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Geologic map of the Adams Mesa Quadrangle, Maricopa County, Arizona

S.J. Skotnicki, R.S. Leighty

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Abstract

The Adams Mesa quadrangle straddles the boundary between Proterozoic granitic and mid-Tertiary rocks of the Transition Zone, and overlapping late Tertiary basin-fill sediments of the Lower Verde River Valley. The area is dominated by Sycamore Creek, which cuts diagonally across the quadrangle from northeast to southwest and defines the base level for most of the area (see Figures 1 and 2).

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What this paper is about

The Adams Mesa quadrangle straddles the boundary between Proterozoic granitic and mid-Tertiary rocks of the Transition Zone, and overlapping late Tertiary basin-fill sediments of the Lower Verde River Valley. The area is dominated by Sycamore Creek, which cuts diagonally across the quadrangle from northeast to southwest and defines the base level for most of the area (see Figures 1 and 2).

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Available abstract

The Adams Mesa quadrangle straddles the boundary between Proterozoic granitic and mid-Tertiary rocks of the Transition Zone, and overlapping late Tertiary basin-fill sediments of the Lower Verde River Valley. The area is dominated by Sycamore Creek, which cuts diagonally across the quadrangle from northeast to southwest and defines the base level for most of the area (see Figures 1 and 2).

Key concepts: Quadrangle, Geology, Proterozoic, Archaeology, Geomorphology, Structural basin, Excavation, Geochemistry

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