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Examples
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Pacific tree species are more numerous than in the Idaho Batholith (16) and are never dominant in the Middle Rockies (17).
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Most of central Idaho and the Salmon River Mountains are formed by granitic intrusions that collectively make up the Idaho Batholith, with altitudes ranging from 3,000 to 7,000 ft (900 to 2,130 m).
Middle Rocky Mountain Steppe - Coniferous Forest - Alpine Meadow Province (Bailey) 2009
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Here, tailings cover a valley floor in the Northern Rockies (15); placer mining tailings are more common in the Idaho Batholith (16), particulary in Ecoregion 16i.
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Pacific tree species are more numerous than in the Idaho Batholith (16) and are never dominant in the Middle Rockies (17).
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The wet, severely exposed, glaciated High Idaho Batholith contains jagged peaks, tarns, and rockland.
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Like the Cascades (4), but unlike the Northern Rockies (15) and the Idaho Batholith (16), the Blue Mountains (11) is mostly volcanic in origin.
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Batholith: large plutonic masses of intrusive rock with more than 100 square kilometers of surface area.
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Structures in the Kurupung Batholith, please visit the following link:
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Map of airborne magnetic data from the Kurupung Batholith overlain with interpreted structures (black lines) that extend between the bounding shear zones of the batholith.
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The mineralized zone at Aricheng Epsilon (labelled in red and whose assay results are reported in this press release) is located near the western margin of an extensive magnetic low in the Aricheng West-Aricheng Alpha area of the Kurupung Batholith.
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