New Perspectives on Rio Grande Rift Basins: From Tectonics to Groundwater

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Geological Society of America

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A fault scarp is a small step-like offset of the ground surface in which one side of a fault has shifted vertically in relation to the other.

The Gilman Conglomerate is a geologic formation in northern New Mexico dating to the Oligocene epoch.

The Chamita Formation is a geologic formation in north-central New Mexico. It preserves fossils dating back to the Neogene period.

The El Rito Formation is a geologic formation in New Mexico dating to the Eocene epoch.

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