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Research about Gila County, Arizona

Source-linked reports with geographic coverage including Gila County, Arizona.

12 recordsLinked to original sources

Hydrology and geochemistry of aquifer and stream contamination related to acidic water in Pinal Creek basin near Globe, Arizona

Hydrologic and geochemical research has identified and characterized the physical and chemical processes that control the evolution and movement of metal contaminants in ground water beneath Miami Wash and lower Pinal Creek. The dissolution of calcite in the alluvial aquifer has slowed and neutralized part of the acidic plume, and the sorption of some metals such as nickel and copper to other solids in the subsurface has lowered concentrations of these metals in the ground water.

Arizona

Hydrogeology and hydrologic system of Pinal Creek Basin, Gila County, Arizona

Acidic water that contains elevated concentrations of metals has contaminated a stream and alluvial aquifer in a mining district near Globe, Arizona. The contaminated aquifer is a narrow layer of unconsolidated alluvium along Miami Wash and Pinal Creek. The alluvium overlies basin fill, which extends throughout most of the Pinal Creek basin. The alluvium and basin fill compose the primary aquifer in the basin. Horizontal hydraulic con- ductivities were estimated at about 200 meters per day in the alluvium, and average linear ground- water flow velocities are about 5 meters per day. Water levels in the aquifer respond rapidly to periods of extended runoff in the basin and variable rates of ground-water pumping. Fluctuations of as much as 2.5 meters in 6 months have been measured. Ground-water levels were near record highs during spring 1985 and declined as much as 13 meters by spring 1989. Measured hydraulic gradients indicate that flow is generally upward from the basin fill to the alluvium. From 1980 to 1984, seepage of 155 liters per second from Webster Lake and 279 liters per second streamflow infiltration were estimated to be the two largest sources of inflow to the regional aquifer. Major outflows from the aquifer were 166 liters per second of pumpage and 240 liters per second of natural ground-water discharge to Pinal Creek.

Arizona

Aeromagnetic map of the Hells Gate Roadless Area, Gila County, Arizona

The Hells Gate Roadless Area comprises about 31, 200 acres in the northern part of the Tonto National Forest. It lies beneath the Mogollon Rim between the communities of Payson and Young. The area is roughly a 4 by 15 mi strip along the deeply incised segment of Tonto Creek and along a 2 mi segment of Haigler Creek at its intersection with Tonto Creek. Elevations range from 2,960 ft in the lower Tonto Creek gorge near Gisela, in the southeastern part of the area, to 6,200 ft in the Green Valley Hills, in the northern part of the area. Local relief in the deep canyon of Tonto Creek is commonly greater than 1,000 ft. Hells Gate is the geographic name for the canyon at the confluence of Tonto Creek and Haigler Creek. Foot trails cross Tonto Creek at Hells Gate and between Houston Pocket and McDonald Pocket. Descent into Tonto Creek elsewhere is extremely difficult. The Hells Gate area lies in the central part of the Tonto Basin, which consists of Tonto Creek and tributaries draining the Mogollon escarpment and the northern Sierra Ancha. These streams dissect a table land which is the unconformable surface at the base of the Paleozoic section and the Mogollon Rim. This tableland is a part of the Colorado Plateau margin, which has been slightly structurally disrupted by late Cenozoic faulting and from which most of the Middle Proterozoic and Paleozoic strata have been stripped by subsequent erosion. Early Proterozoic rocks constitute about ninety percent of the exposed rocks in the roadless area and are composed of granite, granophyre, and intrusive and extrusive rhyolite (Conway, 1983).

Arizona

Map showing ground-water conditions in the Tonto basin area, Gila County, Arizona; 1978-79

The Tonto basin area includes about 955 mi 2 in central Arizona. The area is bounded on the north by the Mogollon Rim, on the east by the Sierra Ancha Mountains, on the west by the Mazatzal Mountains, and on the south by Theodore Roosevelt Lake. The area is drained by Tonto Creek, which flows north to south and discharges into Theodore Roosevelt Lake. Because the Tonta basin area is entirely within the Tonto National Forest, only about 3 percent of the land is privately owned and, for the most part, wells inventoried were on private land. Only selected wells are shown on the map because of the high well density on the private land.

Arizona

Map showing mineral resource potential of the Sierra Ancha Wilderness and Salome Study Area, Gila County, Arizona

The Wilderness Act (Public Law 88-577, Sept. 3, 1964) and certain related Acts require the Geological Survey and the Bureau of Mines to survey certain areas on Federal lands to determine their mineral-resource potential. Results must be made available to the public and be submitted to the Administration and the Congress. These maps and reports present the results of a geologic and mineral survey of the Sierra Ancha Wilderness and Salome Study Area, Gila County, Arizona.

Arizona