Roaring Creek (Pennsylvania)
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Roaring Creek (Pennsylvania)
Roaring Creek is a tributary of the Susquehanna River in Columbia County and Montour County, in Pennsylvania, in the United States. It is slightly more than long and flows through Roaring Creek Township, Locust Township, Catawissa Township, Cleveland Township, and Franklin Township in Columbia County and Mayberry Township in Montour County. The watershed of the creek has an area of . It has three named tributaries: South Branch Roaring Creek, Lick Run, and Mill Creek. The creek is not considered to be impaired and is not affected by coal mining. However, its watershed has been impacted by human land use. Claystones, conglomerates, sandstones, siltstones, and shales all occur within the watershed. The creek flows through a gorge in its lower reaches, along the border between Columbia County and Montour County. Most of the watershed of Roaring Creek is in Columbia County, but small areas are in Montour County, Northumberland County, and Schuylkill County. More than 4 ...
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Chesapeake Bay
The Chesapeake Bay ( ) is the largest estuary in the United States. The Bay is located in the Mid-Atlantic (United States), Mid-Atlantic region and is primarily separated from the Atlantic Ocean by the Delmarva Peninsula (including the parts: the Eastern Shore of Maryland / Eastern Shore of Virginia and the state of Delaware) with its mouth of the Bay at the south end located between Cape Henry and Cape Charles (headland), Cape Charles. With its northern portion in Maryland and the southern part in Virginia, the Chesapeake Bay is a very important feature for the ecology and economy of those two states, as well as others surrounding within its watershed. More than 150 major rivers and streams flow into the Bay's drainage basin, which covers parts of six states (New York, Pennsylvania, Delaware, Maryland, Virginia and West Virginia) and all of District of Columbia. The Bay is approximately long from its northern headwaters in the Susquehanna River to its outlet in the Atlantic Ocea ...
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Conglomerate (geology)
Conglomerate () is a clastic sedimentary rock that is composed of a substantial fraction of rounded to subangular gravel-size clasts. A conglomerate typically contains a matrix of finer-grained sediments, such as sand, silt, or clay, which fills the interstices between the clasts. The clasts and matrix are typically cemented by calcium carbonate, iron oxide, silica, or hardened clay. Conglomerates form by the consolidation and lithification of gravel. They can be found in sedimentary rock sequences of all ages but probably make up less than 1 percent by weight of all sedimentary rocks. In terms of origin and depositional mechanisms, they are closely related to sandstones and exhibit many of the same types of sedimentary structures, e.g., tabular and trough cross-bedding and graded bedding.Boggs, S. (2006) ''Principles of Sedimentology and Stratigraphy.'', 2nd ed. Prentice Hall, New York. 662 pp. Friedman, G.M. (2003) ''Classification of sediments and sedimentary rocks.'' In G ...
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Meander
A meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. It is produced as a watercourse erodes the sediments of an outer, concave bank ( cut bank) and deposits sediments on an inner, convex bank which is typically a point bar. The result of this coupled erosion and sedimentation is the formation of a sinuous course as the channel migrates back and forth across the axis of a floodplain. The zone within which a meandering stream periodically shifts its channel is known as a meander belt. It typically ranges from 15 to 18 times the width of the channel. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering challenges for local municipalities attempting to maintain stable roads and bridges.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, J.A., eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Charlton, R., 2007. ''Fundamentals ...
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Lake Glory
Lake Glory (also known as Lake Adell Marie or Lake Adele Marie) is a reservoir in Columbia County, Pennsylvania, in the United States. It has a surface area of approximately and is situated in Cleveland Township, Columbia County, Pennsylvania, Cleveland Township. The lake is in the vicinity of Roaring Creek, Pennsylvania Route 487, and Pennsylvania Route 42. It was first developed in the 1950s and by the 1970s was a significant recreational area in the region. The reservoir is located near the Lake Glory Campground. Geography According to The National Map, Lake Glory is not situated on any stream. However, it is located only a few hundred feet from Roaring Creek (Pennsylvania), Roaring Creek. The reservoir has an elevation of above sea level. The lake is entirely within the United States Geological Survey quadrangle (geography), quadrangle of Catawissa. Lake Glory is a manmade lake. It is situated within the Lake Glory Campground. Lake Glory is in the vicinity of Pennsylvania Ro ...
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Pennsylvania Route 42
Pennsylvania Route 42 (PA 42) is a state route located in central Pennsylvania. The southern terminus of the route is at PA 61 in Centralia. The northern terminus is at U.S. Route 220 (US 220) in Laporte. The route heads north through Columbia County and passes through Catawissa before it crosses the Susquehanna River to Bloomsburg. In Bloomsburg, PA 42 forms a concurrency with US 11 and has an interchange with Interstate 80 (I-80). Past Bloomsburg, the route continues north through Millville and runs through the eastern part of Lycoming County. PA 42 heads into Sullivan County and runs concurrent with US 220 between Beech Glen and Muncy Valley before it loops west through Eagles Mere and reaches its terminus in Laporte. PA 42 was originally designated in 1927 to run from US 1 in Oxford north to the New York border in South Waverly. When first designated, the route ran concurrent with US 120 (now PA 61) between Reading and Centralia and US 220 between Laporte and Sout ...
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Slabtown, Pennsylvania
Slabtown is a census-designated place in Columbia County, Pennsylvania, United States. It is part of Northeastern Pennsylvania. The population was 156 at the 2010 census. It is part of the Bloomsburg-Berwick micropolitan area. Geography Slabtown is located in southern Columbia County at (40.905987, -76.408734), in the northern part of Locust Township. It is in the valley of Roaring Creek, a westward-flowing tributary of the Susquehanna River. Slabtown is served by Pennsylvania Route 42, which leads north to Bloomsburg, the county seat, and south over several mountains to Ashland. According to the United States Census Bureau, the Slabtown CDP has a total area of , of which is land and , or 2.86%, is water. Slabtown has hills in the south and east and is flat in the north and west. The land in the CDP is mostly agricultural, with some forest.maps.google.com Demographics As of the census of 2000, there were 105 people, 44 households, and 31 families residing in the CDP. T ...
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Left Bank
In geography, a bank is the land alongside a body of water. Different structures are referred to as ''banks'' in different fields of geography, as follows. In limnology (the study of inland waters), a stream bank or river bank is the terrain alongside the bed of a river, creek, or stream. The bank consists of the sides of the channel, between which the flow is confined. Stream banks are of particular interest in fluvial geography, which studies the processes associated with rivers and streams and the deposits and landforms created by them. Bankfull discharge is a discharge great enough to fill the channel and overtop the banks. The descriptive terms ''left bank'' and ''right bank'' refer to the perspective of an observer looking downstream; a well-known example of this being the sections of Paris as defined by the river Seine. The shoreline of ponds, swamps, estuaries, reservoirs, or lakes are also of interest in limnology and are sometimes referred to as banks. The grade ...
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Right Bank
In geography, a bank is the land alongside a body of water. Different structures are referred to as ''banks'' in different fields of geography, as follows. In limnology (the study of inland waters), a stream bank or river bank is the terrain alongside the bed of a river, creek, or stream. The bank consists of the sides of the channel, between which the flow is confined. Stream banks are of particular interest in fluvial geography, which studies the processes associated with rivers and streams and the deposits and landforms created by them. Bankfull discharge is a discharge great enough to fill the channel and overtop the banks. The descriptive terms ''left bank'' and ''right bank'' refer to the perspective of an observer looking downstream; a well-known example of this being the sections of Paris as defined by the river Seine. The shoreline of ponds, swamps, estuaries, reservoirs, or lakes are also of interest in limnology and are sometimes referred to as banks. The grade ...
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Catawissa Mountain
Catawissa Mountain is a mountain in Columbia County, Pennsylvania, in the United States. Its peak height is above sea level, making it the fifth-highest mountain in Columbia County. Streams that flow near the mountain include Roaring Creek, Catawissa Creek, and some of its tributaries. The mountain is near Nescopeck Mountain and Little Mountain. Sandstones and rock formations such as the Pocono Formation occur on Catawissa Mountain. The community of Catawissa is near Catawissa Mountain. There have also been several roads on or near the mountain in the past. In more recent times, all terrain vehicle trails were established there, as was Pennsylvania State Game Lands Number 58. There are vernal pools on the mountain, which are used as breeding grounds for amphibians. The mountain is part of a much larger tract of forest. Catawissa Mountain is located in southeastern Catawissa Township, southwestern Main Township, eastern Roaring Creek Township, among other places. Geography C ...
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Roaring Creek (Pennsylvania) In Springtime
Roaring Creek may refer to: In North Carolina * Roaring Creek Township, Avery County, North Carolina * Roaring Creek (North Carolina), a tributary of the North Toe River in the above township In Pennsylvania *Roaring Creek (Pennsylvania), a tributary of the North Branch Susquehanna River **South Branch Roaring Creek, a tributary of the above *Roaring Creek Township, Pennsylvania In West Virginia * Roaring Creek (Tygart Valley River), a tributary of the Ohio River * Roaring Creek (Seneca Creek), a tributary of the North Fork South Branch Potomac River Elsewhere *Roaring Creek, Belize Roaring Creek is a small village in the Cayo District of Belize, just north-west of Belmopan. Its name is derived from the creek waterfalls which flow into the Belize River next to the Guanacaste Park area. Roaring Creek has a population of les ..., a small village in the Cayo District See also * * Roaring Branch {{geodis ...
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Quaker
Quakers are people who belong to a historically Protestant Christian set of Christian denomination, denominations known formally as the Religious Society of Friends. Members of these movements ("theFriends") are generally united by a belief in each human's ability to experience Inward light, the light within or see "that of God in every one". Some profess a priesthood of all believers inspired by the First Epistle of Peter. They include those with evangelicalism, evangelical, Holiness movement, holiness, Mainline Protestant, liberal, and Conservative Friends, traditional Quaker understandings of Christianity. There are also Nontheist Quakers, whose spiritual practice does not rely on the existence of God. To differing extents, the Friends avoid creeds and Hierarchical structure, hierarchical structures. In 2017, there were an estimated 377,557 adult Quakers, 49% of them in Africa. Some 89% of Quakers worldwide belong to ''evangelical'' and ''programmed'' branches that hold ...
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Class A Wild Trout Waters
Class A Wild Trout Waters are the highest biomass class given to streams in Pennsylvania by the Pennsylvania Fish and Boat Commission. They are considered to contain the highest-quality naturally reproducing trout populations in Pennsylvania. The first streams received their Class A Wild Trout Waters designations in 1983. There are now hundreds of such waters, comprising nearly of streams. Class A Wild Trout Waters receive certain legal protections. For instance, they are typically classified by the Pennsylvania Department of Environmental Protection as High-Quality Coldwater Fisheries. Most Class A Wild Trout Waters are subject to standard statewide angling regulations by the Pennsylvania Fish and Boat Commission. The official definition of Class A Wild Trout Waters is "streams that support a population of naturally produced trout of sufficient size and abundance to support a long-term and rewarding sport fishery". These streams are considered to be the best angling streams in ...
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