Snake River Plain
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UNEXPLORED
The Snake River Plain is a broad, arc-shaped volcanic and sedimentary lowland in southern Idaho, formed by the movement of the North American Plate over the Yellowstone hotspot and now a major agricultural and geological region.
Referenced by (3)
| Subject (surface form when different) | Predicate |
|---|---|
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Owyhee Desert
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adjacentTo |
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Snake River
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hasNotableFeature |
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Intermontane Plateaus
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includes |