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Turkey Hill (Pennsylvania)
Turkey Hill is a hill in Columbia County, Pennsylvania, in the United States. It has an elevation of above sea level. The hill has a flat plateau at the top, but steep slopes on its northern, western, and southern sides. The western and southern parts of the hill have some residential development, while the northern side is mostly forested. The views it provides of the surrounding area have been described as "striking" and "breathtaking". Geography Turkey Hill has an elevation of above sea level. It is mainly situated within Bloomsburg and Scott Township; its highest point is in Scott Township. The hill is entirely within the United States Geological Survey quadrangle of Bloomsburg. It has a topographic prominence of approximately . The hill is part of a larger geographic formation known as Montour Ridge, which begins as a moderately sized hill west of Berwick and runs west, eventually becoming a mountain. In Walter M. Brasch's 1982 book ''Columbia County Place Names'', Tu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hill
A hill is a landform that extends above the surrounding terrain. It often has a distinct Summit (topography), summit. Terminology The distinction between a hill and a mountain is unclear and largely subjective, but a hill is universally considered to be not as tall, or as Grade (slope), steep as a mountain. Geographers historically regarded mountains as hills greater than above sea level, which formed the basis of the plot of the 1995 film ''The Englishman who Went up a Hill but Came down a Mountain''. In contrast, hillwalkers have tended to regard mountains as peaks above sea level. The ''Oxford English Dictionary'' also suggests a limit of and Whittow states "Some authorities regard eminences above as mountains, those below being referred to as hills." Today, a mountain is usually defined in the UK and Ireland as any summit at least high, while the official UK government's definition of a mountain is a summit of or higher. Some definitions include a topographical pro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rose Hill Formation
The Rose Hill Formation is a geologic formation in West Virginia, United States. This formation dates back to the Silurian period, and is a source of iron ore for nearby foundries A foundry is a factory that produces metal castings. Metals are cast into shapes by melting them into a liquid, pouring the metal into a mold, and removing the mold material after the metal has solidified as it cools. The most common metals pr .... History The region has historically had numerous names by different geological agencies. West Virginia adopted the name Rose Hill Formation, and the name appears on the Geologic Map of West Virginia. References * Silurian Maryland Silurian West Virginia Silurian geology of Pennsylvania Silurian geology of Virginia Silurian southern paleotemperate deposits {{Silurian-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Susquehanna River
The Susquehanna River (; Lenape: Siskëwahane) is a major river located in the Mid-Atlantic region of the United States, overlapping between the lower Northeast and the Upland South. At long, it is the longest river on the East Coast of the United States. By watershed area, it is the 16th-largest river in the United States,Susquehanna River Trail Pennsylvania Fish and Boat Commission, accessed March 25, 2010.Susquehanna River , Green Works Radio, accessed March 25, 2010. and also the longest river in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bloomsburg University
Bloomsburg University of Pennsylvania (Bloomsburg, BU or Bloom) is a campus of Commonwealth University of Pennsylvania and it is located in Bloomsburg, Pennsylvania. It is part of the Pennsylvania State System of Higher Education (PASSHE). The campus is accredited by the Middle States Commission on Higher Education with some degree programs accredited by specialized accreditors. History It was established as Bloomsburg Academy in 1839. In 1856, it was renamed Bloomsburg Literary Institute. The name became Bloomsburg Literary Institute and State Normal School in 1869. In 1916, the state of Pennsylvania took control and named it Bloomsburg State Normal School. The name was changed to Bloomsburg State Teachers College in 1927. In 1960, the name was changed to Bloomsburg State College. The name was changed to the current Bloomsburg University of Pennsylvania on July 1, 1983. Bloomsburg terminated its Greek Life program on May 13, 2021. In July 2021, Pennsylvania higher education ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bloomsburg State College
Bloomsburg University of Pennsylvania (Bloomsburg, BU or Bloom) is a campus of Commonwealth University of Pennsylvania and it is located in Bloomsburg, Pennsylvania. It is part of the Pennsylvania State System of Higher Education (PASSHE). The campus is accredited by the Middle States Commission on Higher Education with some degree programs accredited by specialized accreditors. History It was established as Bloomsburg Academy in 1839. In 1856, it was renamed Bloomsburg Literary Institute. The name became Bloomsburg Literary Institute and State Normal School in 1869. In 1916, the state of Pennsylvania took control and named it Bloomsburg State Normal School. The name was changed to Bloomsburg State Teachers College in 1927. In 1960, the name was changed to Bloomsburg State College. The name was changed to the current Bloomsburg University of Pennsylvania on July 1, 1983. Bloomsburg terminated its Greek Life program on May 13, 2021. In July 2021, Pennsylvania higher education o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Turkey (bird)
The turkey is a large bird in the genus ''Meleagris'', native to North America. There are two extant turkey species: the wild turkey (''Meleagris gallopavo'') of eastern and central North America and the ocellated turkey (''Meleagris ocellata'') of the Yucatán Peninsula in Mexico. Males of both turkey species have a distinctive fleshy wattle, called a snood, that hangs from the top of the beak. They are among the largest birds in their ranges. As with many large ground-feeding birds (order Galliformes), the male is bigger and much more colorful than the female. Native to North America, the wild species was bred as domesticated turkey by indigenous peoples. It was this domesticated turkey that later reached Eurasia, during the Columbian exchange. In English, "turkey" probably got its name from the domesticated variety being imported to Britain in ships coming from the Turkish Levant via Spain. The British at the time therefore associated the bird with the country Turkey a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mifflintown Formation
The Mifflintown Formation is a geologic formation in Maryland. It preserves fossils dating back to the Silurian period. See also * List of fossiliferous stratigraphic units in Maryland * Paleontology in Maryland The location of the state of Maryland Paleontology in Maryland refers to paleontological research occurring within or conducted by people from the U.S. state of Maryland. The invertebrate fossils of Maryland are similar to those of neighboring D ... References * Silurian Maryland Silurian geology of Pennsylvania Silurian southern paleotemperate deposits {{Maryland-geologic-formation-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keefer Formation
The Keefer Sandstone is a geologic formation in West Virginia. It dates back to the Silurian period Period may refer to: Common uses * Era, a length or span of time * Full stop (or period), a punctuation mark Arts, entertainment, and media * Period (music), a concept in musical composition * Periodic sentence (or rhetorical period), a concept ... References * Silurian Maryland Silurian West Virginia Silurian geology of Virginia Silurian southern paleotemperate deposits {{Silurian-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Silt
Silt is granular material of a size between sand and clay and composed mostly of broken grains of quartz. Silt may occur as a soil (often mixed with sand or clay) or as sediment mixed in suspension with water. Silt usually has a floury feel when dry, and lacks plasticity when wet. Silt also can be felt by the tongue as granular when placed on the front teeth (even when mixed with clay particles). Silt is a common material, making up 45% of average modern mud. It is found in many river deltas and as wind-deposited accumulations, particularly in central Asia, north China, and North America. It is produced in both very hot climates (through such processes as collisions of quartz grains in dust storms) and very cold climates (through such processes as glacial grinding of quartz grains.) Loess is soil rich in silt which makes up some of the most fertile agricultural land on Earth. However, silt is very vulnerable to erosion, and it has poor mechanical properties, making construction ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Interbedding
In geology, interbedding occurs when beds (layers of rock) of a particular lithology lie between or alternate with beds of a different lithology. For example, sedimentary rocks may be interbedded if there were sea level variations in their sedimentary depositional environment. Intercalation is a special case of interbedding where a layer is variably inserted into an already existing sequence; or where two separate depositional environments in close spatial proximity migrate alternately across the contact. While interbedding has layers that are horizontally flat (or aligned with the angle of the entire stratum), intercalated rock on the other hand has slanted layers that streak through each other (even when it aligns with the stratum). For example intercalated conglomerate and sandstone looks like ripples of different material networked through each other somewhat off the horizontal, as the beds are deposited in a gradient. This is likely due to differing fluvial conditions and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hematitic Sandstone
Hematite (), also spelled as haematite, is a common iron oxide compound with the formula, Fe2O3 and is widely found in rocks and soils. Hematite crystals belong to the rhombohedral lattice system which is designated the alpha polymorph of . It has the same crystal structure as corundum () and ilmenite (). With this it forms a complete solid solution at temperatures above . Hematite naturally occurs in black to steel or silver-gray, brown to reddish-brown, or red colors. It is mined as an important ore mineral of iron. It is electrically conductive. Hematite varieties include ''kidney ore'', ''martite'' (pseudomorphs after magnetite), ''iron rose'' and ''specularite'' (specular hematite). While these forms vary, they all have a rust-red streak. Hematite is not only harder than pure iron, but also much more brittle. Maghemite is a polymorph of hematite (γ-) with the same chemical formula, but with a spinel structure like magnetite. Large deposits of hematite are found in ba ... [...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 beddin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
