Steamboat Mountain (Coconino County, Arizona) Explained

Steamboat Mountain
Label:Steamboat Mountain
Label Position:bottom
Elevation Ft:7410
Elevation Ref:[1]
Prominence Ft:1370
Isolation Mi:2.48
Isolation Ref:[2]
Parent Peak:Powell Plateau (7,661 ft)
Location:Grand Canyon National Park
Coconino County, Arizona, US
Range:Kaibab Plateau
Colorado Plateau
Map:Arizona#USA
Map Size:230
Coordinates:36.3658°N -112.3988°W
Coordinates Ref:[3]
Topo:USGS Powell Plateau
Rock:sandstone, limestone, mudstone
First Ascent:October 17, 1964 Harvey Butchart, Marshall Demick [4]

Steamboat Mountain is a 7410feet summit located in the Grand Canyon, in Coconino County of northern Arizona, US.[3] It is situated four miles northwest of Holy Grail Temple, and 2.5 miles west-southwest of Timp Point on the North Rim. George Wharton James described it as a "majestic butte", nearly encircled by Galloway and Saddle Canyons.[5] Topographic relief is significant as it rises over 5400abbr=offNaNabbr=off above the Colorado River in three miles. According to the Köppen climate classification system, Steamboat Mountain is located in a Cold semi-arid climate zone, with precipitation runoff draining west to the Colorado River via Tapeats Creek and Stone Creek.[6] This feature's name was officially adopted in 1932 by the U.S. Board on Geographic Names.[3]

History

In 1858, Lieutenant Joseph Ives led an expedition up the Colorado River, starting at the river's mouth and making it to the lower Grand Canyon. The mode of transportation was a steamboat named Explorer. Steamboat Mountain is located in an area of geographical features that were named after the canyon's early explorers. Steamboat Mountain is set at the northern tip of Powell Plateau, named for John Wesley Powell. Ives Point lies six miles to the southwest at the southwest tip of Powell Plateau. Also on Powell Plateau are Newberry Point, Dutton Point, Wheeler Point, Thompson Point, and Beale Point. These Grand Canyon pioneers are collectively commemorated by Explorers Monument, located immediately south of Powell Plateau.[7]

Geology

Steamboat Mountain is composed of Permian Kaibab Limestone, overlaying a conspicuous band of cream-colored, cliff-forming, Permian Coconino Sandstone.[8] The sandstone, which is the third-youngest of the strata in the Grand Canyon, was deposited 265 million years ago as sand dunes. Below the conspicuous Coconino Sandstone layer is slope-forming, Permian Hermit Formation, which in turn overlays the Pennsylvanian-Permian Supai Group.[9] Further down are strata of Mississippian Redwall Limestone, the Cambrian Tonto Group, and finally Paleoproterozoic Vishnu Basement Rocks at river level in Granite Gorge.

See also

External links

Notes and References

  1. 3905. Steamboat Mountain, Arizona. 2021-01-09.
  2. Web site: Steamboat Mountain – 7,410' AZ . Lists of John . January 9, 2021 .
  3. 42841 . Steamboat Mountain . 2021-01-09.
  4. https://archive.library.nau.edu/digital/collection/cpa/id/66659 Harvey Butchart’s Hiking Log – Detailed Hiking Log (February 28, 1964 – December 31, 1964)
  5. George Wharton James, The Grand Canyon of Arizona How to See It, 1910, Little Brown and Company, page 83.
  6. Peel, M. C. . Finlayson, B. L. . McMahon, T. A. . 2007 . Updated world map of the Köppen−Geiger climate classification . Hydrol. Earth Syst. Sci. . 11 . 1027-5606.
  7. Randy Moore and Kara Felicia Witt, The Grand Canyon: An Encyclopedia of Geography, History, and Culture, 2018, ABC-CLIO Publisher, page 74.
  8. N.H. Darton, Story of the Grand Canyon of Arizona, 1917.
  9. William Kenneth Hamblin, Anatomy of the Grand Canyon: Panoramas of the Canyon's Geology, 2008, Grand Canyon Association Publisher, .