The maps, reports, and other information and content on this website are provided as a public service for informational purposes only. Elevation Change from Base: 4,463 feet Vegetation at Highest Elevations: pine forests The Galiuro Mountains are a block-fault range consisting of two high parallel ridges separated by two valleys, one sloping to the north and the other to the south.

Accuracy is not guaranteed, and the information contained or linked on this website should not be relied on except as general information. The University makes no warranties or representations of any kind, and specifically disclaims all warranties including the warranty of merchantability and fitness for a particular purpose. Some of these features are common throughout this southern part of the Santa Catalina Mountains. Limestone formed in the sea was metamorphosed by mafic intrusions. The Galiuro Mountains are a north-northwest-trending, elongate range a­ long the eastern edge of the San Pedro Valley and are formed mostly of gently east-dipping Tertiary volcanic rocks. Geology, landscape development, adventure and foreign travel, philosophical and scientific musings, photography and earthly explorations. Galiuro Mountains. The University makes no warranties or representations of any kind, and specifically disclaims all warranties including the warranty of merchantability and fitness for a particular purpose. Geology Figure 1 shows the general geology of the Copper Creek area. The maps, reports, and other information and content on this website are provided as a public service for informational purposes only.

Basic Information. Geologic Map of Catalina Core Complex and San Pedro Trough. High Point: Bassett Peak, 7,663 feet.

Accuracy is not guaranteed, and the information contained or linked on this website should not be relied on except as general information. ARIZONA GEOLOGY REFERENCES: G . Pre … Users are responsible for verification of all facts and information to their own satisfaction. 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. Others occur in many other parts of the American Southwest. A Guide to the Geology of Sabino Canyon and the Catalina Highway. Friday, February 17, 2012. Users are responsible for verification of all facts and information to their own satisfaction. Basic Information.

Neogene erosion along the southwestern flank of the Galiuro Mountains in the Basin and Range province of southeastern Arizona has exposed multiple strands of a mid-Tertiary low-angle normal-fault system that offsets Oligocene-Miocene and older strata. In the near middle-ground, gently tilted Miocene-age interbedded sandstones and conglomerates exposed near Hookers Hot Springs in the Galiuro Mountains of southeastern Arizona. Galiuro Mountains.

Galiuro Mountains *Cox, L.J., 1995, Geologic map of the southern Galiuro Mountains in Pinal, Graham, and Cochise Counties, Arizona: USGS …

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