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Mount Minsi
Mount Minsi forms the Pennsylvania side of the Delaware Water Gap, and is the eastern extent of the Blue Mountain. It is composed of sandstone and conglomerates of the Shawangunk Formation. Hiking The easiest route to the summit of Minsi is by way of the Appalachian Trail, from the Lake Lenape trailhead near the town of Delaware Water Gap. The Mount Minsi fire road shares and parallels parts of the same route on the same northwest slopes. Both travel about round trip, and gain of elevation. Climbing The band of exposed metaquartzite cliffs on east face of Minsi hold a number of traditional climbing routes. The earliest of these were put up in 1975, and established routes range from 5.0 to 5.12+. Winter can offer some mixed and ice climbing as well. Gallery File:Appalachian Trail Blaze on the Hike to Mt. Minsi.jpg, Appalachian Trail The Appalachian Trail (also called the A.T.), is a hiking trail in the Eastern United States, extending almost between Springer Mo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Warren County, New Jersey
Warren County is a county located in the U.S. state of New Jersey. As of the 2020 U.S. census, the county's population was 109,632, representing an increase of 940 (0.9%) from the 108,692 residents counted at the 2010 census. The county borders the Delaware River and Easton, Pennsylvania in the Lehigh Valley to its west, the New York City metropolitan area to its east, and The Poconos to its northwest. Warren County is the only county in New Jersey which is not part of the combined statistical areas of New York City or Philadelphia. The most populous place is Phillipsburg, with 14,950 residents at the time of the 2010 census while Hardwick Township had both the largest area and the fewest people with 1,696 residents. Its county seat is Belvidere.New Jersey County Map , |
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 related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Climbing Areas Of The United States
Climbing is the activity of using one's hands, feet, or any other part of the body to ascend a steep topographical object that can range from the world's tallest mountains (e.g. the eight thousanders), to small boulders. Climbing is done for locomotion, sporting recreation, and for competition, and is also done in trades that rely on ascension; such as emergency rescue and military operations. Climbing is done indoors and outdoors and on natural (e.g. rock and ice) and artificial surfaces. Professional mountain guides or rock climbing guides (e.g. the UIAGM), were a significant element in developing the popularity of the sport in the natural environment, and remain so today. Since the 1980s, the development of competition climbing and the availability of artificial climbing walls have dramatically increased the popularity of rock climbing as a sport and led to the emergence of professional rock climbers, such as Wolfgang Güllich, Chris Sharma, Lynn Hill and Catherine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Traditional Climbing
Traditional climbing (or Trad climbing) is a style of rock climbing in which the climber places all the necessary protection gear required to arrest any falls as they are climbing, and then removes it when the pitch is complete (often done by the second/follow-on climber). Traditional bolted aid climbing means the bolts were placed while on lead and/or with hand drills (the bolts tend to be much farther apart than for sport climbs). Traditional climbing carries a higher level of risk than bolted sport climbing, as the climber may not have placed the safety equipment correctly while trying to ascend the route; for some of the world's hardest climbs (e.g. '' Realization/Biographie''), there may not be sufficient cracks or features in the rock that can accept protection gear, and the climb can only be safely attempted by bolting as a sport climb. Overview Characterizing climbing as ''traditional'' distinguishes it from bolted climbing—either trad bolted or sport climbing ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartzite
Quartzite is a hard, non- foliated metamorphic rock which was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of hematite. Other colors, such as yellow, green, blue and orange, are due to other minerals. The term ''quartzite'' is also sometimes used for very hard but unmetamorphosed sandstones that are composed of quartz grains thoroughly cemented with additional quartz. Such sedimentary rock has come to be described as orthoquartzite to distinguish it from metamorphic quartzite, which is sometimes called metaquartzite to emphasize its metamorphic origins. Quartzite is very resistant to chemical weathering and often forms ridges and resistant hilltops. The nearly pure silica conte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Delaware Water Gap, Pennsylvania
Delaware Water Gap is a borough in Monroe County, Pennsylvania, United States. It is located adjacent to the Delaware Water Gap, the pass through which the Lackawanna Corridor and Interstate 80 run across the Pennsylvania-New Jersey border along the Delaware River. The population of Delaware Water Gap was 675 at the 2020 census. History The Delaware Water Gap station (Delaware, Lackawanna and Western Railroad) was added to the National Register of Historic Places in 2002. Geography Delaware Water Gap is located at (40.982028, -75.142624). According to the United States Census Bureau, the borough has a total area of , all land. Demographics As of the 2010 United States Census, there were 746 people living in the borough. The racial makeup of the borough was 81.4% White, 6.3% Black, 0.1% Native American, 3.9% Asian, 0.1% Pacific Islander and 0.9% from two or more races. 7.2% were Hispanic or Latino of any race. As of the census of 2000, there were 744 people, 345 househ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Woodstock, Vermont
Woodstock is the shire town (county seat) of Windsor County, Vermont, United States. As of the 2020 census, the town population was 3,005. It includes the villages of Woodstock, South Woodstock, Taftsville, and West Woodstock. History Chartered by New Hampshire Governor Benning Wentworth on July 10, 1761, the town was a New Hampshire grant to David Page and 61 others. It was named after Woodstock in Oxfordshire, England, as a homage to both Blenheim Palace and its owner, George Spencer, 4th Duke of Marlborough. The town was first settled in 1768 by James Sanderson and his family. In 1776, Joab Hoisington built a gristmill, followed by a sawmill, on the south branch of the Ottauquechee River. The town was incorporated in 1837. Although the Revolution slowed settlement, Woodstock developed rapidly once the war ended in 1783. The Vermont General Assembly met here in 1807 before moving the next year to the new capital at Montpelier. Waterfalls in the Ottauquechee River provid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shawangunk Formation
The Silurian Shawangunk Formation is a mapped bedrock unit in eastern Pennsylvania, New Jersey, and New York (state), New York. It is named for the Shawangunk Ridge for which it is the dominant rock type. The division of the Shawangunk between the Tuscarora Formation and Clinton Group has not been conclusively determined. The shift of nomenclature currently has the divide between Hawk Mountain and Lehigh Gap. Description The Shawangunk is defined as a light to dark-gray, fine to very coarse grained sandstone and Conglomerate (geology), conglomerate, containing a few shale interbeds.Berg, T.M., Edmunds, W.E., Geyer, A.R. and others, compilers, (1980). Geologic Map of Pennsylvania: Pennsylvania Geologic Survey, Map 1, scale 1:250,000. There are also four Member (geology), members of this formation: Tammany, Lizard Creek, Minsi, and Weiders. The Lizard Creek member is described at Lehigh Gap as having conglomerates, sandstone, calcareous sandstone, siltstone, and shale with a few ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hiking
Hiking is a long, vigorous walk, usually on trails or footpaths in the countryside. Walking for pleasure developed in Europe during the eighteenth century.AMATO, JOSEPH A. "Mind over Foot: Romantic Walking and Rambling." In ''On Foot: A History of Walking'', 101-24. NYU Press, 2004. Accessed March 1, 2021. http://www.jstor.org/stable/j.ctt9qg056.7. Religious pilgrimages have existed much longer but they involve walking long distances for a spiritual purpose associated with specific religions. "Hiking" is the preferred term in Canada and the United States; the term "walking" is used in these regions for shorter, particularly urban walks. In the United Kingdom and the Republic of Ireland, the word "walking" describes all forms of walking, whether it is a walk in the park or backpacking in the Alps. The word hiking is also often used in the UK, along with rambling , hillwalking, and fell walking (a term mostly used for hillwalking in northern England). The term bushwalking is end ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kittatinny Mountain
Kittatinny Mountain (Lenape: Kitahtëne) is a long ridge traversing primarily across Sussex County in northwestern New Jersey, running in a northeast-southwest axis, a continuation across the Delaware Water Gap of Pennsylvania's Blue Mountain (also known as Kittatinny Ridge). It is the first major ridge in the far northeastern extension of the Ridge and Valley province of the Appalachian Mountains, and reaches its highest elevation (the state's highest), 1,803 feet, at High Point in Montague Township. Kittatinny Mountain forms the eastern side of Wallpack Valley; the western side comprises the Wallpack Ridge (highest elevation: above sea level. Protected areas Most of the range is publicly owned and protected. In the far northeast, High Point State Park protects the area around High Point itself. Further southwest, Stokes State Forest encompasses much of the range from the southern boundary of High Point State Park to the eastern boundary of the Delaware Water Gap Natio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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