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The Ives flow is a young tholeiitic basalt flow in the southernmost Pinacate. Seen here is a broad tumulus whose brittle crust fractured when it arched upward. The Sierra Blanca is in the background.
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The Ives flow is a young tholeiitic basalt flow in the southernmost Pinacate. Seen here is a broad tumulus whose brittle crust fractured when it arched upward. The Sierra Blanca is in the background.
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