Bonanza Peak (Alaska)

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Bonanza Peak
Summit of Bonanza Peak in Alaska.jpg
South aspect of Bonanza Peak
Highest point
Elevation 6,983 ft (2,128 m) [1]
Prominence 1,583 ft (482 m) [1]
Parent peak Peak 12454
Isolation 4.94 mi (7.95 km) [2]
Coordinates 61°31′14″N142°50′06″W / 61.5205763°N 142.8350518°W / 61.5205763; -142.8350518 [3]
Geography
Relief map of USA Alaska.png
Red triangle with thick white border.svg
Bonanza Peak
Location of Bonanza Peak in Alaska
Location Wrangell-St. Elias National Park
Valdez-Cordova Borough
Alaska, United States
Parent range Wrangell Mountains
Topo map USGS McCarthy C-5
Geology
Type of rock Limestone, Greenstone

Bonanza Peak is a 6,983-foot (2,128 meter) mountain summit located in the Wrangell Mountains, in the U.S. state of Alaska. [3] The peak was notable for its abundance of copper deposits which were mined from 1909 through 1938. The peak is situated in Wrangell-St. Elias National Park and Preserve, immediately northeast of Kennecott, 7 mi (11 km) northeast of McCarthy, 3.46 mi (6 km) north of Porphyry Mountain, and 5.2 mi (8 km) southeast of Donoho Peak. The confluence of the Kennicott and Root Glaciers lies below the mountain's west slope. Precipitation runoff from the mountain drains into tributaries of the Nizina River, which in turn is part of the Copper River drainage basin. The mountain's local name was reported in 1914 by the U.S. Geological Survey. On a clear day the summit of Bonanza Peak offers views of Sourdough Peak, Mount Blackburn, and Fireweed Mountain.

Contents

History

Bonanza Peak hosted five mines: Bonanza, Jumbo, Mother Lode, Erie, and Glacier. The Bonanza ore body was discovered August 1900 by prospectors "Tarantula" Jack Smith and Clarence L. Warner. [4] Bonanza Mine was located on a ridge south of the summit, and was in the early 1900s, confirmed by Stephen Birch as the richest known concentration of copper in the world. [5] Glacier Mine, which is really an ore extension of the Bonanza, was an open-pit mine and was only mined during the summer. Jumbo Mine was in the west cirque below the summit. The Mother Lode mine was located in a cirque on the east side of the summit. The Erie mine was perched on the northwest slope above the Root Glacier. The Bonanza, Jumbo, Mother Lode and Erie mines were connected by tunnels. From 1909 until 1938, the mines produced over 4.6 million tons of ore containing 1.183 billion pounds of copper mainly from the Bonanza, Jumbo and Mother Lode, as well as several million ounces of silver. [5] :260 The Kennecott operations reported gross revenues above $200 million and a net profit greater than $100 million. [6]

Present-day visitors may hike to the abandoned Bonanza, Jumbo, and Erie mines, all of which are strenuous full-day hikes, with Erie Mine being a somewhat terrifying scramble along cliffs overlooking the Stairway Icefall.

Geology

Bonanza Peak is part of the Wrangellia Terrane. Copper deposits are found at the disconformity between the Upper Triassic Chitistone limestone and underlying Permian Nikolai greenstone. [7] Copper is found as polymetallic replacement deposits in the fault planes, fractures and joints. Minerals include chalcocite, bornite and chalcopyrite, with associated malachite, azurite, and cupriteNative copper can also be found in the greenstone. [4] :77 The deposits were mined for their spectacularly high-grade copper ore which exceeded 70 percent.

Climate

Based on the Köppen climate classification, Bonanza Peak is located in a subarctic climate zone with long, cold, snowy winters, and cool summers. [8] Weather systems coming off the Gulf of Alaska are forced upwards by the Wrangell Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The months May through June offer the most favorable weather for viewing and climbing.

See also

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<span class="mw-page-title-main">Regal Mountain</span>

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In an effort to thwart statehood and Alaskan home rule from Washington D.C., the Alaska Syndicate, was formed in 1906 by J. P. Morgan and Simon Guggenheim. The Syndicate purchased the Kennicott-Bonanza copper mine and had majority control of the Alaskan steamship and rail transportation. The syndicate also was in charge of a large part of the salmon industry.

<span class="mw-page-title-main">Sourdough Peak</span> Summit in the Wrangell Mountains, Alaska, USA

Sourdough Peak is a 6,201-foot mountain summit located at the southern edge of the Wrangell Mountains, in the U.S. state of Alaska. The peak is situated in Wrangell-St. Elias National Park and Preserve, 7 mi (11 km) east-southeast of McCarthy, on the north bank of the Nizina River. The peak is notable for a rock glacier on its south slope. The peak's name was used by early prospectors as reported in 1908 by the USGS. A "sourdough" is defined as an experienced prospector or an old-timer in the western US or Canada, because they always carried sourdough starter with them. Sourdough Peak's nearest higher neighbor is Porphyry Mountain, 5.1 miles to the northwest.

<span class="mw-page-title-main">Donoho Peak</span> Mountain in Alaska

Donoho Peak is a 6,696-foot-elevation 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, 6 mi (10 km) north-northwest of Kennecott, and 9 mi (14 km) north of McCarthy, at the confluence of the Kennicott Glacier and Root Glacier. The peak's name was reported in 1931 by the United States Geological Survey. The mountain lies within the Copper River drainage basin. Bears frequent the Donoho Peak and Donoho Lakes area. An ascent of the mountain involves 14 miles round-trip from Kennecott to the summit, including crossing the Root Glacier and gully scramble via the south aspect of the mountain. Ruins of the Regal Mine remain at an elevation of 5,440 feet on the south slope of the mountain. Only small amounts of copper ore were ever produced, however. On a clear day the summit of Donoho Peak offers views of Mount Blackburn to the northwest and the Stairway Icefall on Regal Mountain to the north-northeast.

<span class="mw-page-title-main">Fireweed Mountain</span> Mountain summit in Alaska, U.S.

Fireweed Mountain is a prominent 6,956-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 west of the terminus of the Kennicott Glacier, and 5 mi (8 km) west-northwest of McCarthy. Precipitation runoff from the eight-mile-long by five-mile-wide mountain drains into tributaries of the Chitina River, which in turn is part of the Copper River drainage basin. The mountain's name was given in the 1920s by Molly Gilmore, a lifelong resident of the McCarthy area, who at age 17, named the mountain for the abundance of fireweed which grew on the mountain following forest fires. Although fireweed is the most common and well-known flower in Alaska, it is not commemorated on any other Alaskan mountain. The mountain's name was officially adopted in 1966 by the U.S. Board on Geographic Names. On a clear day the summit of Fireweed Mountain offers views of Mount Blackburn to the northwest, and Regal Mountain to the northeast.

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<span class="mw-page-title-main">Williams Peak (Alaska)</span> Mountain in Alaska

Williams Peak is a 7,431-foot mountain summit located at the western edge of the Saint Elias Mountains, in the U.S. state of Alaska. The peak is situated in Wrangell-St. Elias National Park and Preserve, 15 mi (24 km) east-southeast of McCarthy, and 4 mi (6 km) west-southwest of Joshua Green Peak in the Dan Creek area. Precipitation runoff from the mountain drains into tributaries of the Nizina River, which in turn is part of the Copper River drainage basin.

<span class="mw-page-title-main">Chitistone Mountain</span> Mountain in Alaska

Chitistone Mountain is a 6,844-foot (2,086-meter) mountain summit located at the southeastern edge of the Wrangell Mountains, in the U.S. state of Alaska. The peak is situated in Wrangell-St. Elias National Park and Preserve, 15 mi (24 km) east-northeast of McCarthy, 13 mi (21 km) east of Bonanza Peak, and 12 mi (19 km) north of Williams Peak, where it is wedged between the confluence of the Nizina River and Chitistone River.

<span class="mw-page-title-main">Castle Mountain (Alaska)</span> Mountain summit in the state of Alaska

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.

<span class="mw-page-title-main">Pyramid Peak (Alaska)</span> Mountain in Alaska

Pyramid Peak is an 8,875-foot (2,705-meter) mountain summit located at the western edge of the Saint Elias Mountains, in the U.S. state of Alaska. The peak is situated in Wrangell-St. Elias National Park and Preserve, 22 mi (35 km) southeast of McCarthy, 7 mi (11 km) southeast of Williams Peak, and 6 mi (10 km) south-southeast of Joshua Green Peak. The peak's descriptive local name was reported in 1908 by the United States Geological Survey. Precipitation runoff from the mountain drains into tributaries of the Nizina River, which in turn is part of the Copper River drainage basin.

References

  1. 1 2 "Bonanza Peak, Alaska". Peakbagger.com. Retrieved 2020-02-14.
  2. Bonanza Peak, listsofjohn.com
  3. 1 2 "Bonanza Peak". Geographic Names Information System . United States Geological Survey, United States Department of the Interior . Retrieved 2020-02-14.
  4. 1 2 Fred H. Moffit; Stephen R. Capps (1911). Geology and Mineral Resources of the Nizina District, Alaska, USGS Bulletin 448. U.S. Government Printing Office. p. 76.
  5. 1 2 Charles Caldwell Hawley (2014). A Kennecott Story. The University of Utah Press.
  6. Alfredo O. Quinn (1995). Iron Rails to Alaskan Copper. D'Aloguin Publishing Co. p. 175.
  7. Geologic Studies in Alaska by the U.S. Geological Survey, 1995. Robert P. Eppinger,Stephen J. Sutley, and John B. McHugh. Page 19-22.
  8. Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11. ISSN   1027-5606.