Atna Peaks
The mountain's main summit is 13,860 feet (4,225 m), making it the second-highest thirteener (a peak between 13,000 and 13,999 feet in elevation) in Alaska. The second summit is located about 0.6 miles (0.97 km) to the east, reaching over 13,600 feet (4,100 m), and another named summit, 13,280 ft (4,048 m) Parka Peak, is about 1.6 miles (2.6 km) further east across a glacier-covered saddle. The steep rocky south faces of these three peaks form part of the cirque of the Kennicott Glacier, which flows southeast over 20 mi (32 km) to just above the town of McCarthy.
Atna Peaks was named in 1965 by the first ascent party from the Mountaineering Club of Alaska, because the "peaks are at the edge of the Copper River drainage and the old Indian name for that river was Atna."
Gallery
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Looking north at Parka Peak centered with Atna Peaks to left reflected in a lake near Donoho Peak
See also
References
- Richter, Donald H.; Danny S. Rosenkrans; Margaret J. Steigerwald (1995). Guide to the Volcanoes of the Western Wrangell Mountains, Alaska. USGS Bulletin 2072.
- Winkler, Gary R. (2000). A Geologic Guide to Wrangell—Saint Elias National Park and Preserve, Alaska: A Tectonic Collage of Northbound Terranes. USGS Professional Paper 1616. ISBN 0-607-92676-7.
- Richter, Donald H.; Cindi C. Preller; Keith A. Labay; Nora B. Shew (2006). Geologic Map of the Wrangell-Saint Elias National Park and Preserve, Alaska. USGS Scientific Investigations Map 2877.
- ^ "Club Activities: Mountaineering Club of Alaska" (PDF). American Alpine Journal. 15 (40). American Alpine Club: 225. 1966. Archived from the original (PDF) on September 27, 2007.
- ^ "USGS Geographic Names Information System: Atna Peaks". Retrieved 2007-03-07.