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Neacola Mountains

Mountain range in Alaska


Summary

Mountain range in Alaska

FieldValue
nameNeacola Mountains
photoNeacola1.jpg
photo_captionBlockade Glacier in the Neacola Mountains
etymologyNamed for the Neacola River
highestMount Neacola
elevation_ft9426
elevation_ref
coordinates
countryUnited States
stateAlaska
parentAleutian Range
borders_on
length_mi88
length_orientationNorth-South
length_ref
width_mi157
width_orientationEast-West
width_ref
range_coordinates
range_coordinates_ref
mapUSA Alaska
map_captionLocation of Neacola Mountains

The Neacola Mountains are the northernmost subrange of the Aleutian Range in the U.S. state of Alaska. The range is named for the Neacola River which bounds it to the north and drains the highest and most rugged peaks of the group. They are bordered on the southeast by the Chigmit Mountains, another subrange of the Aleutian Range, on the northeast by the Tordrillo Mountains, and on the west and southwest by the lakes and lowlands of Lake Clark National Park and Preserve. The highest peak is Mount Neacola (also known as "Neacola Peak"), 9,426 feet (2,873 m) although the name is not officially recognized. These mountains have not seen extensive exploration, due to their remoteness, typically poor weather, and lack of truly high peaks. However they are rugged and offer many climbing possibilities of an exploratory nature. Noted climber Fred Beckey visited the range in the early 1970s; in 1991, when he was "spiritual leader" of the expedition which made the first ascent of Mount Neacola; and again in 2004. Other recorded climbing visits occurred in 1979 and 1995.

Sources

  • American Alpine Journal, 1980, 1992, 1996, 2005.
  • {{cite book | title = Alaska: a climbing guide

References

References

  1. {{cite peakbagger
  2. {{cite peakbagger
  3. {{cite gnis
  4. The USGS GNIS does not contain an entry for this peak.
Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

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