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Revision as of 06:38, 16 August 2007 editEncMstr (talk | contribs)Edit filter managers, Administrators49,259 edits remove unused nps.gov refererence; add some history; tidy up some wording← Previous edit Revision as of 20:51, 2 December 2007 edit undo67.142.130.29 (talk) See www.govtrack.us/congress/bill.xpd?bill=s110-647....new expanded wilderness bill has not passed yet...DLinthNext edit →
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{{main|Mount Hood}} {{main|Mount Hood}}
The '''Palmer Glacier''' is a ] located on the upper slopes of ] in the ] of ].<ref> {{cite web| title =Palmer Glacier, USGS Mount Hood South (OR) Topo Map| publisher =Topozone| url =http://www.topozone.com/map.asp?lat=45.35086&lon=-121.70643&s=100&size=l&u=6&datum=nad27&layer=DRG| accessdate = 2007-02-20}} </ref> It is on the south side of the mountain ranging in elevation from about 6,200 to 9,300 ft (1,900 to 2,830 m), and was named for ], an Oregon pioneer. Palmer Glacier is the most well-known of the twelve glaciers on the mountain, and is a popular destination for snow sport enthusiasts. Some of the lower part is within the ], and can be accessed by ] or by ], conditions permitting. The rest is in ]. The '''Palmer Glacier''' is a ] located on the upper slopes of ] in the ] of ].<ref> {{cite web| title =Palmer Glacier, USGS Mount Hood South (OR) Topo Map| publisher =Topozone| url =http://www.topozone.com/map.asp?lat=45.35086&lon=-121.70643&s=100&size=l&u=6&datum=nad27&layer=DRG| accessdate = 2007-02-20}} </ref> It is on the south side of the mountain ranging in elevation from about 6,200 to 9,300 ft (1,900 to 2,830 m), and was named for ], an Oregon pioneer. Palmer Glacier is the most well-known of the twelve glaciers on the mountain, and is a popular destination for snow sport enthusiasts. Some of the lower part is within the ], and can be accessed by ] or by ], conditions permitting.


The glacier is a remnant of the massive glaciers that formed during the last ], and is the only location in ] that provides skiing and snowboarding all twelve months of the year. The glacier is a remnant of the massive glaciers that formed during the last ], and is the only location in ] that provides skiing and snowboarding all twelve months of the year.
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], a warming hut for climbers and skiers, is located near the base of the glacier, about 1,000 vertical feet (305 m) up from ] near the upper terminal of the ] ski lift. ], a warming hut for climbers and skiers, is located near the base of the glacier, about 1,000 vertical feet (305 m) up from ] near the upper terminal of the ] ski lift.


The glacier is bounded on the east by a ridge shared with ] Canyon (which contains White River Glacier) and on the west by Zigzag Glacier and Zigzag Canyon, the source of the ]. The upper glacier narrows to a vertex near the base of ''Steel Cliff'', an area known as ''Triangle Moraine''. The lower extent of the glacier varies significantly seasonally, varying in length by almost two miles (3.2 km), where it might better be referred to as a ''snow field''. The glacier is bounded on the east by a ridge shared with ] Canyon (which contains White River Glacier) and on the west by Zigzag Glacier and Zigzag Canyon, the source of the ]. The upper glacier narrows to a vertex near the base of ''Steel Cliff'', an area known as ''Triangle Moraine''. Below the glacier, its snowfield varies significantly seasonally, varying in length by almost two miles (3.2 km.)
During the summer ski season (approximately May through September), the upper half of the ''Palmer Chairlift'' terrain is divided into lanes (visible in photo) for the same reason as a lap swimming pool. The lanes beside the lift are open to the public; the others are allocated to ski and snowboard camps, coaches and other organizations. During the summer ski season (approximately May through September), the upper half of the ''Palmer Chairlift'' terrain is divided into lanes (visible in photo) for the same reason as a lap swimming pool. The lanes beside the lift are open to the public; the others are allocated to ski and snowboard camps, coaches and other organizations.

Revision as of 20:51, 2 December 2007

TypeMountain glacier
LocationOregon, U.S.
Coordinates45°21′03″N 121°42′23″W / 45.35083°N 121.70639°W / 45.35083; -121.70639
Length2 mi or 3 km (est)
TerminusTalus
StatusRetreating
Main article: Mount Hood

The Palmer Glacier is a glacier located on the upper slopes of Mount Hood in the U.S. state of Oregon. It is on the south side of the mountain ranging in elevation from about 6,200 to 9,300 ft (1,900 to 2,830 m), and was named for Joel Palmer, an Oregon pioneer. Palmer Glacier is the most well-known of the twelve glaciers on the mountain, and is a popular destination for snow sport enthusiasts. Some of the lower part is within the Timberline ski area, and can be accessed by Sno-Cat or by chairlift, conditions permitting.

The glacier is a remnant of the massive glaciers that formed during the last ice age, and is the only location in North America that provides skiing and snowboarding all twelve months of the year.

The glacier was considered a snow field until a Mazama committee investigated on October 191924 and determined it was, in fact, a glacier and should be named on maps. For some time after that it was known as Salmon River Glacier as it is the headwaters of the Salmon River.

Silcox Hut, a warming hut for climbers and skiers, is located near the base of the glacier, about 1,000 vertical feet (305 m) up from Timberline Lodge near the upper terminal of the Magic Mile ski lift.

The glacier is bounded on the east by a ridge shared with White River Canyon (which contains White River Glacier) and on the west by Zigzag Glacier and Zigzag Canyon, the source of the Zigzag River. The upper glacier narrows to a vertex near the base of Steel Cliff, an area known as Triangle Moraine. Below the glacier, its snowfield varies significantly seasonally, varying in length by almost two miles (3.2 km.)

During the summer ski season (approximately May through September), the upper half of the Palmer Chairlift terrain is divided into lanes (visible in photo) for the same reason as a lap swimming pool. The lanes beside the lift are open to the public; the others are allocated to ski and snowboard camps, coaches and other organizations.

See also

References cited

  1. "Palmer Glacier, USGS Mount Hood South (OR) Topo Map". Topozone. Retrieved 2007-02-20.
  2. The Mazamas committee consisted of Rodney L. Glisan, L. A. Nelson, Earl A. Marshall, Raymond Smith, Fred McNeil, Everett Philpoe, T. Raymond Conway, and Fred W. Stadter.
  3. Jack Grauer (July 1975). Mount Hood: A Complete History. self published. p. 289. ISBN 0-930584-01-5.
Glaciers of Mount Hood
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