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Agua Dulce Mountains
The Agua Dulce Mountains are a mountain range in the north-central Sonoran Desert of southwestern Arizona. The range is located in the extreme southwestern portion of Pima County, Arizona, immediately north of the international boundary with Mexico and about 30 miles southwest of Ajo, Arizona. The range has three main sections that total about 15 miles in length and about nine miles in width. The range is located entirely within the Cabeza Prieta National Wildlife Refuge. The highpoint of the range is 2,852 feet (869 meters) above sea level and is located at 32°01'32"N, 113°08'44"W (NAD 1983 datum). The summit is unnamed, but is marked on U.S. Geological Survey (USGS) maps for the "Quitovaquita" benchmark that was placed on the summit in 1920. The original surveyed height was 2,850 feet above sea level, but recent datum adjustments calculate the summit to be two feet higher.〔National Geodetic Survey Datasheet, DA1412, Quitovaquita BM.〕〔U.S. Geological Survey. 1964. Agua Dulce Mts. Quadrangle, Arizona. 15-minute Series (Topographic). N3200-W113/15. Washington, D.C.〕
The name of the range has been in use for at least 100 years, though it has been called the "Sierra del Ojo" and the "Sonoyta Mountains" on some older maps. A map created by the U.S. Army Corps of Engineers around 1920 labeled the range the "Quitovaquita Mountains." This is in reference to Quitobaquito Springs, which lie approximately nine miles southeast of the range in what are now called the Quitobaquito Hills. The Quitobaquito Hills, however, do not share a connection with the Agua Dulce Mountains. "Agua Dulce" means "sweet water" in Spanish and refers to pools of non-saline water on the Sonoyta River several miles to the south in Mexico. These pools are in contrast to "Agua Salada," which is located further downstream on the river and yields only highly mineralized and brackish water. The range also contains a small spring on its southern slope that also bears the name Agua Dulce, though it is likely that the range is named for the pools on the river rather than the spring, since the pools played prominently in the history of the area whereas the spring is small and well away from the historical Sonoyta River travel corridor.〔Broyles, Bill, Luke Evans, Richard Stephen Felger, and Gary Nabhan. 2007. Our Grand Desert: A Gazetteer for Northwestern Sonora, Southwestern Arizona, and Northeastern Baja California. In Dry Borders: Great Natural Reserves of the Sonoran Desert, Broyles, B. and R. Felger, editors. University of Utah Press.〕
The range is home to a number of abandoned mines, most notably the Papago Mine and the Legal Tender Mine, which were worked in the late 19th and early 20th centuries. Papago Well was drilled nearby during the same period to provide water to the mines.〔Bryan, Kirk. 1925. The Papago Country, Arizona: A Geographic, Geologic, and Hydrologic Reconnaissance with a Guide to Desert Watering Places. Water Supply Paper No. 499. United States Geological Survey. Washington, D.C.〕 Later the well was used to provide water to cattle that grazed in the area, and now the windmill pumps water to a guzzler for wildlife. The Davidson Canyon area and the associated bajada to the south of the range contain the northernmost populations of senita cactus (''Pachycereus schottii''). This columnar cactus is very common further south in Mexico, but in the United States it is restricted to small areas of Organ Pipe Cactus National Monument and this isolated population in the Cabeza Prieta National Wildlife Refuge.
== References ==
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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