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Big Jim Mountain Lakes

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and other diorites. Mineral boundaries are sharp along Big Jim Mountain except between these two matrix subdomains, which are not immediately distinguishable.
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is a short distance on the opposite side of Icicle Ridge. The lakes are located approximately 2.5 miles from a trail junction area called "The Badlands".
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the first half and boulders added in the second half of the trajectory. The west hills of Big Jim Mountain surrounding Lake Augusta grow
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Assimilation of peridotite in zoned calc-alkaline plutonic complexes: evidence from the Big Jim complex, Washington Cascades
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is 93 million years old, while the more-western rock mass is between 83 and 86 million years old.
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Cascade Alpine Guide: Climbing and High Routes - 1: Columbia River to Stevens Pass
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U.S. Geological Survey Geographic Names Information System: Big Jim Mountain Lakes
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Revised metamorphic history for the Chiwaukum Schist, North Cascades, Washington
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The Big Jim Mountain Lakes are located on the northern skirt of
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Contributions to Mineralogy and Petrology, 94(1), 12-28.
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with influence from the intrusions originated from the
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and rocks of the Ingalls Complex. The more-eastern
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Index

Location of Eightmile Lake in Washington, USA.
Location of Eightmile Lake in Washington, USA.
Chelan County
Washington
United States
47°39′58″N 120°49′24″W / 47.6662365°N 120.8233391°W / 47.6662365; -120.8233391
Primary outflows
Basin
lakes
Big Jim Mountain
Icicle Ridge
Chelan County
Washington
Lake Augusta
Big Jim Mountain
intrusive rock
quartz-dolerite
granodiorite
Mount Stuart Batholith
Wenatchee Mountains
Schist
pluton
loam
tonalite
granodiorite
pyroxenites
gabbro
amphibolites
List of lakes of the Alpine Lakes Wilderness
Northwest Fishing Guide

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