Case Mountain
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Case Mountain
Located in the southeastern section of Manchester, Connecticut, the Case Mountain Recreational Area encompasses of combined open space and watershed land Town of Manchester Recreation stretching from the Glastonbury border north to Case Pond. Some trails lead south across the Glastonbury border to a larger area of land owned by the Town of Manchester to maintain the Buckingham Reservoir and provide drinking water to Manchester. The land around the reservoir is open to recreation. While there is a hill named Case Mountain in this area, locals refer to this entire trail system and forest in Manchester and Glastonbury simply as “Case Mountain.” History The Case family were prominent industrialists in Manchester where they operated a paper mill and water bottling facility. In 1861 Alfred Wells Case and his twin brother Albert Willard Case opened the Case Brothers Inc. paper mill in Highland Park where they produced washed cotton supplied to the Union Army during the Civil War. ...
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Manchester, Connecticut
Manchester is a town in Hartford County, Connecticut, United States. As of the 2020 census, the town had a total population of 59,713. The urban center of the town is the Manchester census-designated place, with a population of 36,379 at the 2020 census. The town is named after Manchester, in England. History The area known as Manchester began its recorded history as the camping grounds of a small band of peaceful Native Americans known as the Podunk tribe. The area was settled by colonists around 1673, some 40 years after Thomas Hooker led a group of Puritans from Massachusetts Bay Colony to found Hartford. At the time it was known just as Orford Parish, a name that can still be found on the memorial to the Revolutionary soldiers from the town. The many rivers and brooks provided power for paper, lumber, and textile industries, and the town quickly evolved into an industrial center. The town of Hartford once included the land now occupied by the towns of Manchester, East Ha ...
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Secondary Forest
A secondary forest (or second-growth forest) is a forest or woodland area which has re-grown after a timber harvest or clearing for agriculture, until a long enough period has passed so that the effects of the disturbance are no longer evident. It is distinguished from an old-growth forest (primary or primeval forest), which has not recently undergone such disruption, and complex early seral forest, as well as third-growth forests that result from harvest in second growth forests. Secondary forest regrowing after timber harvest differs from forest regrowing after natural disturbances such as fire, insect infestation, or windthrow because the dead trees remain to provide nutrients, structure, and water retention after natural disturbances. However, often after natural disturbance the timber is harvested and removed from the system, in which case the system more closely resembles secondary forest rather than seral forest. Description Depending on the forest, the development of ...
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American Black Bear
The American black bear (''Ursus americanus''), also called simply a black bear or sometimes a baribal, is a medium-sized bear endemic to North America. It is the continent's smallest and most widely distributed bear species. American black bears are omnivores, with their diets varying greatly depending on season and location. They typically live in largely forested areas, but will leave forests in search of food, and are sometimes attracted to human communities due to the immediate availability of food. The International Union for Conservation of Nature (IUCN) lists the American black bear as a least-concern species, due to its widespread distribution and a large population estimated to be twice that of all other bear species combined. Along with the brown bear (''Ursus arctos''), it is one of only two modern bear species not considered by the IUCN to be globally threatened with extinction. Taxonomy and evolution Despite living in North America, American black bears are not ...
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Vernal Pool
Vernal pools, also called vernal ponds or ephemeral pools, are seasonal pools of water that provide habitat for distinctive plants and animals. They are considered to be a distinctive type of wetland usually devoid of fish, and thus allow the safe development of natal amphibian and insect species unable to withstand competition or predation by fish. Certain tropical fish lineages (such as killifishes) have however adapted to this habitat specifically. Vernal pools are a type of wetland. They can be surrounded by many communities/species including deciduous forest, grassland, lodgepole pine forest, blue oak woodland, sagebrush steppe, succulent coastal scrub and prairie. These pools are characteristic of Mediterranean climates, but occur in many other ecosystems. Generation and annual development During most years, a vernal pool basin will experience inundation from rain/precipitation, followed by desiccation from evapotranspiration. These conditions are commonly associated with M ...
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Eastern White Pine
''Pinus strobus'', commonly called the eastern white pine, northern white pine, white pine, Weymouth pine (British), and soft pine is a large pine native to eastern North America. It occurs from Newfoundland, Canada west through the Great Lakes region to southeastern Manitoba and Minnesota, United States, and south along the Appalachian Mountains and upper Piedmont to northernmost Georgia and perhaps very rarely in some of the higher elevations in northeastern Alabama. It is considered rare in Indiana. The Native American Haudenosaunee named it the "Tree of Peace". It is known as the "Weymouth pine" in the United Kingdom, after Captain George Weymouth of the British Royal Navy, who brought its seeds to England from Maine in 1605. Distribution ''P. strobus'' is found in the nearctic temperate broadleaf and mixed forests biome of eastern North America. It prefers well-drained or sandy soils and humid climates, but can also grow in boggy areas and rocky highlands. In mixed f ...
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Ice Age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the planet. Earth is currently in the Quaternary glaciation. Individual pulses of cold climate within an ice age are termed ''glacial periods'' (or, alternatively, ''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called '' interglacials'' or ''interstadials''. In glaciology, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for th ...
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Glaciers
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 over many years, often centuries. It acquires distinguishing features, such as crevasses and 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 latitudes 35°N and 35°S, glaciers occur only ...
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Boulder
In geology, a boulder (or rarely bowlder) is a rock fragment with size greater than in diameter. Smaller pieces are called cobbles and pebbles. While a boulder may be small enough to move or roll manually, others are extremely massive. In common usage, a boulder is too large for a person to move. Smaller boulders are usually just called rocks or stones. The word ''boulder'' derives from ''boulder stone'', from the Middle English ''bulderston'' or Swedish ''bullersten''.boulder. (n.d.)
Online Etymology Dictionary. Retrieved December 9, 2011, from Dictionary.com website. In places covered by s during s, s ...
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Mountain Biking
Mountain biking is a sport of riding bicycles off-road, often over rough terrain, usually using specially designed mountain bikes. Mountain bikes share similarities with other bikes but incorporate features designed to enhance durability and performance in rough terrain, such as air or coil-sprung shocks used as suspension, larger and wider wheels and tires, stronger frame materials, and mechanically or hydraulically actuated disc brakes. Mountain biking can generally be broken down into five distinct categories: cross country, trail riding, all mountain (also referred to as "Enduro"), downhill, and freeride. This sport requires endurance, core strength and balance, bike handling skills, and self-reliance. Advanced riders pursue both steep technical descents and high incline climbs. In the case of freeride, downhill, and dirt jumping, aerial maneuvers are performed off both natural features and specially constructed jumps and ramps. Mountain bikers ride on off-road trails su ...
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Glastonbury, Connecticut
Glastonbury ( ) is a town in Hartford County, Connecticut, United States, formally founded in 1693 and first settled in 1636. It was named after Glastonbury in Somerset, England. Glastonbury is on the banks of the Connecticut River, southeast of Hartford, Connecticut, Hartford. The town center is defined by the U.S. Census Bureau as a census-designated place (CDP). The population was 35,159 at the 2020 United States Census, 2020 census. History In 1636, 30 families settled in Pyaug, a tract of land belonging to Wethersfield, Connecticut, Wethersfield on the eastern bank of the Connecticut River, bought from the Native American Tribal chief, chief Sowheag for of trading cloth. In 1672, the General Court granted Wethersfield, Connecticut, Wethersfield and Hartford, Connecticut, Hartford permission to extend Pyaug's boundary line to the east. By 1690, Wethersfield had permitted Pyaug residents to form a separate town and, the town of Glassenbury was created in 1693. The ties hav ...
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Somers, Connecticut
Somers is a town in Tolland County, Connecticut. The population was 10,255 at the 2020 census. The town center is listed by the U.S. Census Bureau as a census-designated place (CDP). In 2007, ''Money Magazine'' listed Somers 53rd on its "100 Best Places to Live", based on "economic opportunity, good schools, safe streets, things to do and a real sense of community." Bordering Massachusetts, Somers is considered part of the city of Springfield, Massachusetts NECTA. Somers is southeast of Springfield and considered more oriented toward it than the city of Hartford, which lies to the southwest. History Somers was originally part of the Agawam Plantation in the 17th century. Agawam Plantation became Springfield, Massachusetts, in 1641 and in 1682, the Enfield Parish broke off from the Springfield settlement. In 1689, the first settler, Benjamin Jones, came to Somers in what was then East Enfield about a half mile from the current town center, it was only a summer house and in the ...
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East Hampton, Connecticut
East Hampton is a town in Middlesex County, Connecticut, United States. The population was 12,717 at the 2020 census. The town center village is listed as a census-designated place (CDP). East Hampton includes the boroughs of Cobalt, Middle Haddam, and Lake Pocotopaug. The southern trailhead of the Shenipsit Trail is in Cobalt, and the Airline State Park (a rail trail) has its southern trailhead in East Hampton, at Main Street in the Village Center. The Hurd State Park, Meshomasic State Forest, and Salmon River State Forest are located in town. Comstock's Bridge, more commonly known as the Comstock Covered Bridge and the only remaining covered bridge in eastern Connecticut, spans the Salmon River near Route 16 in East Hampton. The Chatham Historical Society Museum and the Joseph N. Goff House Museum and Cultural Center are located in the town. History The first European-derived settlers of the area arrived in 1739 by sea from Eastham, Massachusetts. They traveled up ...
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