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Geology of Arizona. The geology of Arizona began to form in the Precambrian. Igneous and metamorphic crystalline basement rock may have been much older, but was overwritten during the Yavapai and Mazatzal orogenies in the Proterozoic. The Grenville orogeny to the east caused Arizona to fill with sediments, shedding into a shallow sea.
Website. www .azgs .az .gov. The Arizona Geological Survey ( AZGS) was established by the Arizona Legislature to investigate and describe Arizona's geology and to educate and inform the public regarding its geologic setting. Each year since 1915, AZGS has released geologic maps, formal reports, and other geology-related publications.
Dells Granite showing spheroidal weathering. The Granite Dells is a geological feature north of Prescott, Arizona. The Dells consist of exposed bedrock and large boulders of granite that have eroded into an unusual lumpy, rippled appearance. Watson Lake and Willow Lake are small man-made reservoirs in this formation.
The Yavapai Geology Museum include three-dimensional models, photographs, and exhibits which allow park visitors to see and understand the complicated geologic story of the area. The museum building, the historic Yavapai Observation Station (built 1928), located one mile (1.6 km) east of Market Plaza, features expansive canyon views.
The Echo Cliffs are a prominent geological feature in northern Arizona. The cliffs stretch for 70 miles (110 km) and reach over 1000 feet (300 m) high. They are found in Coconino County in the Navajo Nation [1] about 20 miles (32 km) east of Grand Canyon National Park . U.S. Highway 89 runs parallel to the cliffs for 60 miles (97 km).
Website. www.arizonageologicsoc.org. The Arizona Geological Society ( AGS) is a non-profit scientific organization founded in 1948 whose purpose is to promote and encourage interest in the science of geology and in the geology of the State of Arizona. [2] The Society holds monthly meetings, and sponsors field trips and symposia.
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