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95 FOSSAE HISTORY STAGES OTHER STRUCTURES SYSTEM 70 100 2 5 Fault or graben Bar and ball on downthrown side of fault; dotted where buried 16 Scarp Line marks top of slope; barb points downslope. Forms contact in places 40 or less 65 105 Contact Dashed where approximately located or gradational NO. CRATERS LARGER THAN 2, 5, AND 16 KM DIAMETER PER 1,000,000 KM2 Mare-type (wrinkle) ridge Symbol on ridge crest; dashed where buried Subdued mare-type (wrinkle) ridge.
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Valles FAQ
Geologic Setting The Winslow quadrangle is characterized by gently dip- ping Paleozoic and Mesozoic strata, which dip 1° to 2° north- eastward in the southwestern part of the quadrangle (sheet 1) and become nearly flat-lying in the northeastern part of the quadrangle (sheet 2).
Large rocks like these are transported in massive debris flows down steep canyons, then spread out along the mountain front during times of rare, intense rains. In the mountains, balanced boulders form from certain rock types, such as granite and thickly-layered sandstone or volcanic ash.
Early in the Triassic Period, the shallow seas of the Paleozoic began to recede and southern Arizona entered a period of uplift, resulting in the formation of mountains. Climates were arid, with strong seasonal temperature fluctuations and enormous monsoons that weathered the terrain.
The landscape of this plateau is composed of remarkable geologic features: the towering, glaciated peaks of San Francisco Mountain, underground lava tubes and blowholes; meteor-blasted Barringer Crater, and cinder cones and lava flows of the San Francisco volcanic field.
The U.S. Geological Survey (USGS) is the nation's largest water, earth, and biological science and civilian mapping agency. It collects, monitors, analyzes, and provides scientific understanding of natural resource conditions, issues, and problems.
A generalized view illustrating the approximate distribution of major rock types in Arizona: silt, sand & gravel (aggregate), granite, schist & gneiss, limestone, sandstone, basalt, and mixed volcanic rocks.
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