S P Crater

In this article we are going to explore the fascinating world of S P Crater. From its origin to its evolution today, S P Crater has left an indelible mark on society. Whether you are passionate about S P Crater or this is the first time you are hearing about it, this article will take you on a journey through its most relevant aspects. We will discover its importance in different contexts and its impact on our lives. Prepare to immerse yourself in the richness and diversity of S P Crater, and you will find that it never ceases to surprise and enrich our lives in unexpected ways.

S P Crater
Highest point
Elevation7,021 ft (2,140 m) NGVD 29[1]
Coordinates35°34′56″N 111°37′55″W / 35.5822254°N 111.6318207°W / 35.5822254; -111.6318207[2]
Geography
S P Crater is located in Arizona
S P Crater
S P Crater
LocationCoconino County, Arizona, U.S.
Geology
Rock age~6.0–5.5 ka[3]
Mountain typeCinder cone
Volcanic fieldSan Francisco volcanic field

S P Crater is a cinder cone volcano in the San Francisco volcanic field, 25 miles (40 km) north of Flagstaff, Arizona, United States.[4] It is surrounded by several other cinder cones which are older and more eroded. It is a striking feature on the local landscape, with a well-defined lava flow that extends for 4.3 miles (7 km) to the north.[5] American astronauts use the crater to train for moonwalking.[6]

Name

The naming of the mountain is a bit of lore from the Old West. S P Crater can be climbed, and the lava flow can be viewed from the crater rim. C. J. Babbit, an 1880s rancher and early landowner of the mountain, expressed his opinion that the mountain resembled a spilled chamber pot (or Shit Pot, "SP"),[7] and locally this became the accepted name.[5] When viewed from certain angles on the ground, the combination of the smooth round shape of the cone, the dark lava spatter on the rim, and the long dark lava flow extruding from the base may resemble human waste. Mapmakers refused to spell out the full name, and the mountain has been shown on maps and other literature with the abbreviated name.[8]

Geology

S P Crater is an 820-foot (250 m) high cinder cone of basaltic andesite. The cone is capped by an agglomerate rim that helps to protect its structure. A lava flow extends to the north of the cone for about 7 km (4.3 mi) and originated from the same vent.[9] Some scientists consider the lava flow to have slightly predated the cinder cone because of geochemical data that suggests the flow is more silica rich than the cinders and based on the observation that the cone overlaps the lava flow and shows no sign of deformation.[9] However, there is some debate about the relationship between the cone and flow as it is not uncommon to form cinder cones during the early phase of an eruption as a magma degasses, and then to have lava push through the side of a cone during a late phase of eruption.

K–Ar dates on the lava are about 70 ka,[10] but are considered unreliable because of excess argon[11] and the un-weathered young appearance of the cone. More recent optically stimulated luminescence age dating on single-grain quartz xenocrysts from basalt flows at S P Crater has yielded more reliable ages of 6.25±0.86 ka and 5.46±0.70 ka for the older flow, and 5.51±0.60 ka for the younger flow, together suggesting a generalized date of ~6.0–5.5 ka that is more concordant with its youthful geomorphic character.[3]

References

  1. ^ "S P Mountain". ListsOfJohn.com. Retrieved January 25, 2013.
  2. ^ "S P Crater". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved June 30, 2021.
  3. ^ a b Rittenour, T. M.; Riggs, N. R.; Kennedy, L. E. (February 9, 2012). "Application of single-grain OSL to date quartz xenocrysts within a basalt flow, San Francisco volcanic field, northern Arizona, USA". Quaternary Geochronology. 10. Elsevier BV: 300–307. doi:10.1016/j.quageo.2012.02.002. Retrieved February 24, 2024.
  4. ^ Priest, Susan S.; Wendell A. Duffield; Karen Malis-Clark; James W. Hendley II; et al. (December 21, 2001). "The San Francisco Volcanic Field, Arizona: USGS Fact Sheet 017-01". United States Geological Survey. Retrieved September 2, 2008.
  5. ^ a b Lopes, Rosaly (February 7, 2005). The Volcano Adventure Guide. Cambridge University Press. p. 153. ISBN 978-0521554534.
  6. ^ In the Arizona desert, NASA prepares for walking on the moon National Geographic, 2022-11-09.
  7. ^ Weir, Bill (1999). Arizona Handbook. Moon Publications. p. 205. ISBN 1566911435.
  8. ^ Hannigan, Chris (August 24, 2011). "San Francisco Volcanic Field (Volcano week 6)". Google Sightseeing. Retrieved February 1, 2014.
  9. ^ a b Ulrich, G E (1987). "SP Mountain cinder cone and lava flow, northern Arizona" (Document). Geological Society of American Centennial Field Guide – Rocky Mountain Section. pp. 385–388.
  10. ^ Baksi, A. K. (1974). "K-Ar study of the S.P. flow". Canadian Journal of Earth Sciences. 11 (10): 1350–1356, v11. Bibcode:1974CaJES..11.1350B. doi:10.1139/e74-131.
  11. ^ Duffield, Wendell A.; Riggs, Nancy; Kaufman, Darrell; Champion, Duane; et al. (2006). "Multiple constraints on the age of a Pleistocene lava dam across the Little Colorado River at Grand Falls, Arizona". Geological Society of America Bulletin. 118 (3–4): 421–429. Bibcode:2006GSAB..118..421D. doi:10.1130/B25814.1.
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