- Stuart Range
The Stuart Range is a
mountain range in centralWashington ,USA . The range lies on the eastern side of theCascade Range . To the north isThe Enchantments , a well-known backpacking destination. To the south isIngalls Creek and theWenatchee Mountains .Partial list of peaks:
*Mount Stuart - 9,415' (2870m)
* Dragontail Peak - 8,840' (2694m)
* Colchuck Peak - 8,705' (2653m)
* Cannon Mountain - 8,638' (2633m)
* Sherpa Peak - 8,605' (2623m)
* Enchantment Peak - 8,520' (2597m)
* Witches Tower - 8,520' (2597m)
* Argonaut Peak - 8,453' (2576m)
* Little Annapurna - 8,440' (2573m)
* McClellan Peak - 8,364' (2549m)Geology
The Mount Stuart
batholith underlies the Stuart Range and the nearbyWenatchee Mountains . The batholith is about 13 by 16 miles in extent. Two plutonic masses are separated by a thin screen of ChiwaukumSchist and rocks of the Ingalls Complex. The more-easternpluton is 93 million years old, while the more-western rock mass is between 83 and 86 million years old. Exposed rock tends to bequartz diorite andgranodiorite . [cite book | last = Beckey | first = Fred
authorlink =Fred Beckey | coauthors =
title = Cascade Alpine Guide: Climbing and High Routes - 1: Columbia River to Stevens Pass
publisher = The Mountaineers Books | date = 2003
location = Seattle, WA, USA | pages = 236 | url = | doi = | id =
isbn = 9780898865776 ]The range sits near a convergent plate boundary where one plate overrides another. In Western Washington, the
North American plate overrides theJuan de Fuca plate , resulting in both volcanic and seismic activity. This convergence has been ongoing for over 200 million years. Continuing uplift and erosion has exposed the underlying granite batholith, making for one of the more spectacular mountain ranges in Washington.References
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