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Phillips Creek
Phillips Creek (also known as Philips Creek) is a tributary of Huntington Creek in Luzerne County, Pennsylvania, in the United States. It is approximately long and flows through Fairmount Township. The watershed of the creek has an area of and has no named tributaries. The creek is considered by the Pennsylvania Fish and Boat Commission to be Class A Wild Trout Waters for brook trout throughout its entire length. Glacial till, alluvium, sandstone, and shale can be found in its vicinity. Its course has been altered by glaciation and it is in the vicinity of North Mountain. At least one bridge has been built over the creek and a number of hunting cabins and cottages existed in the area. The creek's discharge has a 10 percent chance of reaching 915 cubic feet per second in any given year. Course Phillips Creek begins in a deep valley near North Mountain in Fairmount Township. It flows south for nearly a mile before passing through a pond and receiving two unnamed tributaries, one ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fishing Creek (North Branch Susquehanna River)
Fishing Creek is a long tributary of the Susquehanna River in Columbia County, Pennsylvania, in the United States. It joins the Susquehanna River near the census-designated place of Rupert and the town of Bloomsburg. The 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, mills, and dams. It drains parts of five Pennsylvania counties: Columbia, Montour, Sullivan, Luzerne, and Lycoming. The creek's main tributaries include Hemlock Creek, Little Fishing Creek, Green Creek, Huntington Creek, West Branch Fishing Creek, and East Branch Fishing Creek. Public recreation activities include canoeing, birdwatching, and fishing. The creek is known for its trout population, which includes brook, brown and rainbow trout; it also contains many o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sea Level
Mean sea level (MSL, often shortened to sea level) is an average surface level of one or more among Earth's coastal bodies of water from which heights such as elevation may be measured. The global MSL is a type of vertical datuma standardised geodetic datumthat is used, for example, as a chart datum in cartography and marine navigation, or, in aviation, as the standard sea level at which atmospheric pressure is measured to calibrate altitude and, consequently, aircraft flight levels. A common and relatively straightforward mean sea-level standard is instead the midpoint between a mean low and mean high tide at a particular location. Sea levels can be affected by many factors and are known to have varied greatly over geological time scales. Current sea level rise is mainly caused by human-induced climate change. When temperatures rise, mountain glaciers and the polar ice caps melt, increasing the amount of water in water bodies. Because most of human settlement and in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable bedding ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bedrock
In geology, bedrock is solid rock that lies under loose material ( regolith) within the 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 geophysical methods is an important task in most civil engineering projects. Superficial 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 it susceptible to erosion. Bedrock may also experience sub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually relate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bowman Creek
Bowman Creek (also known as Bowmans Creek or Bowman's Creek) is a tributary of the Susquehanna River in Luzerne County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Ross Township and Lake Township in Luzerne County and Noxen Township, Monroe Township, and Eaton Township in Wyoming County. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody and its pH is close to neutral, although it has experienced some problems with acid rain. It has low concentrations of dissolved solids like calcium. The creek is relatively small in its upper reaches, but by Noxen, its width is . It is also relatively shallow in many reaches. Rock formations in the watershed include the Catskill Formation, the Huntley Mountain Formation, Burgoon Sandstone, the Mauch Chunk Formation, the Pottsville Group, and the Pocono Formation. Soil associations in the creek's watershed include the Wellsboro-Morris-Oquaga asso ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Lake
A glacial lake is a body of water with origins from glacier activity. They are formed when a glacier erodes the land and then melts, filling the depression created by the glacier. Formation Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. This is apparent in the Lake District in Northwestern England where post-glacial sediments are normally between 4 and 6 metres deep. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks. These lakes are clearly visible in aerial photos of landforms in regions that were glaciated during the last ice age. The formation and characteristics of glacial lakes vary between location and can be classified into glacial erosion lake, i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gorge
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waterfall
A waterfall is a point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several ways, but the most common method of formation is that a river courses over a top layer of resistant bedrock before falling on to softer rock, which erodes faster, leading to an increasingly high fall. Waterfalls have been studied for their impact on species living in and around them. Humans have had a distinct relationship with waterfalls for years, travelling to see them, exploring and naming them. They can present formidable barriers to navigation along rivers. Waterfalls are religious sites in many cultures. Since the 18th century they have received increased attention as tourist destinations, sources of hydropower, andparticularly since the mid-20th centuryas subjects of research. Definition and terminology A waterfall is genera ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Pass
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap, saddle, col or notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pass. Passes are often found just above the source of a river ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lick Branch (Huntington Creek)
Lick Branch is a tributary of Huntington Creek in Luzerne County, Pennsylvania, in the United States. It is approximately long and flows through Ross Township and Fairmount Township. The watershed of the stream has an area of and has no tributaries. The stream is considered by the Pennsylvania Fish and Boat Commission to be Class A Wild Trout Waters for brook trout throughout its entire length. Glacial till, alluvium, and wetlands can be found in its vicinity. Course Lick Branch begins in a steep valley in the foothills of North Mountain, just south of Pennsylvania Route 118 in western Ross Township. The stream flows southwest and enters Fairmount Township. In Fairmount Township, it turns south and then south-southeast, reentering Ross Township and its valley deepens. In Ross Township, the stream continues flowing south-southwest for more than a mile, while its valley deepens. It then turns southeast and then south, leaving the valley and reaching its confluence with Hunting ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Overbank
An overbank is an alluvial geological deposit consisting of sediment that has been deposited on the floodplain of a river or stream by flood waters that have broken through or overtopped the banks. The sediment is carried in suspension, and because it is carried outside of the main channel, away from faster flow, the sediment is typically fine-grained. An overbank deposit usually consists primarily of fine sand, silt and clay. Overbank deposits can be beneficial because they refresh valley soils. Overbank deposits can also be referred to as floodplain deposits. Examples include natural levees and crevasse splays. Geomorphology Floodplains are far wider than the channel they border, reaching widths of up to 100 kilometers, and their length is 10 times that. They are thin and roughly planar in shape. Unlike channel bars, which often build horizontally, overbank deposits build vertically. Depositional processes and facies Overbank deposits are fine-grained and accumulate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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