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bottom (syncline) of one of these folds, but over time cracks in the Pottsville Conglomerate in the
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higher elevations allowed it to erode quickly, and the softer layers of shale and limestone were
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quick to follow. This left Spruce Knob as the highest point in the landscape. Spruce Knob (Spruce
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Mountain) is the westernmost extent of this intense folding and faulting. To the west, the
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Allegheny Plateau is composed of more gently sloping hills and dendritic drainages.
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Climate
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Spruce Knob's climate can be classified as cold continental or highland. Summers are cool and
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often damp, with thunderstorms common both in spring and summer. Winters are cold and snowy, with
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an average of around of annual snowfall leaving the summit access road often impassible between
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October and April. Blizzard conditions can develop in minutes behind cold frontal passages and last
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days with upslope snowfall continuing with northwest winds, making travel on the mountain dangerous
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during the colder months. This mountain can receive high winds year-round; red spruce deformed by
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constant exposure to strong westerly winds are scattered across its rocky ridges.
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Ecology
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Flora
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As with almost the entirety of the MNF, most of the original Spruce Mountain upland forest was
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completely denuded by logging around the turn of the 20th century and now consists of second- or
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third-growth forest. (The only documented exception to this on the Mountain is the North Spruce
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Mountain Old Growth Site.
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) The present second-growth forest of Spruce Mountain is characterized by a dominance of sugar
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maple (Acer saccharum), American beech (Fagus grandifolia), and yellow birch (Betula lutea). Other
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characteristic species of the mixed mesophytic forest region are also present: tuliptree
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(Liriodendron tulipifera), basswood (Tilia heterophylla, T.floridana, T. neglecta), chestnut
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(Castanea dentata), yellow buckeye (Aesculus flava), red oak (Quercus borealis), white oak (Q.
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alba), and eastern hemlock (Tsuga canadensis). The upper reaches of Spruce Mountain also include
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areas termed northern hardwood and northern evergreen forest types. The former is typified by red
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oak, white ash (Fraxinus americana), basswood (Tilia spp.), red maple (Acer rubrum), and cherry
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(Prunus spp.). The latter is dominated by the Mountain's eponymous red spruce (Picea rubens). While
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not extending above the timberline, the stunted tree growth high on this windy mountaintop is
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relatively open.
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The summit was named for the spruce trees which grow there. Red spruce (Picea rubens) is the most
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common tree species on the summit. The lower altitudes are populated by oak, hickory, birch, beech
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and maple
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Fauna
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Bald eagles, hawks and peregrine falcons have been seen on the mountain. Mammals such as black
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bear, white-tailed deer, weasel, porcupine, skunk and rabbit are also found. The important presence
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of ruffed grouse (Bonasa umbellus) on the Mountain has been acknowledged by the establishment of
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the Spruce Mountain Grouse Management Area by the MNF
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Recreation
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Spruce Knob is within the Spruce Knob-Seneca Rocks National Recreation Area, which in turn is part
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of Monongahela National Forest. Established in 1965, it was the first National Recreation Area
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designated by the U.S. Forest Service and includes more than .
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There are over of hiking trails around the mountain and a small lake well stocked with trout on
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the west side of the mountain. Two campgrounds are also on the mountain.
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Hiking trails — Huckleberry Trail, Lumberjack Trail, Spruce Mountain Trail — extend the length of
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the ridge. There are over 75 miles (121 km) of trails around the Mountain and a small 25 acre (10
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ha) lake well stocked with trout on the west side. There are also two campgrounds on the Mountain;
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the larger (43 sites) is nearest the lake.
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Access
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Paved access is from U.S. Route 33/West Virginia Route 28 about south of Riverton. Briery Gap
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Road (County Route 33/4), Forest Road 112 and Forest Road 104 have been reconstructed and paved to
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provide a hard-surfaced road to the summit.
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Forest Roads 104 and 112 are not maintained in the winter. Impassable conditions can be expected
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any time from mid-October to mid-April.
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See also List of mountains of the Alleghenies List of mountain peaks of North America
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List of mountain peaks of the United States List of mountains of West Virginia
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List of U.S. states by elevation
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References Citations
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Other sources
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Core, Earl L. (1928), "Ecological Studies on Spruce Mountain", Proc. W.Va. Acad. Sci. 2:36-39.
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Core, Earl L. (1929), "The Plant Ecology of Spruce Mountain, West Virginia", Ecology, 10:1-13.
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Robison, William C. (1960), “Spruce Knob Revisited: A Half-Century of Vegetation Change”, Castanea,
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Vol. 25, No. 1 (March issue), pp 53–61.
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External links
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Spruce Mountain page at Peakbagger.com Spruce Knob-Seneca Rocks National Recreation Area
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Monongahela National Forest: Spruce Knob
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Ridges of West Virginia Landforms of Pendleton County, West Virginia Allegheny Mountains
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Monongahela National Forest Protected areas of Pendleton County, West Virginia
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Saugus is a town in Essex County, Massachusetts, United States, in the Greater Boston area. The
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population was 28,619 at the 2020 census. Saugus is known as the site of the first integrated iron
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works in North America.
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History
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Native Americans inhabited the area around Saugus for thousands of years prior to the arrival of
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European settlers in the 1620s. At the time of European arrival, the Naumkeag, also known as
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Pawtucket, under the leadership of Montowampate were based near present day Saugus and controlled
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land extending from what is now Boston to the Merrimack River. English settlers took the name Sagus
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or Saugus from the Pawtucket word for "outlet," and used the term to refer to the Saugus River and
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the region that includes the present day cities and towns of Swampscott, Nahant, Lynn, Lynnfield,
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Reading, North Reading and Wakefield) which were later renamed Lin or Lynn in 1637, after King's
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Lynn in Norfolk, England.
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In 1646, the Saugus Iron Works, then called Hammersmith, began operations. It was the first
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integrated iron works in North America as well as one of the most technologically advanced in the
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world. The Iron Works produced over one ton of iron a day, but was not financially successful. It
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closed around 1670.
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In September 1687, Major Samuel Appleton was said to have given a speech from a rocky cliff near
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the Iron Works denouncing the tyranny of Colonial Governor Sir Edmund Andros. The place where he is
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said to have delivered the speech became known as Appleton's Pulpit.
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Nearly 100 men from Saugus fought in the American Revolutionary War. Saugus' preacher, Parson
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Joseph Roby, worked to strengthen the spirit of independence in Saugus and was instrumental in
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seeing that Saugus sent a large contingent to fight in the war.
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The nineteenth century ice industry began in Saugus when in 1804 Frederic Tudor cut ice from a pond
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on the family farm and shipped it to Martinique.
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In 1805 the Newburyport Turnpike (now U.S. 1) was built. About four miles of this road was built in
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Saugus. At first the turnpike was considered a mistake, as it was built over hills and swamps and
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grass soon grew over the road bed. From 1840 to 1846, the tolls were discontinued and it became a
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public highway. The invention of the automobile resulted in an increase of traffic on the Turnpike.
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In 1933 the road was widened and an overpass was added to separate the traffic on Route 1 and Main
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Street. In the 1950s new businesses began moving to Route 1. Today the businesses along Route 1
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generate millions in dollars for Saugus.
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The Lynn territory was shortened beginning in 1814 with the incorporation of Lynnfield. On February