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The butte lies on the west bank of the south-flowing Colorado River. The outfall from the Little Colorado River, draining from the Painted Desert to the east and southeast, is about two miles upstream. Temple Butte is 5,308 feet (1,618 m) in elevation. It is the historical site of some wreckage of the 1956 Grand Canyon mid-air collision.
Description. Camel Butte is situated 2.75 miles (4.43 km) southeast of the Monument Valley visitor center on Navajo Nation land. Precipitation runoff from this butte's slopes drains into Gypsum Creek which is a tributary of the San Juan River. Topographic relief is significant as the summit rises 550 feet (168 meters) above the surrounding ...
Tempe Butte (O'odham: ʼOidbaḍ Doʼag) is the official name of an andesite butte of volcanic origin, located partially on Arizona State University's Tempe campus in Tempe, Arizona. It is often referred to by locals as A Mountain , after the 60-foot-tall (18 m) gold-painted letter 'A' near the top.
Approximately 3.6 miles west-southwest of the peak on US Route 60 is the Jones Water campground. [4] Jones Water is a special developed campground with some small private tent sites along a mature and lush riparian area at an elevation of 4,000 ft (1,200 m). Jones Water is a free primitive campground and offers only basic amenities. [citation ...
The upper and lower contacts of the Temple Butte Formation are major unconformities. Within the Grand Canyon region, its base is a major unconformity within the Paleozoic rock record. The time represented by this unconfomity spans about 100 million years, including part of Late Cambrian , all of Ordovician and Silurian , and most of Early and ...
The West Silver Bell Mountains are a small 10 mile (16 km) long mountain range of south-central Arizona, United States. The range lies in the north-central arid Sonoran Desert; the Madrean Sky Islands region of southeast Arizona, around Tucson is adjacent to the southeast. The range lies mostly in Pima County with only the northernmost end ...
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