Geologic map of the Adams Mesa Quadrangle, Maricopa County, Arizona
S.J. Skotnicki, R.S. Leighty
Abstract
S.J. Skotnicki, R.S. Leighty
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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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