Provin Mountain is a very narrow traprock mountain ridge located in the Connecticut River Valley of Massachusetts . It is part of the Metacomet Ridge which extends from Long Island Sound near New Haven, Connecticut , north through the Connecticut River Valley of Massachusetts to the Vermont border. Provin Mountain is known for its scenic cliffs, unique microclimate ecosystems, and rare plant communities. It is traversed by the 114 mile (183 km) Metacomet-Monadnock Trail .
107-580: Provin Mountain rises steeply between 200 and 450 feet (61 and 137 m) above the river valleys of the Connecticut River and Westfield River below, with a high point of 600 feet (183 m) above sea level. It is roughly 5 miles (8 km) long but is not much more than 0.5 miles (800 m) wide at its widest point. Although, the steepness of the terrain makes the actual square mileage much larger. The Provin Mountain ridgeline extends from
214-643: A 1635 scouting party commissioned by William Pynchon to found a city on the river's most advantageous site for commerce and agriculture. Pynchon's Massachusetts scouts located the Pocomtuc village of Agawam, where the Bay Path trade route crossed the Connecticut River at two of its major tributaries—the Chicopee River to the east and Westfield River to the west—and just north of Enfield Falls,
321-493: A boulder cave located on the west side of Rattlesnake Mountain , is an historic landmark of the town of Farmington. A plaque affixed to the cave reads, "Said Warren, according to legend, after being flogged for not going to church, tried to burn the village of Farmington. He was pursued into the mountains, where some Indian squaws hid him in this cave." The personage of Will Warren has never been vindicated historically, and may have been an amalgamation of several individuals. The cave
428-525: A campaign of water conservation. Demand was reduced to sustainable levels by 1989, reaching approximately a 25% margin of safety by 2009. The Connecticut River is the largest river ecosystem in New England. Its watershed spans Connecticut, Massachusetts, New Hampshire, Vermont, small portions of Maine, and the Canadian province of Quebec. The Connecticut River rises from Fourth Connecticut Lake ,
535-576: A center of wildlife and recreation. Starting about 1865, the river was used for massive logging drives from Third Connecticut Lake to initially water powered sawmills near Enfield Falls. Trees cut adjacent to tributary streams including Perry Stream and Indian Stream in Pittsburg, New Hampshire , Halls Stream on the Quebec –New Hampshire border, Simms Stream , the Mohawk River , and
642-494: A combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Massachusetts. Provin Mountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Provin Mountain). Provin Mountain is used for hiking , mountain biking , cross country skiing , hunting , and snowshoeing ; many cliffs provide sweeping views of
749-885: A diversity of colonial organisms including bryozoa . Freshwater sponges the size of dinner plates have been found by scuba divers at depths of more than 130 feet (40 m), thought to be the deepest location of the river, around the French King Bridge in Erving, Massachusetts. Mussels, eels, and northern pike were also observed there. There are several species of anadromous and catadromous fish, including brook trout , winter flounder , blueback herring , alewife , rainbow trout , large brown trout , American shad ( Alosa sapidissima ), hickory shad , smallmouth bass , Atlantic sturgeon , striped bass ( Morone saxatilis ), American eel , sea lamprey , and endangered shortnose sturgeon and dwarf wedgemussels. Additionally,
856-522: A dry-loving species, clings to the barren edges of cliffs. Prickly pear cactus has been recorded on the south-facing slopes of Ragged Mountain. Backslope plant communities tend to be more similar to the adjacent upland plateaus containing species common to the northern hardwood and oak-hickory forest types. Eastern hemlock crowds narrow ravines, blocking sunlight and creating damp, cooler growing conditions with associated cooler climate plant species. Talus slopes are especially rich in nutrients and support
963-417: A museum, was created on 250 acres (1.0 km ) of Farmington Mountain as a country estate for wealthy industrialist Alfred Atmore Pope , to the designs of his daughter Theodate Pope Riddle in 1901. Theodate inherited the house after her parents' deaths, and prior to her own passing in 1946 willed Hill-Stead Museum as a memorial to her parents. Hill-Stead comprises 152 acres (0.62 km ). Buildings include
1070-564: A number of calcium-loving plants uncommon in Massachusetts. Many bogs, ponds, and reservoirs lie cupped between trap rock ridge shelves, demonstrating the value of these ridges as important aquifers and wetland ecosystem habitats. Because the Metacomet Ridge generates such varied terrain, it is the home of several plant and animal species that are state-listed or globally rare. The Traprock Wilderness Recovery Strategy (1991)
1177-642: A potential hazard. The northern copperhead snake , while considered rare, does inhabit portions of the Metacomet Ridge in Connecticut. Poison ivy is native to the Metacomet Trail environs, prolific in some areas. The Metacomet Trail passes through public land (state parks, town parks, and municipal watershed areas), land managed by conservation non-profit organizations, private land under conservation easement, and unprotected private land via permission of individual land owners. Significant threats to
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#17327878573631284-526: A seasonal migration path for raptors . Viewshed from the ledges include agrarian land, suburbs, small towns, river corridors, the eastern Berkshires ridgeline, and metropolitan Meriden and Hartford. The Metacomet Trail passes through land located within the following incorporated towns, from south to north: Berlin , Meriden , Southington , New Britain , Plainville , Farmington , West Hartford , Avon , Bloomfield , Simsbury , East Granby , and Suffield, Connecticut The Metacomet Ridge that forms
1391-671: A series of slow-flowing basins from Lake Francis Dam in Pittsburg, New Hampshire, to the Holyoke Dam at South Hadley Falls in Massachusetts. Among the most extensively dammed rivers in the United States, the Connecticut may soon flow at a more natural pace, according to scientists at the University of Massachusetts at Amherst, who have devised a computer that – "in an effort to balance human and natural needs" – coordinates
1498-565: A small pond 300 yards (270 m) south of the Canada–United States border in the town of Pittsburg, New Hampshire , at an elevation of 2,670 feet (810 m) above sea level. It flows through the remaining Connecticut Lakes and Lake Francis for 14 miles (23 km), all within the town of Pittsburg, and then widens as it delineates 255 miles (410 km) of the border between New Hampshire and Vermont. The river drops more than 2,480 feet (760 m) in elevation as it winds south to
1605-503: A stone observation tower built on East Peak , and Mirror Lake, nestled between the high ledges of East Peak and South Mountain , are considered particularly scenic. Heublein Tower , 165 feet (50 m) tall and 1,040 feet (317 m) above sea level, built for Gilbert F. Heublein in 1914 on the summit crest of Talcott Mountain as a summer retreat and home, was designed to withstand winds of 100 mph (160 km/h). Put up for sale in
1712-482: A toll on Connecticut Colony ships entering Boston Harbor . Connecticut was largely dependent on sea trade with Boston and therefore permanently dropped its tax on Springfield, but Springfield allied with Boston nonetheless, drawing the first state border across the Connecticut River. The Fort at Number 4 in Charlestown, New Hampshire , was the northernmost British colonial presence on the Connecticut River until
1819-432: A unique "postpile" appearance. Huge slopes made of fractured basalt scree are visible beneath many of the cliffs along the Metacomet Trail. The Metacomet Ridge was the product of several massive lava flows hundreds of feet deep that welled up in faults created by the rifting apart of North America from Eurasia and Africa . The basalt floods of lava occurred over a period of 20 million years. Erosion occurring between
1926-538: Is accessible from the Metacomet Trail. The Hanging Hills are allegedly stalked by the supernatural presence of the "Black Dog of the Hanging Hills", an American example of traditional English Black dog folklore. According to local mythology extant since at least the early 19th century, the Black Dog manifests as a small black dog, often gregarious in nature, who leaves no footprints and makes no sound. To see
2033-685: Is also often referred to as the 3-M, MMM or Metacomet-Monadnock-Mattabesett trail. The New England National Scenic Trail includes all or almost all of the MMM trails as well as the new extension trail from the southernmost point on the Mattabesett Trail through Guilford, Connecticut to the northern shore of Long Island Sound. The Metacomet Trail extends from the Connecticut / Massachusetts border south through Hartford and northern New Haven counties in Connecticut. The southern terminus of
2140-769: Is an important conduit of many anadromous fish, such as American shad , lamprey , and Atlantic salmon . American eels are also present, as are predators of these migratory fish including striped bass . Shad run as far north as Holyoke, Massachusetts where they are lifted over the Holyoke Dam by a fish elevator. This station publishes annual statistics of the run, and has recorded an occasional salmon. They pass an additional elevator in Turners Falls, Massachusetts , and make it at least as far as Bellows Falls, Vermont . Harbor seals have been recorded traveling upriver as far north as Holyoke in pursuit of migratory fish; it
2247-594: Is home to some of the northeastern United States' most productive farmland, as well as the Hartford–Springfield Knowledge Corridor , a metropolitan region of approximately two million people surrounding Springfield, Massachusetts , and Hartford, Connecticut . The word "Connecticut" is a corruption of the Mohegan word quinetucket and Nipmuc word kwinitekw , which mean "beside the long, tidal river". The word came into English usage during
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#17327878573632354-480: Is never more than a mile or two from a public road. However, cliffs and steep terrain make access much more difficult in some areas. There are no camping facilities along the trail and camping is generally prohibited. Trail descriptions are available from a number of commercial and non-commercial sources, and a complete guidebook is published by the Connecticut Forest and Park Association Weather along
2461-693: Is now inundated by the impoundments of dams built after this time. The Treaty of Paris (1783) that ended the American Revolutionary War created a new international border between New Hampshire and the Province of Canada at "northwesternmost headwaters of the Connecticut". Several streams fit this description, and thus a boundary dispute led to the short-lived Indian Stream Republic , which existed from 1832 to 1835. The broad, fertile Connecticut River Valley attracted agricultural settlers and colonial traders to Hartford, Springfield, and
2568-652: Is one of the few major rivers in the United States without a major city at its mouth because of this obstacle. Major cities on the Connecticut River are Hartford and Springfield, which lie 45 and 69 miles (70 and 110 km) upriver respectively. The Nature Conservancy named the Connecticut River's tidelands one of the Western Hemisphere's "40 Last Great Places", while the Ramsar Convention on Wetlands listed its estuary and tidal wetlands as one of 1,759 wetlands of international importance. In 1997,
2675-405: Is possible that they ranged farther upstream before the dam was built. In the southernmost portions in southern Connecticut near Long Island Sound, dolphins are spotted on occasion. There are 12 species of freshwater mussels. Eleven of them occur in the mainstem of the Connecticut; the brook floater is found only in small streams and rivers. Species diversity is higher in the southern part of
2782-509: Is to picture a layer cake tilted slightly up with some of the frosting (the sedimentary layer) removed in between. The sedimentary rock of the Metacomet ridge is well known for its fossils, especially dinosaur tracks. The Metacomet Ridge hosts a combination of microclimates unusual in New England. Dry, hot upper ridges support oak savannas , often dominated by chestnut oak and a variety of understory grasses and ferns. Eastern red cedar ,
2889-486: Is well known for Connecticut shade tobacco . The Connecticut River is influenced by the tides as far north as Enfield Rapids in Windsor Locks, Connecticut , approximately 58 miles (93 km) north of the river's mouth. Two million residents live in the densely populated Hartford-Springfield region, which stretches roughly between the college towns of Amherst, Massachusetts, and Middletown, Connecticut. Hartford,
2996-743: The Appalachian Mountain Club [1] , the Green Mountain Club [2] , and the Connecticut Forest and Park Association . Following the pioneering effort of the Green Mountain Club in the inauguration of Vermont's Long Trail in 1918, the Connecticut Forest and Park Association, spearheaded by Edgar Laing Heermance, created the 23-mile (37 km) Quinnipiac Trail on the Metacomet Ridge in southern Connecticut in 1928 and soon followed it up with
3103-617: The CCC , contributed aid and manpower to the effort. Flooding of roads isolated the city for a time. When the water receded, it left behind silt-caused mud which in places was 3 feet (1 m) thick; the recovery effort in Springfield, at the height of the American Great Depression , took approximately a decade. Overall, the flood caused 171 deaths and US$ 500 million (US$ 11,000,000,000 with inflation ) in damages. Across
3210-590: The Connecticut border (near the Suffield hamlet of Rising Corner) to the Westfield River on the tri-border of Westfield , West Springfield , and Agawam, Massachusetts . It lies within the towns of Southwick , Agawam, and Westfield. The Metacomet Ridge continues north from the Westfield River as East Mountain and continues south into Connecticut as West Suffield Mountain . The south side of
3317-661: The Hill-Stead museum in Farmington, Connecticut , notable for its French impressionist painting collection and gardens; and Hubbard Park of the Hanging Hills of Meriden, designed with the help of famous landscape architect Frederick Law Olmsted and crowned with a small observation tower known as Castle Craig. The trap rock ridges and talus slopes of the Metacomet Ridge are also home to several unique microclimate ecosystems that support species of plants that are unusual or endangered in this part of New England , and are
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3424-738: The Mohawk , Mahican , and Iroquois tribes. The Pennacook tribe mediated many early disagreements between colonists and other Indian tribes, with a territory stretching roughly from the Massachusetts border with Vermont and New Hampshire, northward to the rise of the White Mountains in New Hampshire. The Western Abenaki ( Sokoki ) tribe lived in the Green Mountains region of Vermont but wintered as far south as
3531-676: The Monadnock-Sunapee Greenway in New Hampshire continue the footway north from the Metacomet Trail another 160 miles (260 km) to central New Hampshire. The 50-mile (80 km) Mattabesett Trail picks up where the Metacomet Trail leaves off in Berlin and continues south to Totoket Mountain then northeast to the Connecticut River in Middletown . Significant networks of shorter hiking trails intersect
3638-563: The New England National Scenic Trail , which also includes the Mattabesett Trail and Metacomet-Monadnock Trail . The Connecticut Forest and Park Association (CFPA) provides commemorative patches as recognition to hikers completing the entire length of one of the three original Blue-Blazed trails in Connecticut (Quinnipiac, Metacomet and Mattabesett). The Metacomet Trail patch can be obtained for
3745-617: The New Netherland colony. In 1623, Dutch traders constructed a fortified trading post at the site of Hartford, Connecticut , called the Fort Huys de Hoop ("Fort House of Hope"). Four separate Puritan -led groups also settled the fertile Connecticut River Valley, and they founded the two large cities that continue to dominate the Valley: Hartford (est. 1635) and Springfield (est. 1636). The first group of pioneers left
3852-531: The Northfield, Massachusetts , area. The ( Sokoki ) tribe migrated to Odanak, Quebec following the epidemics and the wars with the settlers but returned to Vermont. In 1614, Dutch explorer Adriaen Block became the first European to chart the Connecticut River, sailing as far north as Enfield Rapids . He called it the "Fresh River" and claimed it for the Netherlands as the northeastern border of
3959-761: The Nulhegan River basin in Essex County, Vermont , would be flushed into the main river by the release of water impounded behind splash dams . Several log drivers died trying to move logs through Perry Falls in Pittsburg. Teams of men would wait at Canaan, Vermont , to protect the bridges from log jams. Men guided logs through a 400-foot (120 m) drop along the length of Fifteen-Mile Falls (now submerged under Moore and Comerford reservoirs), and through Logan's Rips at Fitzdale, Mulligan's Lower Pitch, and Seven Islands. The White River from Vermont and Ammonoosuc River from New Hampshire brought more logs into
4066-714: The Passumpsic , Ammonoosuc , White , Black , West , Ashuelot , Millers , Deerfield , Chicopee , Westfield , and Farmington rivers. The Swift River , a tributary of the Chicopee, has been dammed and largely replaced by the Quabbin Reservoir which provides water to the Massachusetts Water Resources Authority district in eastern Massachusetts, including Boston and its metropolitan area . Along its southern reaches,
4173-732: The Plymouth Colony in 1632 and ultimately founded the village of Matianuck (which became Windsor, Connecticut ) several miles north of the Dutch fort. A group left the Massachusetts Bay Colony from Watertown , seeking a site where they could practice their religion more freely. With this in mind, they founded Wethersfield, Connecticut , in 1633, several miles south of the Dutch fort at Hartford. In 1635, Reverend Thomas Hooker led settlers from Cambridge, Massachusetts , where he had feuded with Reverend John Cotton , to
4280-525: The Six Flags New England amusement park. The Connecticut's largest falls – South Hadley Falls – features a vertical drop of 58 feet (18 m). Lush green forests and agricultural hamlets dot this middle portion of the Connecticut River; however, the region is best known for its numerous college towns , such as Northampton, South Hadley , and Amherst , as well as the river's most populous city, Springfield. The city sits atop bluffs beside
4387-602: The Society for the Protection of New Hampshire Forests , The Nature Conservancy of New Hampshire, and others to raise around $ 42 million. A conservation easement over 146,000 acres (590 km ) of the property prohibits development of the land while allowing public access. The forest is managed by the Lyme Timber Company, and the conservation easement over the land ensures sustainable forest management of
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4494-602: The Trust for Public Land purchased 171,000 acres (690 km ) of land in New Hampshire from International Paper , allowing the Connecticut Lakes Headwaters Partnership Task Force to plan the future protection of the land. The property spans the towns of Pittsburg , Clarksville , and Stewartstown, New Hampshire , nearly 3 percent of the land in the state of New Hampshire. The Trust for Public Land worked in partnership with
4601-778: The United States Fish and Wildlife Service has repopulated the river with another species of migratory fish, the Atlantic salmon , which for more than 200 years had been extinct from the river due to damming . Several fish ladders and fish elevators have been built to allow fish to resume their natural migration upriver each spring. Fresh and brackish water residents of the main branch and tributaries include common carp , white catfish , brown bullhead , fallfish , yellow perch , smallmouth bass , largemouth bass , northern pike , chain pickerel , bluegill , pumpkinseed sunfish , golden shiner , and rock bass . Much of
4708-620: The Western Niantics , while maintaining an uneasy stand-off with their rivals the Mohegans . The Mattabesset (Tunxis) tribe takes its name from the place where its sachems ruled at the Connecticut River's Big Bend at Middletown, in a village sandwiched between the territories of the aggressive Pequots to the south and the more peaceable Mohegans to the north. The Mohegans dominated the region due north, where Hartford and its suburbs sit, particularly after allying themselves with
4815-491: The issuance of land grants by New Hampshire Governor Benning Wentworth beginning in the 1740s. New York protested these grants, and King George III decided in 1764 that the border between the provinces should be the western bank of the Connecticut River. Ethan Allen, the Green Mountain Boys , and other residents of the disputed area resisted attempts by New York to exercise authority there, which resulted in
4922-821: The trap rock Metacomet Ridge which extends from Long Island Sound to the Massachusetts/ Vermont border. This ridge, rising hundreds of feet above the Connecticut River , Farmington River , and Quinnipiac River valleys, is a prominent landscape feature of central Connecticut. From south to north, the trail uses the ridges of the Hanging Hills , Short Mountain , Ragged Mountain , Bradley Mountain , Pinnacle Rock , Rattlesnake Mountain , Farmington Mountain , Talcott Mountain , Hatchet Hill , Peak Mountain , and West Suffield Mountain . Abrupt vertical cliffs with visible talus slopes and frequent viewpoints are common throughout. Views are generally to
5029-471: The 1860s it has been mainly a tourist attraction. In 1972 Old Newgate Prison was declared a National Historic Landmark . The Hanging Hills' Hubbard Park was financed by Walter Hubbard, local entrepreneur and president of the Bradley & Hubbard Manufacturing Company. Most of the land in the park was given to the town of Meriden by him, offered outright, with the stipulation that everything connected with
5136-568: The 1960s and slated for residential development, the tower became part of the Talcott Mountain State Park in 1965 through the efforts of conservation non-profit groups, the state of Connecticut, and the United States government. The tower has been renovated as a museum with period artifacts and furnishings. Visitors may climb to the top of the tower for a 360-degree view encompassing four states. Hill-Stead , now
5243-502: The 33,000-square-foot (3,100 m ) colonial-revival style Pope-Riddle House; an 18th-century farm house; a carriage garage with an arts and crafts theater; and a barn and additional farm buildings. The house is extensively furnished with paintings, prints, and art. Highlights include works by Édouard Manet , Claude Monet , James McNeill Whistler , Albrecht Dürer and postcards including correspondence from Mary Cassatt , Henry James , and James McNeill Whistler. Will Warren's Den,
5350-677: The Bay Path where the Connecticut River meets the western Westfield River and eastern Chicopee River . The Pocomtuc villagers at Agawam helped Puritan explorers settle this site and remained friendly with them for decades, unlike tribes farther north and south along the Connecticut River. The region stretching from Springfield north to the New Hampshire and Vermont state borders fostered many agricultural Pocomtuc and Nipmuc settlements, with its soil enhanced by sedimentary deposits. Occasionally, these villages endured invasions from more aggressive confederated tribes living in New York , such as
5457-420: The Black Dog the first time results in joy; a second sighting, misfortune. Seeing the Black Dog a third time would result in one's death. At least six deaths have been blamed on third meetings with the Black Dog. The trail is blazed with blue rectangles. It is regularly maintained, and is considered easy hiking, with sections of rugged and moderately difficult hiking. As the crow flies, the Metacomet Trail route
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#17327878573635564-740: The Colonists against the Pequots during the Pequot War of 1637. Their culture was similar to the Pequots, as they had split off from them and become their rivals some time prior to European exploration of the area. The agricultural Pocomtuc tribe lived in unfortified villages alongside the Connecticut River north of the Enfield Falls on the fertile stretch of hills and meadows surrounding Springfield, Massachusetts . The Pocomtuc village of Agawam eventually became Springfield, situated on
5671-499: The Connecticut Colony and New Netherland Colony to a point near Greenwich, Connecticut . The treaty allowed the Dutch to maintain their trading post at Fort Huys de Hoop, which they did until the 1664 British takeover of New Netherland. The Connecticut River Valley's central location, fertile soil, and abundant natural resources made it the target of centuries of border disputes, beginning with Springfield's defection from
5778-448: The Connecticut Colony in 1641, which brought the Massachusetts Bay Colony to the river. In 1640, Massachusetts Bay Colony asserted a claim to jurisdiction over lands surrounding the river; however, Springfield remained politically independent until tensions with the Connecticut Colony were exacerbated by a final confrontation later that year. Hartford kept a fort at the mouth of the Connecticut River at Old Saybrook for protection against
5885-702: The Connecticut River has carved a wide, fertile floodplain valley (known in Massachusetts as the Pioneer Valley), depositing rich silt and loam soils known internationally for their agricultural merit. Abundant riparian hardwood species include sycamores, cottonwood , basswood, willows, sassafras, box elder, black elder, osier dogwood and more. The river itself and its many tributaries are home to many typical New England freshwater species. These include dace , crawfish , hellgramites , freshwater mussels , typical frog species, snapping turtles , brook trout , freshwater sturgeon, catfish, walleye, chain pickerel and carp. Introduced species include stocked rainbow trout . The river
5992-435: The Connecticut River was designated one of only 14 American Heritage Rivers , which recognized its "distinctive natural, economic, agricultural, scenic, historic, cultural, and recreational qualities." In May 2012, the Connecticut River was designated America's first National Blueway in recognition of the restoration and preservation efforts on the river. The Connecticut River's flow is slowed by main stem dams, which create
6099-419: The Connecticut's confluence with two major tributaries, the Chicopee River to the east and Westfield River to the west. The region around the Connecticut River is known locally as the Pioneer Valley , and the name adorns many local civic organizations and local businesses. While the southern part of the valley in Massachusetts is heavily urbanized, the northern section is largely rural and the local agriculture
6206-546: The Connecticut. After the first major dam was built near Turners Falls, Massachusetts , thirteen additional dams have ended the Connecticut River's great anadromous fish runs. Salmon restoration efforts began in 1967, and fish ladders at a fish elevator at Hadley Falls have since enabled migrating fish to return to some of their former spawning grounds. In addition to dams, warm water discharges between 1978 and 1992 from Vermont Yankee Nuclear Power Plant in Vernon, Vermont released water up to 105 °F (41 °C) degrees, with
6313-489: The Connecticut. A log boom was built between Wells River, Vermont , and Woodsville, New Hampshire , to hold the logs briefly and release them gradually to avoid jams in the Ox Bow. Men detailed to this work utilized Woodsville's saloons and red-light district . Some of the logs were destined for mills in Wilder and Bellows Falls, Vermont , while others were sluiced over the Bellows Falls dam. North Walpole, New Hampshire , contained twelve to eighteen saloons, patronized by
6420-399: The Connecticut. This resulted in an unsuccessful lawsuit by the state of Connecticut against the diversion of its riparian waters. Demand for drinking water in eastern Massachusetts passed the sustainable supply from the existing system in 1969. Diverting water from the Connecticut River was considered several times, but in 1986 the Massachusetts Water Resources Authority instead undertook
6527-413: The Massachusetts Bay Colony. For decades, Springfield remained the Massachusetts Bay Colony's westernmost settlement, on the northern border of the Connecticut Colony. Of these settlements, Hartford and Springfield quickly emerged as powers. By 1654, however, the success of these English settlements rendered the Dutch position untenable on the Connecticut River. A treaty moved the boundary westward between
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#17327878573636634-522: The Metacomet Trail, most notably on Talcott Mountain , the Hanging Hills , and Ragged Mountain . The Metacomet Trail is primarily used for hiking , backpacking , picnicking , and in the winter, snowshoeing . Portions of the trail are suitable for, and are used for, mountain biking and cross-country skiing . Site-specific activities enjoyed along the route include hunting , fishing , horseback riding , boating , bouldering , rock climbing (access), and swimming . The Metacomet Trail traverses
6741-422: The Metacomet Trail. Over 700 miles (1,100 km) of "blue blaze trails" in Connecticut were completed by the association by the end of the 20th century. The name " Metacomet " was borrowed from the 17th century sachem of the Wampanoag Tribe of southern New England who led his people during King Philip's War . According to popular folklore, Metacomet, dubbed "King Phillip" by the English colonists, watched
6848-442: The Pequots, Wampanoags , Mohegans, and the New Netherland Colony. After Springfield broke ties with the Colony, the remaining Connecticut settlements demanded that Springfield's ships pay tolls when passing the mouth of the river. The ships refused to pay this tax without representation at Connecticut's fort, but Hartford refused to grant it. In response, the Massachusetts Bay Colony solidified its friendship with Springfield by levying
6955-533: The United States, flowing roughly southward for 406 miles (653 km) through four states. It rises 300 yards (270 m) south of the U.S. border with Quebec , Canada , and discharges at Long Island Sound . Its watershed encompasses 11,260 square miles (29,200 km ), covering parts of five U.S. states and one Canadian province, via 148 tributaries, 38 of which are major rivers. It produces 70% of Long Island Sound's fresh water, discharging at 18,400 cubic feet (520 m ) per second. The Connecticut River Valley
7062-528: The beginning of the river's course in the town of Pittsburg is occupied by the Connecticut Lakes, which contain lake trout and landlocked salmon . Landlocked salmon make their way into the river during spring spawning runs of bait fish and during their fall spawn. The river has fly-fishing-only regulations on 5 miles (8 km) of river. Most of the river from Lake Francis south is open to lure and bait as well. Two tail-water dams provide cold river water for miles downstream, making for bountiful summer fishing on
7169-452: The border of Massachusetts where it sits 190 feet (58 m) above sea level. The region along the river upstream and downstream from Lebanon, New Hampshire , and White River Junction, Vermont , is known as the "Upper Valley". The exact definition of the region varies, but it generally is considered to extend south to Windsor, Vermont , and Cornish, New Hampshire , and north to Bradford, Vermont , and Piermont, New Hampshire . In 2001,
7276-476: The burning of the village of Simsbury in 1676 from a cave on Talcott Mountain. The cave is now known as King Phillip's Cave , accessible via a side trail from the Metacomet Trail. Joseph Wadsworth is also said to have camped at the cave after saving the Charter of Connecticut from being repossessed by the King's emissary. Old Newgate Prison , located below Peak Mountain, was originally a copper mine , opened in 1705. After mining operations proved unprofitable,
7383-612: The college town of Northampton. Metacomet Trail The Metacomet Trail is a 62.7-mile (100.9 km) Blue-Blazed hiking trail that traverses the Metacomet Ridge of central Connecticut as part of the New England National Scenic Trail . Despite being easily accessible and close to large population centers, the trail is considered remarkably rugged and scenic. The route includes many areas of unique ecologic, historic, and geologic interest. Notable features include waterfalls, dramatic cliff faces, woodlands, swamps, lakes, river flood plain, farmland, significant historic sites, and
7490-399: The colony of Connecticut converted it to a prison and named it after Newgate Prison of London . The first prisoner, John Hinson, was committed for burglary in 1773. Later Tories and Loyalists were held there during the Revolutionary War . In 1790 it became a state prison, the first such in the United States. After the prison closed in 1827 mining operations resumed for a time, but since
7597-406: The current 475 foot (139 m) tower. WAQY , WHTX-LD , and WDMR-LD also maintain transmitters there. WUCS used to operate from this site as WPKX, prior to moving to Hartford in 2012. It is also home to numerous cellular, paging, and two-way radio users. Provin Mountain, like much of the Metacomet Ridge, is composed of basalt , also called traprock, a volcanic rock. The mountain formed near
7704-617: The dam's powerhouse from being overwhelmed, despite blocks of ice breaking through the upstream walls. In Northampton, Massachusetts , looting during the flood became a problem, causing the mayor of the city to deputize citizen patrols to protect flooded areas. Over 3,000 refugees from the area were housed in Amherst College and the Massachusetts State Agricultural College (now UMass Amherst ). Unprecedented accumulated ice jams compounded
7811-715: The early 1600s to name the river, which was also called simply "The Great River". It was also known as the Fresh River, and the Dutch called it the Verse River. Early spellings of the name by European explorers included "Cannitticutt" in French or in English. Archaeological digs reveal human habitation of the Connecticut River Valley for 6,000 years before present. Numerous tribes lived throughout
7918-496: The ecological sensitivity of the area. Other ecosystems on the southern sections of the Metacomet Trail include the northern riverine community which supports species such as willow , American elm , and sycamore ; this ecosystem can be found along the Westfield and Connecticut Rivers. In the late 19th century, interests in mountains as places to build recreational footpaths took root in New England with organizations such as
8025-544: The end of the French and Indian War in 1763. The Abenaki had resisted British colonial settlement for decades, but colonists began settling north of Brattleboro, Vermont , following the war. Settlement of the Upper Connecticut River Valley increased quickly, with population assessments of 36,000 by 1790. Vermont was claimed by both New Hampshire and New York , and was settled primarily through
8132-554: The end of the Triassic Period with the rifting apart of the North American continent from Africa and Eurasia . Lava welled up from the rift and solidified into sheets of strata hundreds of feet thick. Subsequent faulting and earthquake activity tilted the strata, creating the cliffs and ridgeline of Provin Mountain. Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce
8239-488: The eruptions deposited deep layers of sediment between the lava flows, which eventually lithified into sedimentary rock . The resulting "layer cake" of basalt and sedimentary sheets eventually faulted and tilted upward. Subsequent erosion wore away the weaker sedimentary layers a faster rate than the basalt layers, leaving the abruptly tilted edges of the basalt sheets exposed, creating the distinct linear ridge and dramatic cliff faces visible today. The best way to imagine this
8346-463: The establishment of the independent Vermont Republic in 1777 and its eventual accession to the United States in 1791 as the fourteenth state. Boundary disputes between Vermont and New Hampshire lasted for nearly 150 years and were finally settled in 1933, when the U.S. Supreme Court reaffirmed King George's boundary as the ordinary low-water mark on the Vermont shore. In some places, the state line
8453-576: The fertile Connecticut River valley prior to Dutch exploration beginning in 1614. Information concerning how these tribes lived and interacted stems mostly from English accounts written during the 1630s. The Pequots dominated a territory in the southern region of the Connecticut River valley, stretching roughly from the river's mouth at Old Saybrook, Connecticut , north to just below the Big Bend at Middletown, Connecticut . They warred with and attempted to subjugate neighboring agricultural tribes such as
8560-463: The holding and releasing of water between the river's 54 largest dams. The Cabot and Turners Falls hydroelectric stations generate up to 68 MW. The Holyoke Canal System and Hadley Falls Station at Holyoke Dam are rated a combined 48 MW. The Connecticut River watershed encompasses 11,260 square miles (29,200 km ), connecting 148 tributaries, including 38 major rivers and numerous lakes and ponds. Major tributaries include (from north to south)
8667-409: The log drivers. Mount Tom was the landmark the log drivers used to gauge the distance to the final mills near Holyoke, Massachusetts . These spring drives were stopped after 1915, when pleasure boat owners complained about the hazards to navigation. The final drive included 500 workers controlling 65 million feet of logs. A final pulp drive consisted of 100,000 cords of four-foot logs in 1918. This
8774-623: The mountain drains into the Connecticut River, thence to Long Island Sound; the rest of the mountain drains into the Westfield River, thence to the Connecticut River. The mountain hosts several underground reservoirs which augment the water supply of municipal Springfield. Located at the summit of Provin Mountain is where the original studios and current transmitters for WWLP exist. WWLP first signed on from this location in March 1953. WWLP's studios remained there until 2000 when they were moved to Chicopee . The transmitter has remained there, as well as
8881-530: The northeast, over 430,000 people were made homeless or destitute by flooding that year. The Connecticut River Flood Control Compact between the states of Connecticut, Massachusetts, New Hampshire, and Vermont was established in 1953 to help prevent serious flooding. The creation of the Quabbin Reservoir in the 1930s diverted the Swift River , which feeds the Chicopee River, a tributary of
8988-517: The park was to remain free of charge for the people of Meriden, and that no concessions for profit would ever allowed within the park. Hubbard elicited the assistance of notable landscape architect Fredrick Law Olmsted in drawing up the design. Finished in 1900, it comprises approximately 1,800 acres (7.3 km ) of carefully kept woodlands, streams, dramatic cliff faces, flower gardens, and the James Barry bandshell and picnic spots. Castle Craig ,
9095-452: The police to issue a "shoot on sight" edict; 800 National Guard troops were brought in to help maintain order. Rescue efforts using a flotilla of boats saved people trapped in upper stories of buildings, bringing them to local fraternal lodges, schools, churches and monasteries for lodging, medical care, and food. The American Red Cross and local, state and federal agencies, including the WPA and
9202-481: The presence of large, shifting sandbars at its mouth, the Connecticut is the only major river in the Northeastern United States without a port at its mouth. The Connecticut River carries a heavy amount of silt from as far north as Quebec, especially during the spring snow melt. This results in a large sandbar near the river's mouth which is a formidable obstacle to navigation. The Connecticut
9309-609: The problems created by the flood, diverting water into unusual channels and damming the river, raising water levels even further. When the jam at Hadley, Massachusetts , gave way, the water crest overflowed the dam at Holyoke , overwhelming the sandbagging there. The village of South Hadley Falls was essentially destroyed, and the southern parts of Holyoke were severely damaged, with 500 refugees. In Springfield, Massachusetts, 5 sq mi (13 km ), and 18 miles (29 km) of streets, were flooded, and 20,000 people lost their homes. The city lost power, and nighttime looting caused
9416-628: The property. Following the most recent ice age , the Middle Connecticut River Valley sat at the bottom of Lake Hitchcock . Its lush greenery and rich, almost rockless soil comes from the ancient lake's sedimentary deposits. In the Middle Connecticut region, the river reaches its maximum depth – 130 feet (40 m) – at Gill, Massachusetts , around the French King Bridge , and its maximum width – 2,100 feet (640 m) – at Longmeadow , directly across from
9523-520: The river's first unnavigable waterfall. Pynchon surmised that traders using any of these routes would have to dock and change ships at his site, thereby granting the settlement a commercial advantage. It was initially named Agawam Plantation and was allied with the settlements to the south that became the state of Connecticut. In 1641, Springfield splintered off from the Hartford-based Connecticut Colony, allying itself with
9630-498: The route is typical of Connecticut . Conditions on exposed ridge tops and summits may be harsher during cold or stormy weather. Lightning is a hazard on exposed summits and ledges during thunderstorms. Snow is common in the winter and may necessitate the use of snowshoes. Ice can form on exposed ledges and summits, making hiking dangerous without special equipment. Biting insects can be bothersome during warm weather. Parasitic deer ticks (which are known to carry Lyme disease ) are
9737-510: The rural countryside to the west and the urban landscape of metropolitan Springfield, Massachusetts to the east. Threats to Provin Mountain and its unique habitats include suburban sprawl and quarrying . Although the northern edge of the mountain lies within Robinson State Park , much of the mountain is located on private land. Other landholders include local municipalities and conservation commissions. In 2000, Provin Mountain
9844-637: The second-largest city and the only state capital on the river, is at the southern end of this region on an ancient floodplain that stretches to Middletown. 15 miles (24 km) south of Hartford, at Middletown, the Lower Connecticut River section begins with a narrowing of the river, and then a sharp turn southeast. Throughout southern Connecticut, the Connecticut passes through a thinly populated, hilly, wooded region before again widening and discharging into Long Island Sound between Old Saybrook and Old Lyme in flat coastal marshlands. Due to
9951-499: The shad population has increased. The mouth of the river up to Essex is thought to be one of the busiest stretches of waterway in Connecticut. Some local police departments and the state Environmental Conservation Police patrol the area a few times a week. Some towns keep boats available if needed. In Massachusetts, the most active stretch of the Connecticut River is centered on the Oxbow , 14 miles (23 km) north of Springfield in
10058-534: The site in Connecticut of the Dutch Fort House of Hope, where he founded Newtowne. Shortly after Hooker's arrival, Newtowne annexed Matianuck based on laws articulated in Connecticut's settlement charter, the Warwick Patent of 1631. The patent, however, had been physically lost, and the annexation was almost certainly illegal. The fourth English settlement along the Connecticut River came out of
10165-438: The spine of the Metacomet Trail was formed 200 million years ago during the late Triassic and early Jurassic periods, and is composed of trap rock, also known as basalt , an extrusive volcanic rock . Basalt is a dark colored rock, but the iron within it weathers to a rusty brown when exposed to the air, lending the ledges a distinct reddish appearance. Basalt frequently breaks into octagonal and pentagonal columns, creating
10272-527: The summits of Talcott Mountain and the Hanging Hills . The Metacomet Trail is maintained largely through the efforts of the Connecticut Forest and Park Association . On March 30, 2009, President Barack Obama signed the Omnibus Public Land Management Act of 2009 establishing the New England National Scenic Trail (and two other national scenic trails). The combination of the Metacomet, Monadnock and Mattabesett trails
10379-493: The surrounding region. The high volume and numerous falls of the river led to the rise of industry along its banks during the Industrial Revolution . The cities of Springfield and Hartford in particular became centers of innovation and "intense and concentrated prosperity." The Enfield Falls Canal was opened in 1829 to circumvent shallows around Enfield Falls, and the locks built for this canal gave their name to
10486-457: The thermal plume reaching 55 miles (89 km) downstream as far as Holyoke. This thermal pollution appears to be associated with an 80% decline in American shad fish numbers from 1992 to 2005 at Holyoke Dam. This decline may have been exacerbated by over-fishing in the mid-Atlantic and predation from resurging striped bass populations. The nuclear plant was closed at the end of 2014, after which
10593-436: The town of Windsor Locks, Connecticut . The Connecticut River Valley functioned as America's hub of technical innovation into the 20th century, particularly the cities of Springfield and Hartford, and thus attracted numerous railroad lines. The proliferation of the railroads in Springfield and Hartford greatly decreased the economic importance of the Connecticut River. From the late 1800s until today, it has functioned largely as
10700-400: The trail is located just east of the Hanging Hills on U.S. Route 5 , 4 miles (6 km) north of the city of Meriden , in the town of Berlin, Connecticut ; the northern terminus is located in the hamlet of Rising Corner, part of Suffield, Connecticut , 7 miles (11 km) southwest of Springfield, Massachusetts . The 110-mile (180 km) Metacomet-Monadnock Trail in Massachusetts and
10807-597: The trail, its ecosystems, and its viewshed included quarrying and suburban sprawl . The footway of the Metacomet Trail is maintained by volunteer efforts largely facilitated by the Connecticut Forest and Park Association . Many groups are invested in preserving the landscape and ecosystem of the Metacomet Trail, including the Connecticut Department of Environmental Protection, the Metropolitan District of Connecticut (responsible for
10914-429: The watershed (Connecticut and Massachusetts) than in the northern part (Vermont and New Hampshire), largely due to differences in stream gradient and substrate. Eight of the 12 species in the watershed are listed as endangered, threatened, or of special concern in one or more of the states in the watershed. A number of colonial animal species make their home in the waters of the Connecticut. Deeper areas are habitat for
11021-675: The watershed properties on Talcott Mountain), Suffield Land Conservancy, East Granby Land Trust, Farmington Land Trust, Meriden Land Trust, Berlin Land Trust, Simsbury Land Trust, Ragged Mountain Foundation, and the Avon Land Trust. In 2000, the Metacomet Trail was included in a study by the National Park Service for possible inclusion in a new National Scenic Trail , which was officially recognized in 2009 as
11128-577: The west from West Suffield Mountain south through Ragged Mountain; with views in all directions at varying points in the Hanging Hills. The Farmington River cuts through the ridgeline between Hatchet Hill and Talcott Mountain in the Tariffville Gorge (east of Simsbury ). Historic features along the trail include Old Newgate Prison museum and copper mine in East Granby; Heublein Tower on Talcott Mountain with expansive view of four states;
11235-617: Was an early attempt to protect the ridges from sprawl. It received the Connecticut Governor's Green Circle Award yet was ignored by authorities in Southington, Berlin, New Britain, and Meriden. Since then, sprawl has eroded the ecological integrity of the trail corridor, particularly in Southington. That said, Southington has acquired the Crescent Lake compartment, yet now has plans to log it (2014) without regard for
11342-605: Was included in a study by the National Park Service for the designation of a new National Scenic Trail now tentatively called the New England National Scenic Trail , which would include the Metacomet-Monadnock Trail in Massachusetts and the Mattabesett and Metacomet trails in Connecticut. Connecticut River The Connecticut River is the longest river in the New England region of
11449-490: Was to take advantage of the wartime demand. In March 1936, due to a winter with heavy snowfall, an early spring thaw and torrential rains, the Connecticut River flooded, overflowing its banks, destroying numerous bridges and isolating hundreds of people who had to be rescued by boat. The dam at Vernon, Vermont , was topped by 19 feet (5.8 m). Sandbagging by the National Guard and local volunteers helped prevent
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