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Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification".
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is significant as it rises over 5,000 feet (1,500 m) in less than one mile from the immense Childs
Glacier.
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near this mountain in 1909-1910. The mountain's name was officially adopted in 1930 by the
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zone, with long, cold, snowy winters, and cool summers. Winds coming off the
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Mount
Williams (left), seen with Mt. O'Neel, Childs Glacier, and Copper River
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is a 7,200+ ft (2,190+ m) glaciated mountain summit located in the
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284:are forced upwards by the Chugach Mountains (
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471:Landforms of Chugach Census Area, Alaska
408:United States Department of the Interior
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250:Copper River and Northwestern Railway
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144:Location of Mount Williams in Alaska
399:Geographic Names Information System
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16:Mountain in Alaska, United States
328:List of mountain peaks of Alaska
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233:. Although modest in elevation,
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404:United States Geological Survey
379:Mount Williams, listsofjohn.com
262:U.S. Board on Geographic Names
240:The peak was named in 1910 by
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466:North American 2000 m summits
274:Köppen climate classification
248:, assistant engineer for the
69:9.98 mi (16.06 km)
229:, on land managed by
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97:60.7230556°N 144.8966667°W
59:3,200 ft (980 m)
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356:"Mount Williams, Alaska"
254:$ 1,500,000 steel bridge
102:60.7230556; -144.8966667
429:Hydrol. Earth Syst. Sci
231:Chugach National Forest
158:Chugach National Forest
162:Valdez-Cordova Borough
49:7,200+ ft (2,190+ m)
461:Mountains of Alaska
333:Geography of Alaska
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39:Highest point
211:Chugach Mountains
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184:Chugach Mountains
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227:Mount O'Neel
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178:Parent range
256:across the
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88:144°53′48″W
75:Coordinates
455:Categories
413:2020-01-29
365:2020-01-29
339:References
215:U.S. state
85:60°43′23″N
55:Prominence
441:1027-5606
113:Geography
65:Isolation
45:Elevation
292:See also
191:Topo map
154:Location
268:Climate
223:Cordova
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
