Grand Canyon Monitoring and Research Center

Grand Canyon Sandbar Monitoring

Introduction

Since the completion of Glen Canyon Dam in 1963, the amount of sand supplied to Grand Canyon National Park has been reduced by more than 90 percent. The Paria River, a tributary to the Colorado River 15 miles downstream from the dam, is now the single most important supplier of sand to the Colorado River within the Park. This large reduction in sand supply has resulted in substantial decrease in the number and size of sandbars. Sandbars are important because they serve as campsites for river runner and hikers, provide important aquatic and riparian habitats, and are the source of sand that may help protect archaeological sites. The information collected by this project will be used to determine whether dam operations, including short-duration artificial floods, cause increases or decreases in sandbars and associated campsites in Grand Canyon National Park.

The Sandbar Monitoring Data

Currently, topographic maps are made at a set of monitoring sites annually using conventional survey equipment. These surveys are used to calculate the size of each sandbar in terms of the area of exposed sand and the volume of sand contained in the bar. Both of these calculations are relative to an elevation of interest.




For Additional Information
For additional information, please contact
Project Chief
  • Paul Grams
    • USGS Southwest Biological Science Center
    • Grand Canyon Monitoring Research Center
    • Contact pgrams@usgs.gov or (928)-556-7385
Database Designer/Programmer
  • Kathryn Schoephoester
    • USGS Center for Integrated Data Analytics
Website Design and Programming
  • USGS Center for Integrated Data Analytics
Current Database/Website Maintenance
  • James Hensleigh
    • USGS Southwest Biological Science Center
    • Grand Canyon Monitoring Research Center
Terms of Use

The data presented in this website are collected and processed using standard USGS protocols and other established peer-reviewed methods, and subject to rigorous quality control. Nevertheless, minor edits of these data are possible.

The data are released on the condition that neither the USGS nor the U.S. Government may be held liable for any damages resulting from its authorized or unauthorized use.

References
Methods
  • Hazel, J.E., Jr., Grams, P.E., Schmidt, J.C., and Kaplinski, M., 2010, Sandbar response in Marble and Grand Canyons, Arizona, following the 2008 high-flow experiment on the Colorado River: U.S. Geological Survey Scientific Investigations Report 2010–5015, 52 p. http://pubs.usgs.gov/sir/2010/5015/.
Recent Publications
  • Grams P. E., 2013, A sand budget for Marble Canyon, Arizona -- implications for long-term monitoring of sand storage change, U.S. Geological Survey Fact Sheet 2013–3074, 4p., http://pubs.usgs.gov/fs/2013/3074.
  • Grams P. E., D. J. Topping, J. C. Schmidt, J. E. Hazel Jr., and M. Kaplinski, 2013, Linking morphodynamic response with sediment mass balance on the Colorado River in Marble Canyon: Issues of scale, geomorphic setting, and sampling design, J. Geophys. Res. Earth Surf., 118, 361–381, doi:10.1002/jgrf.20050. http://onlinelibrary.wiley.com/doi/10.1002/jgrf.20050/full
Full Publication List
Cooperating Agencies and Academic Institutions
Cooperating USGS Water Science Centers
Grand Canyon Monitoring & Research Center | 2255 North Gemini Drive Flagstaff, AZ 86001 | Phone: 928.556.7380 Fax: 928.556.7100

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