Doublemint Peak | |
---|---|
![]() Northwest aspect | |
Highest point | |
Elevation | 6,372 ft (1,942 m) [1] |
Prominence | 479 ft (146 m) [2] |
Parent peak | Troublemint Peak [2] |
Isolation | 0.6 mi (0.97 km) [3] |
Coordinates | 61°51′01″N149°02′13″W / 61.850211°N 149.036827°W [2] |
Geography | |
Country | United States |
State | Alaska |
Borough | Matanuska-Susitna |
Protected area | Hatcher Pass Management Area |
Parent range | Talkeetna Mountains [3] |
Topo map | USGS Anchorage D-6 |
Doublemint Peak is a 6,372-foot-elevation (1,942-meter) summit in Alaska, United States.
Doublemint Peak, also known as Doublemint Spires or simply Doublemint, is located 19 miles (31 km) north of Palmer, Alaska, in the Talkeetna Mountains and in the Hatcher Pass Management Area of the state park system. The south spire is 6,372-ft and the lower north spire reaches 6,308-ft elevation. [1] Precipitation runoff from this mountain's west slope drains into headwaters of the Little Susitna River, whereas the east side drains into Moose Creek which is a tributary of the Matanuska River. Topographic relief is significant as the summit rises 3,372 feet (1,028 meters) above Little Susitna River in one mile (1.6 km). The nearest higher neighbor is Troublemint Peak, 0.6 mile (1 km) to the north. [3] The approach to the peak is via the eight-mile Gold Mint Trail which reaches the Mint Glacier Hut. Doublemint was so named in July 1968 by Curt and Gretchen Wagner who compared the granite towers to those in The Bugaboos. [4] Other whimsically named peaks near the Mint Glacier include Spearmint Spire, Triplemint Peak, and Telemint Spire. This mountain's toponym has not been officially adopted by the United States Board on Geographic Names.
Based on the Köppen climate classification, Doublemint is located in a subarctic climate zone with long, cold, snowy winters, and short cool summers. [5] Winter temperatures can drop below 0 °F with wind chill factors below −10 °F. This climate supports remnants of the Doublemint Glacier on the south slope and the Mint Glacier further northwest. The months of May through June offer the most favorable weather for climbing or viewing. [6]
Hatcher Pass is a mountain pass through the southwest part of the Talkeetna Mountains, Alaska. It is named after Robert Hatcher, a prospector and miner. The nearest cities are Palmer and Wasilla approximately 12 miles (19 km) to the south, and Willow approximately 26 mi (42 km) to the west. The communities are at an elevation of approximately 250 ft (76 m) in the Mat-Su valley.
The Talkeetna Mountains are a mountain range in Alaska. The Matanuska and Susitna River valleys, with towns such as Trapper Creek, Talkeetna, Wasilla, Palmer, Sutton, and Chickaloon, roughly bound the Talkeetnas in the westerly parts of the range. Sovereign Mountain rises to 8,849 feet (2,697 m) in the remote and heavily glaciated central part of the range. The east side of the range fronts a broad, about 100 miles (160 km) wide, lake-studded lowland of forests and swamps, across which rises the gigantic Mount Wrangell volcanic edifice. Alaska Highway 4 runs northward through this lowland. Hundreds of miles to the west Alaska Highway 3 runs along the western side of the Talkeetna range, with the Alaska Range directly west. Alaska Highway 1, running along the southern front of the Talkeetna Mountains, lies mainly in a valley marking a tectonic divide between the Jurassic and Cretaceous rocks of the accretionary wedge, island-arc, and basement rocks in the Peninsular terrane, and the Chugach Mountains in the Chugach terrane to the south. The range stretches as much as a hundred miles north to south. Alaska Highway 8, seasonal and unpaved, passes over highlands rising to above 4,000 feet (1,200 m), north of the Talkeetnas.
Tokosha Mountains is a 6,148 ft (1,870 m) multi-peak massif located in the Alaska Range, in Denali National Park and Preserve, in Alaska, United States. It is situated between the toes of Ruth Glacier and Tokositna Glacier, 27 mi (43 km) south-southeast of Denali and 26 mi (42 km) northwest of Talkeetna. Despite its relatively low elevation, it is notable for its Teton-esque granite spires which can be seen from the George Parks Highway. Precipitation runoff from the mountain drains into the Tokositna River → Chulitna River → Susitna River. Topographic relief is significant as the highest summit, Grand Tokosha, rises 3,850 feet above the Ruth Glacier in one mile (1.6 km).
Mount Abbe is an 8200+ feet double summit mountain located in the Fairweather Range of the Saint Elias Mountains, in southeast Alaska. The peak is situated near the terminus of the Johns Hopkins Glacier, within Glacier Bay National Park and Preserve, 100 mi (161 km) northwest of Juneau, and 8.2 mi (13 km) northeast of Mount Orville. Although modest in elevation, relief is significant since the mountain rises up from tidewater in less than two miles. Mount Abbe is often seen and photographed with the Johns Hopkins Glacier, which is a popular destination for cruise ships. The mountain was named in 1936 by William Osgood Field and William Skinner Cooper, of the American Geographical Society, for Cleveland Abbe Jr., (1872-1934), an American geographer. Abbe received a Ph.D. in 1898 from Johns Hopkins University. The Gilman Glacier and Clark Glacier on the mountain's slopes were named for Daniel Coit Gilman, the institution's first president, and William Bullock Clark who was a professor of geology at the university. The mountain's name was officially adopted in 1937 by the United States Geological Survey. The first ascent of the south summit was made June 11, 1977, by Jim Wickwire and Dusan Jagersky via the Southeast Face. Three days later, Dusan Jagersky was killed while descending an unnamed peak. The first ascent of the north summit was made July 14, 1991, by Walter Gove and William Pilling. The months May through June offer the most favorable weather for climbing Mount Abbe, but it's a challenging climb in any conditions, with few attempts.
Awesome Peak is an 8,645-foot-elevation (2,635-meter) mountain summit located 35 miles (56 km) east-northeast of Palmer, in the northern Chugach Mountains of Alaska. This peak of the Matanuska Valley is set midway between Anchorage and Glennallen, near mile 90 of the Glenn Highway. It is situated 15 miles (24 km) west of Matanuska Glacier and 3.7 mi (6 km) southwest of Amulet Peak. Precipitation runoff from the mountain drains into Monument and Coal creeks, which are tributaries of the Matanuska River. Topographic relief is significant as the summit rises 5,650 feet above Coal Creek in 3.75 miles (6 km) and 4,650 feet above Monument Creek in 1.9 mile (3 km). This mountain's toponym has not been officially adopted by the United States Board on Geographic Names, so it is only marked as "8645" on USGS maps.
Tazcol Peak is a 7,850-foot-elevation (2,393-meter) mountain summit located 18 miles (29 km) north-northwest of Valdez in the U.S. state of Alaska. This remote glaciated mountain is set in the Chugach Mountains on land managed by Chugach National Forest. Precipitation runoff from the mountain drains south to Prince William Sound and north to Tazlina Lake → Tazlina River → Copper River. Topographic relief is significant as the summit rises 4,350 feet (1,326 m) above the East Branch of the Columbia Glacier in 1.4 mile (2.25 km). The peak's name was applied in 1959 by mountaineer and glaciologist Lawrence E. Nielsen (1917–1992), and the toponym was officially adopted in 1965 by the U.S. Board on Geographic Names. The word "Tazcol" is a portmanteau blending the names of the Tazlina Glacier and Columbia Glacier which flow from this mountain's north and south slopes respectively.
Mount Balchen is an 11,205-foot-elevation (3,415-meter) mountain summit in Alaska, United States.
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