Double Crater
In today's world, Double Crater has become a topic of great interest and relevance in different areas. The growing importance of Double Crater has sparked a debate in society, generating growing interest in understanding its implications. From diverse perspectives, Double Crater has become an object of study and research, giving rise to numerous analyzes and reflections that seek to understand its impact and scope. In this article, we will explore the different facets of Double Crater, examining its influence in different contexts and its role in contemporary society.
| Double Crater | |
|---|---|
 Double Crater, facing southeast. | |
| Highest point | |
| Elevation | 8,007 ft (2,441 m) |
| Prominence | 944 ft (288 m) |
| Coordinates | 35°20′34″N 111°26′52″W / 35.3427864°N 111.4476552°W |
| Geography | |
  Double Crater | |
| Location | Coconino County, Arizona, U.S. |
| Topo map | USGS Sunset Crater East |
| Geology | |
| Volcanic field | San Francisco volcanic field |
Double Crater is an extinct Pleistocene volcano within the San Francisco volcanic field, north of Flagstaff, Arizona. It is to the southeast of Sunset Crater.
References
- ^ a b "Double Crater, Arizona". Peakbagger.com. Retrieved August 20, 2014.
- ^ "Double Crater". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved June 30, 2021.
- ^ Ulrich, G.E.; Billingsley, G.H.; Hereford, Richard; Wolfe, E.W.; Nealey, L.D.; Sutton, R.L. (1984). Map showing geology, structure, and uranium deposits of the Flagstaff 1 degrees x 2 degrees quadrangle, Arizona: (Map). 1:250000. Miscellaneous Investigations Series Map I-1446. U.S. Geological Survey.