Mount Silvertip | |
---|---|
Highest point | |
Elevation | 9,400 ft (2,865 m) [1] [2] |
Prominence | 2,556 ft (779 m) [1] |
Parent peak | Black Cap (9,850 ft) [3] |
Isolation | 6.23 mi (10.03 km) [3] |
Coordinates | 63°29′20″N145°36′35″W / 63.4889633°N 145.6097857°W [4] |
Geography | |
Country | United States |
State | Alaska |
Census Area | Southeast Fairbanks [4] |
Parent range | Alaska Range Delta Mountains [5] |
Topo map | USGS Mount Hayes B-4 |
Mount Silvertip is a 9,400-foot-elevation (2,865-meter) mountain summit in Alaska.
Mount Silvertip is located 32 miles (51 km) north of Paxson in the Delta Mountains which are a subrange of the Alaska Range. [4] Precipitation runoff and glacial meltwater from the heavily glaciated mountain's slopes drains into tributaries of the Delta River and Tanana River. Topographic relief is significant as the summit rises 4,400 feet (1,341 meters) above the Jarvis Glacier in two miles (3.2 km) and 7,100 feet (2,164 meters) above the Delta River in 6.5 miles (10.5 km). The mountain's toponym was officially adopted in 1968 by the United States Board on Geographic Names. [4]
According to the Köppen climate classification system, Mount Silvertip is located in a tundra climate zone with cold, snowy winters, and cool summers. [6] Weather systems are forced upwards by the Delta Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall. Winter temperatures can drop below 0 °F with wind chill factors below −10 °F. This climate supports the Castner Glacier, Riley Creek Glacier, and smaller unnamed glaciers surrounding the peak. The months of March through June offer the most favorable weather for climbing the mountain. [2]
Mount Huxley is a 12,216-foot glaciated mountain summit located in the Saint Elias Mountains of Wrangell-St. Elias National Park and Preserve, in the U.S. state of Alaska. The remote peak is situated 75 mi (121 km) northwest of Yakutat, and 8.7 mi (14 km) west-northwest of Mount Saint Elias. The peak rises above the Columbus Glacier and Bagley Icefield to its north, the Tyndall Glacier to the south, and the Yahtse Glacier to the west. Precipitation runoff from the mountain drains into the Gulf of Alaska. The mountain was named in 1886 by English mountaineer Harold Ward Topham for Thomas Henry Huxley (1825-1895), an English biologist. The mountain was officially named Huxley Peak in 1917, but the name was officially changed to Mount Huxley in 1968 by the U.S. Board on Geographic Names. The first ascent of the peak was made June 9, 1996 by Paul Claus who landed his plane at 11,500 feet elevation on the western flank and climbed the remaining distance to the summit. The second ascent of Mt. Huxley, and first complete ascent from base to summit, was made in June 2018 by Scott Peters, Andrew Peter, and Ben Iwrey starting from the Columbus Glacier.
Mount Carmack is a prominent 6,808-foot-elevation (2,075-meter) mountain summit located in the Boundary Ranges of the Coast Mountains, in the U.S. state of Alaska. The peak is situated 7 mi (11 km) north-northeast of Skagway, and 3.5 mi (6 km) south of Mount Cleveland, on land managed by Tongass National Forest. As the highpoint on the divide between the Taiya River and the Skagway River, precipitation runoff from the mountain drains east into the Skagway River and west into Taiya River, both of which empty into Taiya Inlet. Although modest in elevation, relief is significant since Mount Carmack rises 6,800 feet above the Taiya valley in less than 2 mi (3 km), and 5,800 feet above Skagway valley in about 2 miles. Mount Carmack has a lower subsidiary summit, elevation 6,621 ft (2,020 m), about 0.5 mi (1 km) to the northeast of the true summit. The USGS topographic map has this lower northeast peak labelled as Mount Carmack.
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