Ch'akajabena Mountain | |
---|---|
Highest point | |
Elevation | 7,530 ft (2,295 m) [1] [2] |
Prominence | 1,730 ft (527 m) [2] |
Isolation | 1.66 mi (2.67 km) [1] |
Coordinates | 61°09′39″N152°25′36″W / 61.1608333°N 152.4266667°W [3] |
Geography | |
Country | United States |
State | Alaska |
Borough | Kenai Peninsula Borough [3] |
Parent range | Aleutian Range Neacola Mountains [3] |
Topo map | USGS Tyonek A-7 |
Ch'akajabena Mountain is a 7,530-foot-elevation (2,295-meter) mountain summit in Alaska.
Ch'akajabena Mountain ranks as the seventh-highest peak in the Neacola Mountains which are the northernmost subrange of the Aleutian Range. [2] The mountain is located 85 miles (137 km) west of Anchorage near Ch'akajabena Lake. Precipitation runoff and glacial meltwater from the mountain drains to Cook Inlet via the Chakachatna River. Topographic relief is significant as the summit rises over 3,500 feet (1,067 meters) above a glacier in the north cirque in one-half mile (0.8 km). The mountain's toponym was officially adopted in 2005 by the United States Board on Geographic Names. [3] The mountain is named in association with Ch'akajabena Lake which in the Denaʼina language means "tail extends-out lake." [4]
According to the Köppen climate classification system, Ch'akajabena Mountain is located in a tundra climate zone with cold, snowy winters, and cool summers. [5] Weather systems coming off the North Pacific are forced upwards by the 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 three unnamed glaciers surrounding the peak.
Mount Foresta is an 11,000+ ft multi-peak massif located in Wrangell–St. Elias National Park, in the Saint Elias Mountains of Alaska in the United States. Rising high above the lower western margin of the Hubbard Glacier, the summit of Mount Foresta is just over nine miles (14 km) from tidewater at Disenchantment Bay, 12 mi (19 km) northwest of Mount Seattle, 14.5 mi (23 km) southeast of Mount Vancouver, and 46 mi (74 km) north of Yakutat.
Mount Watson is a 12,497-foot glaciated mountain summit located in the Fairweather Range of the Saint Elias Mountains, in southeast Alaska, United States. It ranks as the fifth-highest peak in the Fairweather Range. The peak is situated in Glacier Bay National Park, 2 mi (3 km) west of the Canada–United States border, and 7.16 mi (12 km) north of Mount Fairweather, which is the highest peak in the Fairweather Range. The mountain's name was officially adopted by the United States Board on Geographic Names in 1924 to commemorate David Thompson Watson (1844-1916), who was US Counsel to the 1903 Alaska Boundary Tribunal. The first ascent of the peak was made June 18, 1974, by Michael Allen, Walter Gove, Lawrence Dauelsberg, Alice Liska, and Donald Liska via the East Ridge. The first ascent of the North Face was made in April 1999 by Chris Trimble and Jim Earl. The months May through June offer the most favorable weather for climbing.
Castle Peak is a 10,190-foot (3,110-meter) mountain summit located in the Wrangell Mountains, in the U.S. state of Alaska. The peak is situated in Wrangell-St. Elias National Park and Preserve, 21 mi (34 km) northwest of McCarthy, and 9.3 mi (15 km) south of Mount Blackburn on the south margin of the Kuskulana Glacier valley. Precipitation runoff from the mountain drains into Kuskulana River and Lakina River which are both tributaries of the Chitina River. The peak's descriptive name was used by early prospectors as reported in 1901 by the US Geological Survey.
Marble Mountain is a 3,366-foot (1,026-meter) mountain summit located in the Fairweather Range of the Saint Elias Mountains, in southeast Alaska. The peak is situated in Glacier Bay National Park and Preserve at the entrance to Geikie Inlet, 68 mi (109 km) west-northwest of Juneau, and 10.7 mi (17 km) east-northeast of Blackthorn Peak. Although modest in elevation, relief is significant since the mountain rises up from tidewater in Shag Cove in less than one mile. The mountain's name was in local use as reported by the United States Geological Survey in 1951. Marble Mountain can be seen from Glacier Bay which is a popular destination for cruise ships. The months May through June offer the most favorable weather for viewing and climbing Marble Mountain.
Black Mountain is a prominent, 5,891-foot-high (1,796-meter) mountain summit located in the Alsek Ranges of the Saint Elias Mountains in southeast Alaska. The mountain is situated in Glacier Bay National Park and Preserve, 75 mi (121 km) northwest of Juneau, between the Riggs and McBride glaciers. The months May through June offer the most favorable weather for viewing or climbing Black Mountain. Weather permitting, Black Mountain can be seen from Muir Inlet of Glacier Bay, which is a popular destination for cruise ships.
Porphyry Mountain is a prominent 6,375-foot mountain summit located in the Wrangell Mountains, in the U.S. state of Alaska. The peak is situated in Wrangell-St. Elias National Park and Preserve, immediately southeast of Kennecott, 4 mi (6 km) northeast of McCarthy, and, 5 mi (8 km) northwest of Sourdough Peak. Precipitation runoff from the mountain drains into tributaries of the Nizina River, which in turn is part of the Copper River drainage basin. The peak is notable for a rock glacier on its north slope. The mountain was so named because it is largely composed of porphyry, which is a very hard igneous rock. The mountain's local name was reported in 1908 by the U.S. Geological Survey. On a clear day the summit of Porphyry Mountain offers views of Donoho Peak, Kennicott Glacier, and Mount Blackburn to the northwest, and Fireweed Mountain to the west.
Castle Mountain is a remote 8,620-foot (2,630-meter) mountain summit located at the southeastern edge of the Wrangell Mountains, in the U.S. state of Alaska. The peak is situated 35 mi (56 km) northeast of McCarthy at Skolai Pass in Wrangell-St. Elias National Park and Preserve. Although modest in elevation, relief is significant as the south face rises 4,000 feet above the terminus of the Russell Glacier in less than one mile. Precipitation runoff from the peak drains east via the White River, and west to the Nizina River via Skolai Creek. The mountain's descriptive name was reported in 1914 by the United States Geological Survey.
Maynard Mountain is a 4,137-foot (1,261 m) mountain summit located in the Chugach Mountains, in the U.S. state of Alaska. The peak is situated in Chugach National Forest, 3 mi (5 km) northwest of Whittier, Alaska, at the isthmus of the Kenai Peninsula, where the Chugach Mountains meet the Kenai Mountains. Nearby peaks include Bard Peak, 4.14 mi (7 km) to the south, and Begich Peak, 3.1 mi (5 km) to the west-northwest. Although modest in elevation, relief is significant since the eastern aspect of the mountain rises up from the tidewater of Prince William Sound's Passage Canal in approximately one mile. Maynard Mountain is often seen and photographed in the background behind Portage Lake, a popular tourist and recreation destination. The Anton Anderson Memorial Tunnel, often called the Whittier Tunnel, is a dual-use highway and railroad tunnel that passes through Maynard Mountain. With a length of 13,300 feet, it is the second-longest highway tunnel and longest combined rail and highway tunnel in North America.
Lindita Peak is a 7,910-foot-elevation (2,411-meter) mountain summit located 17 miles (27 km) north-northwest of Valdez in the U.S. state of Alaska. Lindita is the highest peak at the head of the Tazlina Glacier when viewed from the Glenn Highway at Mile 156 near the Tazlina Glacier Lodge. 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 2,400 feet (732 m) above the East Branch of the Columbia Glacier in 0.4 mile (0.64 km). The mountain's name Lindita, meaning "little beauty" in Spanish, was applied in 1955 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 first ascent of the summit was made on July 1, 1977, by Lawrence E. Nielsen, Halford Joiner, Tom Lamb, and Dr. Randall Travis via the northeast face and the north-facing knife-edged ridge from the Tazlina Glacier.
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.
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