Camel's Hump, July 2012
|Elevation||4,083 ft (1,244 m) NAVD 88|
|Prominence||1,860 ft (570 m) |
|Listing||New England 4,000-footers|
New England Fifty Finest #46
|Location||Huntington / Duxbury, Vermont, U.S.|
|Parent range||Green Mountains|
|Age of rock||550 million years|
|Easiest route||Hiking trail|
Camel's Hump (alternatively Camels Hump) is a mountain in the Green Mountains in the U.S. state of Vermont. It is Vermont's third-highest mountain and, at 4,085 feet (1,245 m), it is the highest mountain in Camel's Hump State Park. Because of its distinctive profile, it is perhaps the state's most recognized mountain, featured on the state quarter. With its neighbor to the north, Mount Mansfield, it borders the Winooski River, which has carved through the Green Mountains over eons.
Since Europeans first saw the mountain, probably on Samuel de Champlain's 1609 trip down Lake Champlain to the west, the mountain has had a number of names related to its distinctive shape. De Champlain named the mountain "Le Lion Couchant", a heraldic image which roughly translates as "The Resting Lion". Ira Allen later referred to the mountain as "Camel's Rump" on a map from 1798. It was not until 1830 that the name "Camel's Hump" came into usage. The Geographic Names Information System (GNIS) lists twelve variant names including Tah-wak-be-dee-ee-so wadso and Catamountain. While place names are determined by local usage the U.S. Board on Geographic Names (BGN) serves as a central authority in the United States concerning place names. Since its inception in 1890 the BGN has discouraged the use of the genitive apostrophe. Local usage is often at odds with this policy and so the name of this mountain is alternatively spelled with and without an apostrophe.
Camel's Hump is more notable for its shape than its height. Isolated from neighboring peaks by the Winooski Valley and glacial action, the mountain's conical silhouette is distinctive, if misleading. It has two "humps", with the southernmost being the higher, and a steep drop to the south as a result of a quarrying action of the ice passing over it. The movement of glacial ice shaped it into what is referred to as a roche moutonnée. The bedrock consists of phyllite, quartzite and schist.
In 1968 the National Park Service designated Camel's Hump a National Natural Landmark, citing the peak as "an exceptional illustration of the complex anticlinal deformation which formed the Green Mountains". The landmark area consists of approximately 5,300 acres (2,100 ha) from the summit down to 2,500 feet (760 m).
The summit of Camel's Hump is home to 10 acres (4 ha) of alpine tundra vegetation. Common plants found in this area include: Bigelow's sedge (Carex bigelowii), alpine bilberry (Vaccinium uliginosum), mountain sandwort (Minuartia groenlandica), crowberry (Empetrum nigrum), mountain cranberry (Vaccinium vitis-idaea), and Labrador tea (Rhododendron groenlandicum). A direct result of glacial formation, these alpine species were once widespread but as the lower elevations warmed, only the very peak of Camel's Hump remained hospitable to the fragile plants.
There are 18 species of plants at or near the summit of Camel’s Hump that are thought to be rare or very rare. Of these, five species are protected by the Vermont endangered and threatened species rule: Boott's rattlesnake-root (Nabalus boottii, generically known as white lettuce), bearberry willow (Salix uva-ursi), lesser wintergreen (Pyrola minor), alpine sweetgrass (Anthoxanthum monticola), and squashberry (Viburnum edule). The Green Mountain Club's Summit Caretaker program actively promotes Leave No Trace principles and helps to protect the alpine tundra natural community on the summit of Camel's Hump.
Despite extensive logging during the late 1800s and a great fire in 1903, Camel's Hump continues to support a significant population of red spruce (Picea rubens). Starting in the 1960s, Hub Vogelmann and his graduate students from the University of Vermont observed an extensive decline in the red spruce population on the west slope of Camel’s Hump. Vogelmann’s 1982 landmark paper “Catastrophe on Camel’s Hump” identified the cause of the decline to be acid rain. Similarly the Forest Decline Project at the University of Vermont published a study in 1991 that again cited acid rain as the culprit. These findings raised public awareness and eventually led to a revision of the Clean Air Act. By 2017, with mounting evidence that the health of red spruce was on the rise, the scourge of acid rain in the northeast had largely come to an end.
The Abnaki name for the mountain was "ta wak be dee esso wadso," or "tahwahbodeay wadso" (wadso meaning mountain), which has been variously translated as "resting place", "sit-down place", and "prudently, we make a campfire in a circle near water (and rest) at this mountain."
In 1905, publisher and philanthropist Joseph Battell donated 1,200 acres (4.9 km2) of virgin forest, including the summit of Camel's Hump, to the State of Vermont. The bequest was intended to form a state park to be kept in a "primitive state" and in 1911 the state forester was given charge of the area who managed the land in accordance with Battell's wishes. Since then, Vermont has adopted new legislation to preserve its natural areas and in 1969 created a Forest Reserve enclosing the mountain. Camel's Hump State Park has grown since the original bequest and in 1991 totalled approximately 20,000 acres (81 km2).
In October 1944, during World War II, a B-24J bomber on a training mission crashed into the side of the mountain near the summit. While most of the plane was salvaged and removed, portions of the wreckage (principally a wing section) still remain. The Alpine Trail passes by the site.
Though protected, the Camel's Hump area is a favorite recreational venue for hikers. Trail work began on Camel's Hump at the formation of the Green Mountain Club (GMC) and by 1912, a trail had been constructed between the mountain and Sterling Pond. This initial trail would later become a high point in the "footpath in the wilderness" known as the Long Trail. In the 1950s, the GMC constructed shelters along the trail and at the summit. The GMC now trains and pays a caretaker to reside near the summit during the summer and educate hikers to respect the fragile alpine ecosystem that exists on the mountain.
In 1999, an image of Camel's Hump was chosen as a prominent feature for the Vermont state quarter. While many other options were considered, including covered bridges and the snowflake photographs of Wilson Bentley, the seven-person panel ultimately decided on Camel's Hump stating that it was "perfect for the quarter." The panels findings explained the choice: "It's wild and natural, like the Vermont countryside. It's unique and asymmetrical, like the independent and quirky reputation Vermonters have." Many notable Vermont institutions have adopted its memorable name, including the children's radio show "Camel's Hump Radio" hosted by Bill Harley on Vermont Public Radio. The profile of Camel's Hump appears in the Vermont coat of arms on the Vermont flag.
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"With the only undeveloped alpine area in the Green Mountain State and a skyline that sets it apart from everything else, Camel's Hump may be Vermont's finest peak," says Michael Lanza in his guidebook for New England hiking enthusiasts. The views from the summit are panoramic, and on a clear day one can see the highest peaks of the following states: Mount Marcy in New York, Mount Washington in New Hampshire, as well as Vermont's Mount Mansfield.
The most popular access points for hikers are the Burrows Trailhead east of Huntington and the Monroe Trailhead south of Duxbury. In 2016, almost 26,000 visitors signed the trail registers at these two trailheads. Parking is also available along Duxbury Road west of Duxbury, but this parking area is much further from Camel's Hump.
There are multiple trails in the vicinity of Camel’s Hump. The Long Trail traverses the summit of Camel’s Hump on a north-south path. The Burrows Trail (from the west) and the Monroe Trail (from the east) intersect the Long Trail at the Hut Clearing just north of the Camel's Hump summit.
From the Burrows Trailhead
The Burrows Trailhead is at the end of Camel's Hump Road east of Huntington. Since the trailhead is at 1,800 feet (550 m), the vertical rise from there to the summit is 2,283 feet (696 m).
Camel's Hump via the Burrows Trail. The Burrows Trail ascends the west face of Camel's Hump. The trail intersects the Long Trail at the Hut Clearing after 2.1 miles (3.4 km). From the intersection, the summit is 0.3 miles (0.5 km) south on the Long Trail. One-way trip length: 2.4 miles (3.9 km).
The Burrows Trail, the oldest trail on Camel's Hump, travels through some of the oldest spruce-fir forest on the mountain, one of the few areas believed to have escaped the 1903 fire. The Burrows Trail is also used in the winter as a snowshoe and ski route.
Camel's Hump via the Forest City Trail. The Forest City Trail is 0.1 miles (0.2 km) from the Burrows Trailhead along a connector trail. The trail intersects the Long Trail in 1.4 miles (2.3 km). From the intersection, the summit is 1.9 miles (3.1 km) north on the Long Trail. One-way trip length: 3.4 miles (5.5 km).
The Forest City Trail follows an old logging road used by the Forest City Lumber Company to log much of the western side of the mountain in the late 1800s and early 1900s. The trail terminates at the Long Trail, not far from Montclair Glen Lodge, which was built by the Green Mountain Club in 1948.
From the Monroe Trailhead
The Monroe Trailhead is at the end of Camel's Hump Road south of Duxbury. Since the trailhead is at 1,500 feet (460 m), the vertical rise from there to the summit is 2,583 feet (787 m).
Camel's Hump via the Monroe Trail. The Monroe Trail ascends the east face of Camel's Hump. The trail intersects the Long Trail at the Hut Clearing after 3.1 miles (5.0 km). From the intersection, the summit is 0.3 miles (0.5 km) south on the Long Trail. One-way trip length: 3.4 miles (5.5 km).
The Monroe Trail was built in 1912. It is named for Will Monroe, who cut the Long Trail from Camel’s Hump south to Middlebury Gap beginning in 1916. The Monroe Trail climbs through an extensive grove of paper birch that dates from the 1903 fire.
Camel's Hump via the Dean Trail. The Dean Trail is 1.3 miles (2.1 km) from the Monroe Trailhead, intersecting the Long Trail in 1.0 mile (1.6 km). From the intersection, the summit is 1.7 miles (2.7 km) north on the Long Trail. One-way trip length: 4.0 miles (6.4 km).
The Dean Trail crosses the Hump Brook Bridge 0.2 miles (0.3 km) from the Monroe Trail. At 0.3 miles (0.5 km), it reaches a spur trail to the Hump Brook Tenting Area, with tent platforms and campsites (available for a fee). At 0.7 miles (1.1 km) from the Monroe Trail, the Dean Trail overlooks a beaver pond with views of Camel's Hump.
Camel's Hump via the Alpine Trail. The Alpine Trail is 2.5 miles (4.0 km) from the trailhead, intersecting the Long Trail in 0.5 miles (0.8 km). From the intersection, the summit is 0.2 miles (0.3 km) north on the Long Trail. One-way trip length: 3.2 miles (5.1 km).
The Alpine Trail traverses the site of a plane crash that occurred on Camel's Hump in October 1944. A B-24J Liberator bomber from Westover Air Force Base (now Westover Air Reserve Base) in Massachusetts struck the mountain just 100 feet (30 m) below the summit, scattering debris over the snow-covered peak. The collision killed nine crew members and left one survivor.
From Duxbury Road
From the parking lot on Duxbury Road, the Long Trail climbs south 2.7 miles (4.3 km) to a spur that leads 0.2 miles (0.3 km) east to the Bamforth Ridge Shelter. From there, it is 3.5 miles (5.6 km) south on the Long Trail to the summit. With a stop at the shelter, the one-way trip is 6.4 miles (10.3 km) with 3,683 feet (1,123 m) of elevation change. This is the largest vertical climb on the entire Long Trail.
Western face of Camel's Hump Mountain from South Burlington, Vermont.
Camel's Hump from Hinesburg Hollow Rd., Huntington, Vermont: Jul 2006
Painting of Camel's Hump by John Frederick Kensett, 1852, oil on canvas.
- Alfieri, Amy; Chipman, Brian; Gobeille, John; Johnson, Michael; Leonard, Matthew; Nerenberg, Jason; Peterson, Robert; Sausville, David; Sabourin, Gary; Zaino, Robert (2017). "Camel's Hump Management Unit: Long Range Management Plan" (PDF). State of Vermont: Agency of Natural Resources; Department of Forests, Parks and Recreation; Fish and Wildlife Department. Retrieved 21 January 2020.
- Johnson, Charles W. (1998). The Nature of Vermont: Introduction and Guide to a New England Environment. Hanover, NH: University Press of New England. ISBN 0-87451-856-3.
- Meeks, Harold A. (1986). Vermont's Land and Resources. The New England Press. ISBN 0-933050-40-2.
- Morrissey, Charles T. (1984). Vermont: A History. W. W. Norton and Co. ISBN 0-393-30223-7.
- "Camels Hump 2 Reset". NGS data sheet. U.S. National Geodetic Survey. Retrieved 2008-11-24.
- "Camels Hump, Vermont". Peakbagger.com. Retrieved 2008-11-24.
- Bazilchuk, Nancy. "Camel's Hump State Park". The Longstreet Highroad Guide to the Vermont Mountains. ISBN 1-56352-504-6. Retrieved 2008-04-16.
- "Camel's Hump State Park". Retrieved July 1, 2007.
- "Camels Hump". Geographic Names Information System. United States Geological Survey. Retrieved April 4, 2010.
- "Domestic Names - Frequently Asked Questions". U.S. Board on Geographic Names. Retrieved April 4, 2010.
- Thompson, Peter and Thelma (1991). "Bedrock Geology of the Camels Hump-Bolton Mountain Area, North-Central Vermont" (PDF). Retrieved 27 January 2016.
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- "National Natural Landmarks: Camel's Hump". National Park Service. Retrieved 11 February 2020.
- Preserving Our Natural Heritage, Volume II. p. 586. Retrieved 11 February 2020.
- Alfieri et al. 2017, pp. 31–33.
- "10 App. V.S.A. § 10". The Vermont Statutes Online. Retrieved 29 January 2020.
- "Backcountry Caretakers". Green Mountain Club. Retrieved 29 January 2020.
- Alfieri et al. 2017, p. 11.
- Brown, Joshua E. (October 14, 2013). "Remembering Hub Vogelmann". University of Vermont. Retrieved 30 January 2020.
- Klein, Richard M.; Perkins; Tricou; Oates; Cutler (Sep 1991). "Factors Affecting Red Spruce Regeneration in Declining Areas of Camel's Hump Mountain, Vermont". American Journal of Botany. 78 (9): 1191–1198. doi:10.2307/2444923. JSTOR 2444923.
- Alfieri et al. 2017, p. 54.
- Dillon, John (June 12, 2018). "UVM Study: Spruce Trees Are Recovering From Acid Rain, Years After Tighter Pollution Controls". Vermont Public Radio. Retrieved 29 January 2020.
- Huden, John C (1962). Indian Place Names of New England. Museum of the American Indian Heye Foundation. ISBN 0-934490-18-X.
- Ring, Wilson (October 7, 2001). "Vermont still has stands of old-growth forests". The Associated Press State & Local Wire.
- "History of the Long Trail". The Green Mountain Club. Archived from the original on 2007-06-30. Retrieved June 19, 2007.
- "Camel's Hump picked for new Vt. quarter". The Boston Globe. Associated Press. June 11, 1999.
- "Camel's Hump". Vermont Public Radio. Retrieved June 19, 2007.
- Lanza, Michael (2004). Foghorn Outdoors' New England Hiking: The Complete Guide to More Than 380 Hikes. Avalon Travel Publishing. ISBN 1-56691-381-0.
- "Camel's Hump". Dartmouth Outing Guide. Dartmouth Outing Club. 2004. p. 173. Retrieved 2008-11-27.
- Alfieri et al. 2017, Appendix G: Trail Register Sign-Ins Summary 1988–2016.
- "Detailed Directions to Camel's Hump State Park" (PDF). Vermont Department of Forests, Parks and Recreation. Retrieved 6 February 2020.
- "Camel's Hump State Park Trails Guide" (PDF). Vermont Department of Forests, Parks and Recreation. 2017. Retrieved 21 January 2020.
- Day Hiker's Guide to Vermont (6th ed.). Waterbury Center, Vermont: Green Mountain Club. 2011. ISBN 978-1-888021-35-6.
|Wikimedia Commons has media related to Camel's Hump.|
- Camel's Hump State Park - official site
- "Camels Hump". Geographic Names Information System. United States Geological Survey. Retrieved 2008-11-27.
- "Hiking Camel's Hump, Vermont". Peakbagging the 4000 Footer Mountains of New England. Retrieved 2008-11-27.
- "Camel's Hump Mountain Photo Group". Flickr. May 2014. Retrieved 2014-05-24.
- "Camel's Hump hike and trip report". Peak Fever. June 2011. Retrieved 2011-07-14.