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Main articles: Mount Hood

Summer Solstice on the Hogsback looking up toward Pearly Gates; the Bergschrund is at center.
The 'Coalman Glacier' (also 'Coleman Glacier') is a
glacier located on the upper slopes of
Mount Hood in the
U.S. state of
Oregon.
[1] It is the mountain's highest glacier ranging from about 10,500 to 11,200 ft (3,200 to 3,415 m), located within the crater rim, southwest of the peak. It was named for Elija Coalman
[2] (variously spelled ''Elijah Coleman''
[3]), an early
mountain guide who climbed
Mount Hood 586 times.
[4]
It is the second most frequently visited glacier on the mountain because it is part of the popular South Climbing route from
Timberline Lodge. It lies entirely within
Mount Hood Wilderness. The most well known feature of Coalman is the ''Hogsback'': a snow ridge running southwest to northeast from Crater Rock toward the summit ridge. The
Bergschrund is another widely known feature where the glacier pulls away from the headwall leaving a large
crevasse. In 2007, it had become large enough to cause most climbers to use another route.
[5]
The glacier is a remnant of the massive glaciers that formed during the last
ice age. It is historically known to change configuration dramatically, at times a gradual, smooth surface to Hot Rocks; at other times the same place has a 40 ft (12 m) ice cliff.
The glacier flows southwest, and is bounded on the north and east by the summit, on the northwest by the rocky crater wall known as ''Castle Crags'' (also ''Hawkins Cliffs''), on the west by ''Hot Rocks'', and on southeast by the back side of ''Steel Cliff''.
See also
★
List of glaciers
References cited
1. Coalman Glacier, USGS Mount Hood South (OR) Topo Map
2. Mount Hood: A Complete History, Jack Grauer, , , self published, , ISBN 0-930584-01-5
3. Mountain Architecture: An Alternative Design Proposal for the Wy'East Day Lodge, Mount Hood Oregon Thomas P. Deering, Jr.
4. 1910: Famous Early Mount Hood Climber citing Legacy
5. Previous noticed posted at Mount Hood Climbing Report, May 17th