars (Georgina), Ontario, Canada, a lakeside resort * Brier, Washington, U.S. * Briers, Mississippi, , U.S., a ghost town * Brier Island, Nova Scotia, Canada * Briar Creek (other), or Brier Creek * Briar Hill (other) * Brier Hill (other) Buildings * Briars, Saint Helena, a small pavilion in which Napoleon Bonaparte stayed * The Briars (Natchez, Mississippi), U.S., a historic house * The Briars, Wahroonga, Sydney, Australia, a historic house Fictional characters * Briar Moss, from Tamora Pierce's ''Circle of Magic'' and ''Circle Opens'' quartets * Briar Cudgeon, in ''Artemis Fowl'' * Briar, the evil sister of Rose in Bone ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Silt Loam
Loam (in geology and soil science) is soil composed mostly of sand (particle size > ), silt (particle size > ), and a smaller amount of clay (particle size < ). By weight, its mineral composition is about 40–40–20% concentration of sand–silt–clay, respectively. These proportions can vary to a degree, however, and result in different types of loam soils: sandy loam, silty loam, clay loam, sandy clay loam, silty clay loam, and loam. In the , textural classification triangle, the only soil that is not predominantly sand, silt, or clay is called "loam". Loam soils generally contain more nutrients, moisture, and |
Bedrock
In geology, bedrock is solid Rock (geology), rock that lies under loose material (regolith) within the crust (geology), 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 geophysics, geophysical methods is an important task in most civil engineering projects. Superficial deposition (geology), 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Infiltration Capacity
Infiltration is the process by which water on the ground surface enters the soil. It is commonly used in both hydrology and soil sciences. The infiltration capacity is defined as the maximum rate of infiltration. It is most often measured in meters per day but can also be measured in other units of distance over time if necessary. The infiltration capacity decreases as the soil moisture content of soils surface layers increases. If the precipitation rate exceeds the infiltration rate, runoff will usually occur unless there is some physical barrier. Infiltrometers, permeameters and rainfall simulators are all devices that can be used to measure infiltration rates. Infiltration is caused by multiple factors including; gravity, capillary forces, adsorption and osmosis. Many soil characteristics can also play a role in determining the rate at which infiltration occurs. Factors that affect infiltration Precipitation Precipitation can impact infiltration in many ways. The am ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical erosion procee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Divide
A drainage divide, water divide, ridgeline, watershed, water parting or height of land is elevated terrain that separates neighboring drainage basins. On rugged land, the divide lies along topographical ridges, and may be in the form of a single range of hills or mountains, known as a dividing range. On flat terrain, especially where the ground is marshy, the divide may be difficult to discern. A triple divide is a point, often a summit, where three drainage basins meet. A ''valley floor divide'' is a low drainage divide that runs across a valley, sometimes created by deposition or stream capture. Major divides separating rivers that drain to different seas or oceans are continental divides. The term ''height of land'' is used in Canada and the United States to refer to a drainage divide. It is frequently used in border descriptions, which are set according to the "doctrine of natural boundaries". In glaciated areas it often refers to a low point on a divide where it is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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