Geology of the Grand Canyon area (English Wikipedia)

Analysis of information sources in references of the Wikipedia article "Geology of the Grand Canyon area" in English language version.

refsWebsite
Global rank English rank
6th place
6th place
1st place
1st place
3rd place
3rd place
2nd place
2nd place
167th place
198th place
18th place
17th place
11th place
8th place
135th place
105th place
low place
low place
2,446th place
1,661st place
4th place
4th place
4,168th place
2,512th place
5th place
5th place
2,007th place
1,298th place
1,013th place
739th place

3news.co.nz

archive.org

books.google.com

doi.org

flickr.com

gsapubs.org

gsabulletin.gsapubs.org

harvard.edu

ui.adsabs.harvard.edu

nih.gov

pubmed.ncbi.nlm.nih.gov

nps.gov

www2.nature.nps.gov

  • An exception is the slight effect that uplifts, upwarps and swells created by earlier phases of the Laramide orogeny have. For example, formations exposed on the South Rim are 800 feet (240 m) lower than the same formations on the North Rim because the North Rim is closer to the highest part of the Kaibab Uplift.(Foos 1999, p. 1) Foos, Annabelle (1999). "Geology of Grand Canyon National Park, North Rim" (PDF). Archived from the original (PDF) on 2008-10-10. Retrieved 2008-08-11.

nps.gov

  • "There's Only One Grand Canyon" (PDF). National Park Service. Archived from the original (PDF) on September 19, 2020. Retrieved September 13, 2009.

semanticscholar.org

api.semanticscholar.org

unm.edu

tot.unm.edu

usgs.gov

walrus.wr.usgs.gov

3dparks.wr.usgs.gov

  • "Muav Limestone". Geology of National Parks, 3D and Photographic Tours. USGS. January 20, 2015. Archived from the original on November 22, 2015. Retrieved November 24, 2015.

utah.edu

sed.utah.edu

  • "Kaibab Limestone". Geology and Geophysics Department, University of Utah. 2010. Archived from the original on January 12, 2013. Retrieved November 24, 2015.

web.archive.org

  • An exception is the slight effect that uplifts, upwarps and swells created by earlier phases of the Laramide orogeny have. For example, formations exposed on the South Rim are 800 feet (240 m) lower than the same formations on the North Rim because the North Rim is closer to the highest part of the Kaibab Uplift.(Foos 1999, p. 1) Foos, Annabelle (1999). "Geology of Grand Canyon National Park, North Rim" (PDF). Archived from the original (PDF) on 2008-10-10. Retrieved 2008-08-11.
  • "There's Only One Grand Canyon" (PDF). National Park Service. Archived from the original (PDF) on September 19, 2020. Retrieved September 13, 2009.
  • "Muav Limestone". Geology of National Parks, 3D and Photographic Tours. USGS. January 20, 2015. Archived from the original on November 22, 2015. Retrieved November 24, 2015.
  • "Kaibab Limestone". Geology and Geophysics Department, University of Utah. 2010. Archived from the original on January 12, 2013. Retrieved November 24, 2015.
  • Flowers, R. M.; Farley, K. A. (2012). "Apatite 4He/3He and (U-Th)/He Evidence for an Ancient Grand Canyon". Science. 338 (6114): 1616–1619. Bibcode:2012Sci...338.1616F. doi:10.1126/science.1229390. PMID 23196906. S2CID 32277486.
    "Debate rages over Grand Canyon's origins". 3 News. December 3, 2012. Archived from the original on October 31, 2013. Retrieved December 2, 2012.
  • Torresan, Laura Zink. "Grand Canyon Studies: Glen Canyon Dam". United States Geological Survey. Archived from the original on 2009-09-21. Retrieved 2009-08-30.
  • Torresan, Laura Zink. "Effects of Glen Canyon Dam on Water in the Colorado River". United States Geological Survey. Archived from the original on 2009-05-12. Retrieved 2009-08-30.
  • Torresan, Laura Zink. "Controlled Flood". United States Geological Survey. Archived from the original on 2013-04-11. Retrieved 2009-08-30.

worldcat.org

search.worldcat.org