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Fifty Foot Cliff
Fifty Foot Cliff is a glacially carved gneiss cliff in Storrs, Mansfield, Connecticut, with views of Eastern Connecticut. It is, in reality, just over one hundred feet tall, named more for alliterative reasons than anything else. At the top of the ledge is a granite bench in memory of filmmaker Ishmael Rosas. Fifty Foot Cliff is accessed by a trail starting at the Mansfield Historical Society and is part of the Nipmuck Trail. It meets up with several other trails at a cleared space known as "The Junction." Some highlights of the trail include stone walls, cairns, glacial erratics, and a large tree; called the wolf tree, with a rope swing. The Cliff is part of the town-owned Fifty-Foot Cliff Preserve, 102 acres of mostly forested land with a 1.4 mile trail. According to legend, when the cliff was devoid of trees in the late nineteenth and early twentieth centuries, calls from the top of the bluff would carry all the way to nearby Coney Rock. See also *Nipmuck Trail The Nipmuc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Connecticut
Connecticut () is the southernmost state in the New England region of the Northeastern United States. It is bordered by Rhode Island to the east, Massachusetts to the north, New York to the west, and Long Island Sound to the south. Its capital is Hartford and its most populous city is Bridgeport. Historically the state is part of New England as well as the tri-state area with New York and New Jersey. The state is named for the Connecticut River which approximately bisects the state. The word "Connecticut" is derived from various anglicized spellings of "Quinnetuket”, a Mohegan-Pequot word for "long tidal river". Connecticut's first European settlers were Dutchmen who established a small, short-lived settlement called House of Hope in Hartford at the confluence of the Park and Connecticut Rivers. Half of Connecticut was initially claimed by the Dutch colony New Netherland, which included much of the land between the Connecticut and Delaware Rivers, although the firs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Storrs, Connecticut
Storrs is a village and census-designated place (CDP) in the New England town, town of Mansfield, Connecticut, Mansfield in eastern Tolland County, Connecticut, Tolland County, Connecticut, United States. The population was 15,344 at the 2010 United States Census, 2010 census. It is dominated economically and demographically by the main campus of the University of Connecticut and the associated Connecticut Repertory Theatre. Storrs was named for Charles and Augustus Storrs, two brothers who founded the University of Connecticut (originally called the Storrs Agricultural College) by giving the land () and $6,000 in 1881. In the aftermath of September 2005's Hurricane Katrina, ''Slate (magazine), Slate'' named Storrs "America's Best Place to Avoid Death Due to Natural Disaster." Storrs is also home to the new UConn Huskies baseball, University of Connecticut Huskies baseball's home stadium, Elliot Ballpark, which replaced J. O. Christian Field. Geography According to the United Sta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mansfield, Connecticut
Mansfield is a town in Tolland County, Connecticut, United States. The population was 25,892 at the 2020 census. Pequot and Mohegan people lived in this region for centuries before the arrival of English settler-immigrants in the late 17th century. Mansfield was incorporated in October 1702 from the Town of Windham, in Hartford County. The community was named after Major Moses Mansfield, a part owner of the town site. When Windham County was formed on 12 May 1726, Mansfield then became part of that county. A century later, at a town meeting on 3 April 1826, selectmen voted to ask the General Assembly to annex Mansfield to Tolland County. That occurred the following year. The town of Mansfield contains the community of Storrs, which is home to the main campus of the University of Connecticut and the associated Connecticut Repertory Theatre. History English settler-immigrants arrived in the area that is now Mansfield in the late 17th century. The Town of Mansfield was legally ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nipmuck Trail
The Nipmuck Trail is a '' Blue-Blazed'' hiking trail system which meanders through of forests in northeast Connecticut. It is maintained by the Connecticut Forest and Park Association and is considered one of the Blue-Blazed hiking trails. There are two southern trail heads (two tines of a fork) in the south of the town of Mansfield, Connecticut. The southwestern terminus is at a road shoulder parking place on Puddin Lane, and the southeastern terminus is a DEEP parking lot on North Windham Road at the southeast corner of Mansfield Hollow State Park. The northern terminus is at the north end of Breakneck Pond along the Massachusetts border in Nipmuck State Forest. Camping permits may be obtained for up to five separate locations for backpacking. For the Nipmuck Trail travels through the Yale-Myers Forest which is owned by Yale University. The trail also traverses of the University of Connecticut, University of Connecticut's East Campus (the protected Moss tract through the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cairn
A cairn is a man-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the gd, càrn (plural ). Cairns have been and are used for a broad variety of purposes. In prehistoric times, they were raised as markers, as memorials and as burial monuments (some of which contained chambers). In modern times, cairns are often raised as landmarks, especially to mark the summits of mountains. Cairns are also used as trail markers. They vary in size from small stone markers to entire artificial hills, and in complexity from loose conical rock piles to elaborate megalithic structures. Cairns may be painted or otherwise decorated, whether for increased visibility or for religious reasons. A variant is the inuksuk (plural inuksuit), used by the Inuit and other peoples of the Arctic region of North America. History Europe The building of cairns for various purposes goes back into prehistory in Eurasia, ranging in s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Erratics
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The Last Glacial Period ended about 15,000 years ago. The Holocene is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state. Quaternary Period Within the Quaternary, which started about 2.6 million years before present, there have been a number of glacials and interglacials. At least eight glacial cycles have occurred in the last 740,000 years alone. Penultimate Glacial Period The Penultimate Glacial Period (PGP) is the glacial period that occurred before the Last Glacial Period. It began about 194,000 years ago and ended 135,000 years ago, with the beginning of the Eemian interglacial. Last Glacial Period The last glacial period was the most recent glacial period ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coney Rock
Coney Rock is a 600 foot tall, 1,000 foot long, glacially formed granite and gneiss ridge in Storrs, Connecticut, part of the town of Mansfield. It is part of the 200-acre Coney Rock Preserve owned partly by the Town and partly by Joshua's Trust that includes the remains of an old farm, a marsh, a hemlock grove, a hornbeam stand, a birch grove, and glacial erratics, as well as five miles of white and yellow blazed trails. There is a memorial bench at the peak. According to local legend, one can see Rhode Island from the ridge. The cliff is stepped. Ownership Alfred Oden owned Coney Rock until 1933 when he sold the west half to Knute Olsen and the east to Warren Chapin. Olsen's half was bought by the town in 2001 and is part of the 61-acre Dorwart Family Preserve. In response, David Storrs Chapin, Warren's son, sold his half to Joshua's Trust in 2002, who added 9 acres. In 2009, this was connected to Proposal Rocks by another 5.9 acres. History The name Coney Rock is of uncertain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Protected Areas Of Tolland County, Connecticut
Protection is any measure taken to guard a thing against damage caused by outside forces. Protection can be provided to physical objects, including organisms, to systems, and to intangible things like civil and political rights. Although the mechanisms for providing protection vary widely, the basic meaning of the term remains the same. This is illustrated by an explanation found in a manual on electrical wiring: Some kind of protection is a characteristic of all life, as living things have evolved at least some protective mechanisms to counter damaging environmental phenomena, such as ultraviolet light. Biological membranes such as bark on trees and skin on animals offer protection from various threats, with skin playing a key role in protecting organisms against pathogens and excessive water loss. Additional structures like scales and hair offer further protection from the elements and from predators, with some animals having features such as spines or camouflage serving ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Tolland County, Connecticut
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliffs Of The United States
In geography and geology, a cliff is an area of Rock (geology), rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and Dolomite (rock), dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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