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Pages in category "Bodies of water of Yavapai County, Arizona" The following 2 pages are in this category, out of 2 total. This list may not reflect recent changes. C.
Montezuma Well (Yavapai: ʼHakthkyayva), a detached unit of Montezuma Castle National Monument, [1] is a natural limestone sinkhole near the town of Lake Montezuma, Arizona, through which some 1,500,000 US gallons (5,700,000 L; 1,200,000 imp gal) of water emerge each day from an underground spring. It is located about 11 miles (18 km) northeast ...
Lake Montezuma is a census-designated place (CDP) in Yavapai County in the U.S. state of Arizona. The population was 5,111 at the 2020 census. The CDP includes the communities of Rimrock and McGuireville. Located along Interstate 17, it is 20 miles (32 km) south of Sedona and 8 miles (13 km) north of Camp Verde in central Arizona's Verde Valley.
Peeples Valley (Yavapai: Wachinivo) is a census-designated place (CDP) in Yavapai County, Arizona, United States.The population was 374 at the 2000 census.. Peeples Valley is named for prospector A. H. Peeples, who was the leader of the group that discovered Rich Hill, a gold deposit at Weaver, Arizona, in 1863.
The Verde Valley (Yavapai: Matkʼamvaha; Spanish: Valle Verde) is a valley in central Arizona in the United States. The Verde River runs through it. The Verde River is one of Arizona's last free-flowing river systems. It provides crucial habitat for fish and wildlife, fresh water for local agricultural production, recreational opportunities for ...
According to the United States Census Bureau, Clarkdale has a total area of 7.5 square miles (19 km 2), of which 7.3 square miles (19 km 2) is land and 0.2 square miles (0.5 km 2) is water. Clarkdale is at 3,545 feet (1,081 m) above sea level at the confluence of Bitter Creek and the Verde River in Yavapai County, northern Arizona.
Fossil Springs, the source of about 80 percent of the water in Fossil Creek, issues from several vents in close proximity to one another at the base of the Mogollon Rim. [10] The rim is the southern edge of the Colorado Plateau. Water percolating through limestone layers in the rim becomes laden with dissolved carbon dioxide and calcium ...
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