Mount Everett | |
---|---|
Highest point | |
Elevation | 2,602 ft (793 m) |
Prominence | 1,663 ft (507 m) |
Parent peak | 42° 06' 07"N, 73° 25' 57"W |
Coordinates | 42°06′07″N73°25′57″W / 42.10194°N 73.43250°W |
Geography | |
Location | Southwest Berkshire County, Massachusetts |
Parent range | Taconic Mountains |
Geology | |
Rock age | Ordovician |
Mountain type(s) | Thrust fault; metamorphic rock |
Climbing | |
Easiest route | Mount Everett Road and Appalachian Trail |
Mount Everett is the highest peak in the southern Taconic Mountains, rising about 2,000 feet above its eastern footings in Sheffield, Mass. Its summit area is notable for expansive vistas and an unusual dwarf forest of pitch pine and oak. The Appalachian Trail traverses Mount Everett, which prior to the 20th century was called "Dome of the Taconics." Reaching 2,602 feet (793 meters) above sea level, Everett dominates much local scenery of the Housatonic Valley.
Mount Everett helps divide the watersheds of the Hudson and Housatonic rivers. Its eastern slopes share a larger escarpment with Mount Race and Bear Mountain plus several related summits. This escarpment rises from an elevation around 700 feet in Sheffield's Housatonic Valley at a mean angle of about 20 degrees (a 36% grade), although its higher reaches are markedly steeper. Everett's more gentle, western slopes begin in a valley occupied by the township of Mount Washington, where elevations average about 1,700 feet. [1]
A seasonal auto road approaching from the west climbs past Guilder Pond and continues nearly to Everett's summit, but its upper reaches have been long closed to automobiles. The summit area features an open forest of stunted pitch pine and scrub oak. [2] [3] A 40-foot fire tower was on the summit from 1970 until 2003 named "Mt. Washington Fire Tower" after the local township. Earlier towers stood there beginning in 1915. [4] About halfway down the eastern slopes are Race Brook Falls with a source near the gap between Mount Everett and Mount Race.
Much of the mountain is land administered by Mount Washington State Forest and the contiguous Mount Everett State Reservation, [5] which had about 10,000 visitors annually as of a 2005 official estimate. [6] Significant other portions of Everett's slopes are privately held. [7]
Mount Everett is part of the much larger Taconic Allochthon, a rock structure that migrated from about 25 miles to the east and arriving at its present location via low-angle thrust faulting. [8] [9] More narrowly, rocks of the upper mountain are within the "Everett Formation," a term first used by geologist E-An Zen in mapping and studying the allochthon during the 1960s. Zen modified the term "Everett Schist" (coined in 1893 by William Herbert Hobbs) "in order to include rocks of different metamorphic grades." [10] The formation extends intermittently throughout the highlands of the southern Taconics, with metamorphic grades increasing to the west. [11] Everett Formation rocks are principally olive-gray to green, blue-quartz pebble metagraywacke and quartzite of Ordovician and older age. [12] [13] [14] Everett's lower slopes are part of the Stockbridge Formation, which is generally limestone. [15]
In 1777 the peak was labeled "Tacan Mountain" on a map by Claude J. Sauthier [16] Separately, the once-famed Yale College President Timothy Dwight IV wrote of his 1781 ascent of "Taughanuk Mountain" in a travel memoir (posthumously published, 1823). [17] [18] Henry David Thoreau visited mountain's western slopes briefly in 1844 and referred to it as "Bald Mountain." [19]
Despite this history, the name "Mount Everett" was proposed in 1841 by Edward Hitchcock in his role as chief of the state Geological Survey, after Edward Everett, governor of Massachusetts (1836-1840). [20] Hitchcock didn't reference "Taconic Mountain" or any variant in his proposal; [21] he wrote merely that the mountain was "often confounded" with the local town of Mount Washington, Mass., where Hitchcock said it was known as Bald Mountain or Ball Mountain, "but in neighboring towns, I believe this name is rarely given." Hitchcock later became president of Amherst College.
By the late 19th century, "there [had] long been a protest against adopting the name that Prof. Hitchcock gave to the summit," according to Clark W. Bryan's 1886 tourist guide titled Book of the Berkshires. Bryan, with offices in Great Barrington, asserted that "the united public sentiment of the region" favored "Dome of the Taconics." [22]
Yet in 1897, the United States Board on Geographic Names which determines federal usage, accepted "Mount Everett," citing published sources. It listed a half-dozen alternate names as of 1897: Bald Dome, Bald Peak, Dome Peak, Mount Washington, Takonnack Mountain and Taughanuk Mountain. [23]
Bryan, a prolific poet, daily newspaper publisher and founder of Good Housekeeping magazine, died by suicide in 1899. [24] Books concerning the region published subsequently in 1899, 1907 and 1939 continued to reference "Dome of the Taconics," but also preferred the official term "Mount Everett." [25] [26] [27]
A 1987 USGS map (republished until 1997) labeled the entire mountain "Mount Everett" and its immediate summit area "Bald Peak." [28] Earlier and later USGS maps for the area don't reference "Bald Peak" on Mount Everett. [29] A wholly separate "Bald Peak" at 588 meters' elevation is also labeled on USGS maps a few miles to the southwest of Everett.
Henry David Thoreau visited Guilder Pond and "likely" the top of Everett in 1844, according to regional historian Bernard A. Drew. Thoreau was with his companion William Ellery Channing II (1817-1901) during their stay of several days to the region around Bash Bish Falls. Both Thoreau and Channing had read florid descriptions of the falls in Edward Hitchcock's geological survey of Massachusetts (1841). Channing confirmed this itinerary in an annotation of his copy of A Week on the Concord and Merrimack Rivers, "Thoreau also mentioned passing a 'silent gray tarn … high up the side of a mountain, Bald Mountain' — Guilder Pond, no doubt," Drew has offered. [30]
Mount Greylock is the highest point in Massachusetts at 3,489 feet. Located in the northwest region of the state, it is part of the Taconic Mountains, a geologically distinct range from the nearby Berkshires and Green Mountains. Expansive views and a small area of sub-alpine forest characterize its upper reaches. A seasonal automobile road crosses the summit area near three structures from the 1930s; these together constitute a small National Historic District. Various hiking paths including the Appalachian Trail traverse the area, which is part of the larger Mount Greylock State Reservation.
The Berkshires are highlands located in western Massachusetts and northwestern Connecticut in the United States. Generally, "Berkshires" may refer to the range of hills in Massachusetts that lie between the Housatonic and Connecticut Rivers. Highlands of northwest Connecticut may be seen as part of the Berkshires and sometimes called the Northwest Hills or Litchfield Hills. The segment of the Taconic Mountains in Massachusetts is often considered a part of the Berkshires, although they are geologically separate and are a comparatively narrow range along New York's eastern border.
Bear Mountain is a peak of the southern Taconic Mountains in Salisbury, Connecticut. At 2,316 feet (706 m), Bear Mountain is the highest mountain that lies wholly within Connecticut. However, it is not the state highpoint: in the 1940s, the United States Geological Survey determined that the highest elevation in the state, at 2,380 feet (725 m), was actually on the nearby Connecticut-Massachusetts border, on the southern slope of Massachusetts’ Mount Frissell. There is a stone monument on the Bear Mountain summit. The Appalachian Trail crosses the mountain in a generally north-south direction.
The Taconic Mountains are a 150-mile-long sub-range of the Appalachian Mountains lying on the eastern border of New York State and adjacent New England. The range, which played a role in the history of geological science, is separated from the Berkshires and Green Mountains to the east by a series of valleys, principally those of the Housatonic River, Battenkill River and Otter Creek. The Taconics' highest point is Mount Equinox in Vermont at 3,840 feet (1,170 m); among many other summits are Dorset Mountain, Mount Greylock and Mount Everett.
Mount Frissell, 2,454 feet (748 m), which straddles the border of southwest Massachusetts and northwest Connecticut, is part of the Taconic Range. Frissell's south slopes include the highest point in Connecticut, a popular destination for highpointers.
Bash Bish Falls, a waterfall in Bash Bish Falls State Park in the Taconic Mountains of southwestern Massachusetts, is the highest waterfall in the state. The falls are made up of a series of cascades, nearly 200 feet (61 m) in total. The final cascade is split into twin falls by a jutting rock, dropping in a 59-foot (18 m) "V" over boulders to a serene pool below.
The Appalachian National Scenic Trail spans 14 U.S. states over its roughly 2,200 miles (3,500 km): Georgia, North Carolina, Tennessee, Virginia, West Virginia, Maryland, Pennsylvania, New Jersey, New York, Connecticut, Massachusetts, Vermont, New Hampshire, and Maine. The southern end is at Springer Mountain, Georgia, and it follows the ridgeline of the Appalachian Mountains, crossing many of its highest peaks and running almost continuously through wilderness before reaching the northern end at Mount Katahdin, Maine.
Gridley Mountain, 2,211 feet (674 m), is the third highest elevation in the state of Connecticut. The mountain, part of the Taconic Range, has no official trail and is located on private property. The Mount Washington Road passes the mountain from the west.
The South Taconic Trail is a 21.3 mi (34.3 km) hiking trail in the Taconic Mountains of southwest Massachusetts and adjacent New York. The trail extends from Shagroy Road in Millerton, New York, north along the ridgecrest of the southern Taconic Range and the border of New York and Massachusetts, and ends north of the Catamount Ski Area on Massachusetts Route 23 700 feet (210 m) east of the New York border in Egremont, Massachusetts. The Appalachian Trail, which traverses an adjacent ridgeline in the same mountain range, parallels the South Taconic Trail 3 mi (4.8 km) to the east. The trails are connected to one another via shorter trails.
Berlin Mountain is a 2,818-foot-tall (859 m) prominent peak in the Taconic Mountains of western New England and is located adjacent to Massachusetts's border with New York State. It is the highest point in Rensselaer County. The summit and west side of the mountain are located in New York; the east side lies within Williamstown, Massachusetts. The mountain is a bald, notable for its grassy summit and expansive views of the Hudson River Valley to the west. The 37-mile (60 km) Taconic Crest Trail traverses the mountain. Several other hiking trails approach the summit from the east. Much of the upper slopes and summit are within protected conservation land. Historically the lower slopes of the mountain were farmed heavily throughout the 19th Century. In addition to agriculture, there are several remnants of charcoal kilns located on the mountain that produced fuel for iron smelting.
Brodie Mountain, 2,621 feet (799 m), is a prominent 5.5-mile (8.9 km) long ridgeline in the Taconic Mountains of western Massachusetts, known for the former Brodie Mountain ski area, which closed in 2002. The ridge has eight well defined summits, three of which have names: Sheep's Heaven Mountain, 2,530 feet (770 m), the ridge's southern prominatory; Beoadic Mountain, the ridge high point, just north of Sheep's Heaven; and East Mountain, 2,613 feet (796 m) located at the top of the former ski area at the center of the ridge. A northern summit, 2,170 feet (660 m), is shown as "Brodie Mountain" on maps that predate the Brodie Mountain ski area.
Brace Mountain is the peak of a ridge in the southern Taconic Mountains, near the tripoint of the U.S. states of New York, Connecticut and Massachusetts. Its 2,311-foot (704 m) main summit is located in New York; it is the highest point in that state's Dutchess County.
Alander Mountain is a 2,241-foot-tall (683 m) part of the south Taconic Mountains in southwest Massachusetts and adjacent to New York. The summit is grassy and covered with scrub oak and shrubs; the sides of the mountain are heavily forested. Several trails traverse Alander Mountain, most notably is the 15.7 mi (25.3 km) South Taconic Trail, which passes just beneath the summit.
Mount Fray, 1,893 feet (577 m), also known as Catamount because of the Catamount Ski Area located on its north slope, is a prominent peak of the south Taconic Mountains, located in southwest Massachusetts and adjacent New York. The summit is open and covered in scrub oak; it offers views west over the Hudson River Valley. The sides of the mountain are wooded with northern hardwood tree species. The 15.7 mi (25.3 km) South Taconic Trail passes over the summit of Mount Fray.
Mount Race, 2,365 feet (721 m), is a mountain in Berkshire County, Massachusetts. It shares many characteristics with the slightly higher Mount Everett about a mile to the north. Part of the Taconic Mountains, Race is known for its waterfalls, an eastern escarpment of nearly 2,000 feet, and expansive views. The Appalachian Trail crosses its summit, which has an open forest of dwarf pitch pine and scrub oak.
Round Mountain, 2,296 feet (700 m), located on the border of southwest Massachusetts and northwest Connecticut, is a prominent peak of the Taconic Range. The peak and southern slopes of the mountain are within Connecticut; the northern slope lies within Massachusetts.
Holy Mount, 1,968 feet (600 m), is a prominent peak in the Taconic Mountains of western Massachusetts, formerly used as the location of religious ceremonies by a nearby Shaker community.
Located in Berkshire County, Saddle Ball Mountain is the 2nd highest peak in the Commonwealth of Massachusetts.
Monument Mountain is the name of a popular 503-acre (204 ha) open space reservation located in Great Barrington, Massachusetts on the southeast side of Monument Mountain. The reservation is centered on the 1,642 feet (500 m) subordinate summit of Peeskawso Peak. It is managed by The Trustees of Reservations, a non-profit conservation organization and is notable for its expansive views of the Housatonic River Valley, the Berkshires, the Taconic Mountains, and the Catskill Mountains of New York from the knife-edge summit of Peeskawso Peak. Monument Mountain, composed of erosion resistant quartzite, is of The Berkshires geology. The reservation receives more than 20,000 visitors a year. The mountain was logged for charcoal to fuel a furnace in Vandusenville at the corner of Division Street and Route 41 in Great Barrington. Remnants of the furnace can be seen if one stands on the Route 41 bridge and looks upstream on the Williams River.
Monument Mountain is a 2.5-mile (4.0 km) long quartzite ridgeline located in Great Barrington and Stockbridge, Massachusetts in the Berkshires geology. Beside the high point, 1,739 feet (530 m), the mountain has several distinct features, most notably the open, knife-edge Peeskawso Peak, 1,642 feet (500 m) located on the southeast side of the mountain within the 503-acre (204 ha) Monument Mountain reservation managed by The Trustees of Reservations. The mountain receives over 20,000 visitors per year.
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