Camel's Hump

{{Short description|Mountain in Vermont, US}}

{{About||the peak named "Camels Hump" in Australia|Mount Macedon|the hump of a camel|Camel#Hump}}

{{Use mdy dates|date=January 2025}}

{{Infobox mountain

| name = Camel's Hump

| other_name = Moziozagan

| photo = CamelsHumpMT 20060728.jpg

| photo_caption = Camel's Hump, July 2006

| map = Vermont

| map_alt = Camel's Hump in the State of Vermont in the United States

| map_caption = Vermont, U.S.A.

| map_relief = yes

| map_size = 200

| elevation_ft = 4083

| elevation_ref = {{cite map |author=Green Mountain Club |author-link=Green Mountain Club |title=Vermont's Long Trail: A Footpath in the Wilderness |year=2015 |type=Topographic map |scale=1:85,000 |cartography=Center for Community GIS |edition=5th |isbn=978-1-888021-46-2}}

| prominence_ft = 1860

| prominence_ref = {{cite peakbagger |pid=7016 |name=Camels Hump, Vermont |accessdate=2008-11-24}}

| listing = New England 4,000-footers
New England Fifty Finest #46

| country = United States

| state = Vermont

| district = Chittenden / Washington

| district_type = County

| settlement = Huntington / Duxbury

| settlement_type = Town

| range = Green Mountains

| coordinates = {{coord|44|19|11|N|72|53|10|W|region:US-VT_type:mountain_source:ngs|display=inline,title}}

| coordinates_ref = {{cite ngs |id=PG1684 |name=Camels Hump 2 Reset |accessdate=2008-11-24}}

| age = 550 million years

| first_ascent =

| easiest_route = Hiking trail

| embedded = {{designation list |embed=yes |designation1=NNL |designation1_date=1968}}

}}

Camel's Hump (alternatively Camels Hump) is a mountain in the Green Mountains in the U.S. state of Vermont. The north slope of the mountain borders the Winooski River, which has carved through the Green Mountains over eons. At {{cvt|4083|feet}}, it is tied with Mount Ellen for the third-highest mountain in Vermont. Surmounted by {{cvt|10|acre|ha|0}} of alpine tundra, the mountain is the most significant feature 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.

Name

The Abenaki were the first to note this mountain's distinctive shape, calling it Moziozagan, meaning moose's shoulder.{{cite web|url=https://mfw.us/blog/wp-content/uploads/2021/04/0320Dictionary.pdf|title=Abenaki/English|website=mfw.us}} Subsequent European names continued this pattern: in 1609, Samuel de Champlain named the mountain "Le Lion Couchant", a heraldic description which roughly translates as "The Resting Lion".{{cite web |last1=Bushnell |first1=Mark |title=Whence Camel's Hump and other Vermont mountain names? |url=https://vtdigger.org/2019/09/15/then-again-whence-camels-hump-and-other-vermont-mountain-names/ |publisher=VTDigger |access-date=16 March 2020 |date=September 15, 2019}} 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.{{cite web |url=http://www.central-vt.com/visit/attract/camhump/index.html |archive-url=https://web.archive.org/web/19980211044949/http://www.central-vt.com/visit/attract/camhump/index.html |url-status=usurped |archive-date=February 11, 1998 |title=Camel's Hump State Park |access-date=July 1, 2007}}

The Geographic Names Information System (GNIS) lists twelve variant names including {{lang|abe|Tah-wak-be-dee-ee-so wadso}} and Catamountain.{{cite gnis |id=1456724 |name=Camels Hump |accessdate=April 4, 2010}} 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.{{cite web |url=http://geonames.usgs.gov/domestic/faqs.htm |title=Domestic Names - Frequently Asked Questions |publisher=U.S. Board on Geographic Names |access-date=April 4, 2010 |archive-date=January 5, 2017 |archive-url=https://web.archive.org/web/20170105041005/https://geonames.usgs.gov/domestic/faqs.htm |url-status=live }} Local usage is often at odds with this policy and so the name of this mountain is alternatively spelled with and without an apostrophe.

Geology

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.{{Citation needed|reason=Reliable source needed|date=February 2020}} The bedrock consists of phyllite, quartzite, and schist.{{Cite web |url=http://www.anr.state.vt.us/dec/geo/SpecialBulletins/Thompson_1991SpB12.pdf |title=Bedrock Geology of the Camels Hump-Bolton Mountain Area, North-Central Vermont |date=1991 |access-date=27 January 2016 |last=Thompson |first=Peter and Thelma |archive-date=7 September 2015 |archive-url=https://web.archive.org/web/20150907011012/http://www.anr.state.vt.us/dec/geo/SpecialBulletins/Thompson_1991SpB12.pdf |url-status=live }}

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".{{cite web |title=Camel's Hump: National Natural Landmark |publisher=National Park Service |url=http://www.nature.nps.gov/nnl/Registry/USA_Map/States/Vermont/NNL/CH/index.cfm |access-date=2007-06-19 |archive-url=https://web.archive.org/web/20100528141037/http://www.nature.nps.gov/nnl/Registry/USA_Map/States/Vermont/NNL/CH/index.cfm |archive-date=2010-05-28 |url-status=dead}} The landmark area consists of approximately {{cvt|5300|acres}} from the summit down to {{cvt|2500|feet}}.{{cite web |url=https://www.nps.gov/subjects/nnlandmarks/site.htm?Site=CAHU-VT |title=National Natural Landmarks: Camel's Hump |publisher=National Park Service |language=en |access-date=11 February 2020 |archive-date=13 July 2019 |archive-url=https://web.archive.org/web/20190713090053/https://www.nps.gov/subjects/nnlandmarks/site.htm?Site=CAHU-VT |url-status=live }}{{cite book |title=Preserving Our Natural Heritage, Volume II |page=586 |url=https://books.google.com/books?id=bRFF-ixDXT8C&pg=PA586 |access-date=11 February 2020 |archive-date=2 October 2022 |archive-url=https://web.archive.org/web/20221002193922/https://books.google.com/books?id=bRFF-ixDXT8C&pg=PA586 |url-status=live }}

Climate

{{Weather box

|location = Camel's Hump 44.3168 N, 72.8828 W, Elevation: {{cvt|3438|ft}} (1991–2020 normals)

|single line = y

|Jan high F = 19.0

|Feb high F = 21.0

|Mar high F = 28.6

|Apr high F = 42.7

|May high F = 56.0

|Jun high F = 64.3

|Jul high F = 68.4

|Aug high F = 66.8

|Sep high F = 60.6

|Oct high F = 47.6

|Nov high F = 34.7

|Dec high F = 24.6

|Jan mean F = 11.1

|Feb mean F = 13.0

|Mar mean F = 21.0

|Apr mean F = 34.2

|May mean F = 47.7

|Jun mean F = 56.9

|Jul mean F = 61.5

|Aug mean F = 59.9

|Sep mean F = 53.2

|Oct mean F = 40.7

|Nov mean F = 28.2

|Dec mean F = 17.8

|Jan low F = 3.2

|Feb low F = 5.0

|Mar low F = 13.3

|Apr low F = 25.8

|May low F = 39.5

|Jun low F = 49.4

|Jul low F = 54.5

|Aug low F = 53.0

|Sep low F = 45.8

|Oct low F = 33.8

|Nov low F = 21.7

|Dec low F = 11.0

|precipitation colour = green

|Jan precipitation inch = 4.77

|Feb precipitation inch = 4.34

|Mar precipitation inch = 5.21

|Apr precipitation inch = 5.49

|May precipitation inch = 5.93

|Jun precipitation inch = 6.77

|Jul precipitation inch = 6.74

|Aug precipitation inch = 6.33

|Sep precipitation inch = 5.70

|Oct precipitation inch = 6.83

|Nov precipitation inch = 5.62

|Dec precipitation inch = 5.94

|source=PRISM Climate Group{{cite web

|url= https://prism.oregonstate.edu/explorer/

|title= PRISM Climate Group, Oregon State University

|publisher= PRISM Climate Group, Oregon State University

|access-date= October 22, 2023

|quote= To find the table data on the PRISM website, start by clicking Coordinates (under Location); copy Latitude and Longitude figures from top of table; click Zoom to location; click Precipitation, Minimum temp, Mean temp, Maximum temp; click 30-year normals, 1991-2020; click 800m; click Retrieve Time Series button.}}

}}

Botany

File:CamelsHumpSummitGrass 20080624.jpg grasses at the summit of Camel's Hump, Vermont, June 2008.]]

The summit of Camel's Hump is home to {{cvt|10|acre|ha|0}} 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.{{cite book |chapter-url=https://www.nasw.org/users/nbazilchuk/Articles/Camel.htm |last=Bazilchuk |first=Nancy |chapter=Camel's Hump State Park |title=The Longstreet Highroad Guide to the Vermont Mountains |access-date=2008-04-16 |isbn=1-56352-504-6 |archive-date=2022-10-02 |archive-url=https://web.archive.org/web/20221002193919/https://www.nasw.org/users/nbazilchuk/Articles/Camel.htm |url-status=live }}

There are 18 species of plants at or near the summit of Camel's Hump that are thought to be rare or very rare.{{sfn|Alfieri|Chipman|Gobeille|Johnson|2017|pp=31–33}} Of these, five species are protected by the Vermont endangered and threatened species rule:{{cite web |title=10 App. V.S.A. § 10 |url=https://legislature.vermont.gov/statutes/section/10APPENDIX/001/00010 |publisher=The Vermont Statutes Online |access-date=29 January 2020 |archive-date=29 January 2020 |archive-url=https://web.archive.org/web/20200129153101/https://legislature.vermont.gov/statutes/section/10APPENDIX/001/00010 |url-status=live }} 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.{{cite web |title=Backcountry Caretakers |url=https://www.greenmountainclub.org/about/employment-opportunities/seasonal-jobs/backcountry-caretakers/ |publisher=Green Mountain Club |access-date=29 January 2020 |archive-date=29 January 2020 |archive-url=https://web.archive.org/web/20200129153057/https://www.greenmountainclub.org/about/employment-opportunities/seasonal-jobs/backcountry-caretakers/ |url-status=live }}

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.{{sfn|Alfieri|Chipman|Gobeille|Johnson|2017|p=11}}{{cite web |last1=Brown |first1=Joshua E. |title=Remembering Hub Vogelmann |url=https://www.uvm.edu/uvmnews/news/remembering-hub-vogelmann |publisher=University of Vermont |access-date=30 January 2020 |date=October 14, 2013 |archive-date=30 January 2020 |archive-url=https://web.archive.org/web/20200130001400/https://www.uvm.edu/uvmnews/news/remembering-hub-vogelmann |url-status=live }} Similarly the Forest Decline Project at the University of Vermont published a study in 1991 that again cited acid rain as the culprit.{{cite journal |last=Klein |first=Richard M. |title=Factors Affecting Red Spruce Regeneration in Declining Areas of Camel's Hump Mountain, Vermont |journal=American Journal of Botany |volume=78 |issue=9 |date=Sep 1991 |pages=1191–1198 |doi=10.2307/2444923 |author2=Perkins |author3=Tricou |author4=Oates |author5=Cutler |jstor=2444923}}

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,{{sfn|Alfieri|Chipman|Gobeille|Johnson|2017|p=54}}{{cite web |last1=Dillon |first1=John |title=UVM Study: Spruce Trees Are Recovering From Acid Rain, Years After Tighter Pollution Controls |url=https://www.vpr.org/post/uvm-study-spruce-trees-are-recovering-acid-rain-years-after-tighter-pollution-controls |publisher=Vermont Public Radio |access-date=29 January 2020 |date=June 12, 2018 |archive-date=29 January 2020 |archive-url=https://web.archive.org/web/20200129191948/https://www.vpr.org/post/uvm-study-spruce-trees-are-recovering-acid-rain-years-after-tighter-pollution-controls |url-status=live }} the scourge of acid rain in the northeast had largely come to an end.

File:Vermont quarter, reverse side, 2001.jpg depicts Camel's Hump and Maple trees with sap buckets]]

History

The Abenaki name for the mountain is "{{langr|abe|ta wak be dee esso wadso}}," or "{{langr|abe|tahwahbodeay wadso}}" ({{langr|abe|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."{{cite book |last=Huden |first=John C |title=Indian Place Names of New England |url=https://archive.org/details/indianplacenames00hude |publisher=Museum of the American Indian Heye Foundation |year=1962 |isbn=0-934490-18-X}}

In 1905, publisher and philanthropist Joseph Battell donated {{cvt|1200|acres|km2|sigfig=2}} of virgin forest, including the summit of Camel's Hump, to the State of Vermont.{{cite news |last=Ring |first=Wilson |title=Vermont still has stands of old-growth forests |agency=The Associated Press State & Local Wire |date=October 7, 2001}}

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 {{cvt|20000|acres|km2|0}}.

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.{{cite web |url=http://www.greenmountainclub.org/page.php?id=15 |title=History of the Long Trail |publisher=The Green Mountain Club |access-date=June 19, 2007 |archive-url=https://web.archive.org/web/20070630044538/http://www.greenmountainclub.org/page.php?id=15 |archive-date=2007-06-30 |url-status=dead}}

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 panel's 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."{{cite news |title=Camel's Hump picked for new Vt. quarter |agency=Associated Press |publisher=The Boston Globe |date=June 11, 1999}}

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.{{cite web |url=http://www.vpr.net/camelshump/index.html |title=Camel's Hump |publisher=Vermont Public Radio |access-date=June 19, 2007 |archive-date=July 4, 2007 |archive-url=https://web.archive.org/web/20070704025841/http://www.vpr.net/camelshump/index.html |url-status=live }}

The profile of Camel's Hump appears in the Vermont coat of arms on the Vermont flag.

Hiking

File:CamelsHumpMarker.jpg

"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.{{cite book |last=Lanza |first=Michael |title=Foghorn Outdoors' New England Hiking: The Complete Guide to More Than 380 Hikes |url=https://archive.org/details/foghornoutdoorsm00mich_0 |url-access=registration |publisher=Avalon Travel Publishing |isbn=1-56691-381-0 |year=2004}} 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.{{cite web |url=http://www.dartmouth.edu/~doc/hiking/camelshump/ |title=Camel's Hump |work=Dartmouth Outing Guide |publisher=Dartmouth Outing Club |year=2004 |page=173 |access-date=2008-11-27 |archive-date=2008-12-12 |archive-url=https://web.archive.org/web/20081212130219/http://www.dartmouth.edu/~doc/hiking/camelshump/ |url-status=live }}

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.{{sfn|Alfieri|Chipman|Gobeille|Johnson|2017|loc=[https://fpr.vermont.gov/sites/fpr/files/State_Lands_Administration/Lands_Management_Planning/Library/CHMU_LRMP_APPENDIX%20G-Recreation%20Use%20Data.pdf Appendix G: Trail Register Sign-Ins Summary 1988–2016]}} Parking is also available along Duxbury Road west of Duxbury,{{cite web |title=Detailed Directions to Camel's Hump State Park |url=https://vtstateparks.com/assets/pdf/camels-directions-detail.pdf |publisher=Vermont Department of Forests, Parks and Recreation |access-date=6 February 2020 |archive-date=4 October 2019 |archive-url=https://web.archive.org/web/20191004151530/https://vtstateparks.com/assets/pdf/camels-directions-detail.pdf |url-status=live }} but this parking area is much further from Camel's Hump.

There are multiple trails in the vicinity of Camel's Hump.{{cite web |title=Camel's Hump State Park Trails Guide |url=https://vtstateparks.com/assets/pdf/camels_hump_trails.pdf |publisher=Vermont Department of Forests, Parks and Recreation |access-date=21 January 2020 |date=2017 |archive-date=4 October 2019 |archive-url=https://web.archive.org/web/20191004002703/https://vtstateparks.com/assets/pdf/camels_hump_trails.pdf |url-status=live }}{{cite book |title=Day Hiker's Guide to Vermont |date=2011 |publisher=Green Mountain Club |location=Waterbury Center, Vermont |isbn=978-1-888021-35-6 |edition=6th}} 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 ({{cvt|1800|ft|m|disp=or}}) is at the end of Camel's Hump Road east of Huntington. The vertical rise from the trailhead to the summit is {{cvt|2283|feet}}.

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 {{cvt|2.1|mi|1}}. From the intersection, the summit is {{cvt|0.3|mi|1}} south on the Long Trail. One-way trip length: {{cvt|2.4|mi|1}}. This is the shortest (and steepest) hike to the summit of Camel's Hump.

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 {{cvt|0.1|mi|1}} from the Burrows Trailhead along a connector trail. The Forest City Trail intersects the Long Trail in {{cvt|1.4|mi|1}}. From the intersection, the summit is {{cvt|1.9|mi|1}} north on the Long Trail. One-way trip length: {{cvt|3.4|mi|1}}.

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 ({{cvt|1500|ft|m|disp=or}}) is at the end of Camel's Hump Road south of Duxbury. The vertical rise from the trailhead to the summit is {{cvt|2583|feet}}.

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 {{cvt|3.1|mi|1}}. From the intersection, the summit is {{cvt|0.3|mi|1}} south on the Long Trail. One-way trip length: {{cvt|3.4|mi|1}}.

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 {{cvt|1.3|mi|1}} from the Monroe Trailhead. The trail intersects the Long Trail in {{cvt|1.0|mi|1}}. From the intersection, the summit is {{cvt|1.7|mi|1}} north on the Long Trail. One-way trip length: {{cvt|4.0|mi|1}}.

The Dean Trail crosses the Hump Brook Bridge {{cvt|0.2|mi|1}} from the Monroe Trail. At {{cvt|0.3|mi|1}}, it reaches a spur trail to the Hump Brook Tenting Area, with tent platforms and campsites (available for a fee). At {{cvt|0.7|mi|1}} 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 {{cvt|2.5|mi|1}} from the Monroe Trailhead. The trail intersects the Long Trail in {{cvt|0.5|mi|1}}. From the intersection, the summit is {{cvt|0.2|mi|1}} north on the Long Trail. One-way trip length: {{cvt|3.2|mi|1}}.

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 {{cvt|100|feet}} 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 {{cvt|2.7|mi|1}} to a spur that leads {{cvt|0.2|mi|1}} east to the Bamforth Ridge Shelter. From there, it is {{cvt|3.5|mi|1}} south on the Long Trail to the summit. With a stop at the shelter, the one-way trip is {{cvt|6.4|mi|1}} with {{cvt|3683|feet}} of elevation change. This is the longest climb on the entire Long Trail.

Gallery

Image:CamelsHumpFromWest 20150128.jpg|Western face of Camel's Hump Mountain from South Burlington, Vermont.

Image:CamelsHumpSummit Southward2 20170902.jpg|Southward view from the summit of Camel's Hump (with Mt. Ethan Allen in the immediate foreground), September 2017.

Image:View of Lake Champlain and Vermont from Poke-O-Moonshine Mountain fire tower.jpg|View east from old fire tower atop Poke-O-Moonshine Mountain in Chesterfield, NY: 2008

Image:'Camel's Hump from the Western Shore of Lake Champlain' by John Frederick Kensett.JPG|Painting of Camel's Hump by John Frederick Kensett, 1852, oil on canvas.

Image:Camel's Hump-VT.jpg|Eastern face of Camel's Hump taken in 1968

Image:Camels Hump, from golf course, Waterbury, Vt (66378).jpg|Postcard of eastern face of Camel's Hump

Image:Camel's Hump and Winooski River, Green Mountains, Vermont (70586).jpg|Postcard of western face of Camel's Hump

Image:Camels_Hump,_Vermont,_2020-05-19.jpg|A view of Camel's Hump from the Allis Trail to the southeast

See also

References

{{Reflist}}

Bibliography

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  • {{cite web |first1=Amy |last1=Alfieri |first2=Brian |last2=Chipman |first3=John |last3=Gobeille |first4=Michael |last4=Johnson |first5=Matthew |last5=Leonard |first6=Jason |last6=Nerenberg |first7=Robert |last7=Peterson |first8=David |last8=Sausville |first9=Gary |last9=Sabourin |first10=Robert |last10=Zaino |title=Camel's Hump Management Unit: Long Range Management Plan |url=https://fpr.vermont.gov/sites/fpr/files/State_Lands_Administration/Lands_Management_Planning/Library/CHMU_DRAFT_LRMP.pdf |publisher=State of Vermont: Agency of Natural Resources; Department of Forests, Parks and Recreation; Fish and Wildlife Department |access-date=21 January 2020 |date=2017 |archive-date=25 September 2020 |archive-url=https://web.archive.org/web/20200925171640/https://fpr.vermont.gov/sites/fpr/files/State_Lands_Administration/Lands_Management_Planning/Library/CHMU_DRAFT_LRMP.pdf |url-status=live }}
  • {{cite web |first1=Amy |last1=Alfieri |first2=Karen |last2=Bates |first3=John |last3=Gobeille |first4=Michael |last4=Johnson |first5=Matthew |last5=Leonard |first6=Toni |last6=Mikula |first7=Jason |last7=Nerenberg |first8=Robert |last8=Peterson |first9=David |last9=Sausville |first10=Lee |last10=Simard |first11=Kathryn |last11=Wrigley |first12=Robert |last12=Zaino |first13=Bill |last13=Baron |first14=Brian |last14=Chipman |first15=Gary |last15=Sabourin |first16=Gary |last16=Sawyer |title=Camel's Hump Management Unit: Long Range Management Plan |publisher=State of Vermont, Agency of Natural Resources: Department of Forests, Parks and Recreation; Fish and Wildlife Department |date=October 2021 |url=https://fpr.vermont.gov/sites/fpr/files/State_Lands_Administration/Lands_Management_Planning/Library/CHMU%20LRMP%20FINAL%20Signed%20-%20Compressed.pdf |access-date=1 May 2023}}
  • {{cite book |last=Johnson |first=Charles W. |year=1998 |title=The Nature of Vermont: Introduction and Guide to a New England Environment |publisher=University Press of New England |location=Hanover, NH |isbn=0-87451-856-3 |url=https://archive.org/details/natureofvermonti00char |url-access=registration }}
  • {{cite book |last=Meeks |first=Harold A. |year=1986 |title=Vermont's Land and Resources |publisher=The New England Press |isbn=0-933050-40-2 |url-access=registration |url=https://archive.org/details/vermontslandreso00meek }}
  • {{cite book |last=Morrissey |first=Charles T. |year=1984 |title=Vermont: A History |publisher=W. W. Norton and Co. |isbn=0-393-30223-7}}

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