Publications
Filter Total Items: 382
Measurement of ground-water storage change and specific yield using the temporal-gravity method near Rillito Creek, Tucson, Arizona
The temporal-gravity method was used to estimate ground-water storage change and specific -yield values at wells near Rillito Creek, Tucson, Arizona, between early December 1992 and early January 1994. The method applies Newton's Law of Gravitation to measure changes in the local gravitational field of the Earth that are caused by changes in the mass and volume of ground water. Gravity at 50 stati
Authors
Donald R. Pool, Werner Schmidt
Hydrologic data, Colorado River and major tributaries, Glen Canyon Dam to Diamond Creek, Arizona, water years 1990-95
The U.S. Geological Survey collected hydrologic data at 12 continuous-record stations along the Colorado River and its major tributaries between Glen Canyon Dam and Diamond Creek. The data were collected from October 1989 through September 1995 as part of the Bureau of Reclamation's Glen Canyon Environmental Studies. The data include daily values for streamflow discharge, suspended-sediment discha
Authors
John J. Rote, Marilyn E. Flynn, D. J. Bills
Streamflow and sediment data collected to determine the effects of a controlled flood in March and April 1996 on the Colorado River between Lees Ferry and Diamond Creek, Arizona
An 8-day period of planned release of water at 1,275 cubic meters per second from Glen Canyon Dam in March and April 1996 provided an opportunity to collect data on river stage, streamflow, water chemistry, and sediment transport at discharges above powerplant releases. The U.S. Geological Survey collected data at five streamflow-gaging stations on the mainstem of the Colorado River and four on tr
Authors
Alice D. Konieczki, Julia B. Graf, Michael C. Carpenter
The Colorado River in Grand Canyon: how fast does it flow?
Opening the jet tubes at Glen Canyon Dam on March 26, 1996, released from Lake Powell a controlled flood of water that traveled down the Colorado River in Grand Canyon. How fast did the water move? How long did it take for water to reach a particular point along the river? The answers to these questions are important because the speed of river water affects the amount of physical and chemical chan
Authors
Julia B. Graf
Hydrogeology of the Quitobaquito Springs and La Abra Plain area, Organ Pipe Cactus National Monument, Arizona, and Sonora, Mexico
Quitobaquito Springs, in Organ Pipe Cactus National Monument near the south end of the northwestward-trending Quitobaquito Hills, are less than 0.25 mile north of the international boundary between the United States and Mexico. The National Park Service is concerned that the natural flow from Quitobaquito Springs might be reduced by ground-water withdrawals in the adjacent State of Sonora, Mexico.
Authors
R. L. Carruth
An accounting system for water and consumptive use along the Colorado River, Hoover Dam to Mexico
An accounting system for estimating and distributing consumptive use of water by vegetation to water users was developed for the Colorado River to meet the requirements of a U.S. Supreme Court decree and used with data from calendar year 1984. The system is based on a water-budget method to estimate total consumptive use by vegetation which is apportioned to agricultural users by using percentages
Authors
Sandra J. Owen-Joyce, Lee H. Raymond
Sand deposition in the Colorado River in the Grand Canyon from flooding of the Little Colorado River
Methods for computing the volume of sand deposited in the Colorado River in Grand Canyon National Park by floods in major tributaries and for determining redistribution of that sand by main-channel flows are required for successful management of sand-dependent riparian resources. We have derived flow, sediment transport, and bed evolution models based on a gridded topography developed from measure
Authors
S.M. Wiele, J.B. Graf, J.D. Smith
City of Flagstaff Project: Ground Water Resource Evaluation, Remote Sensing Component
Many regions, cities, and towns in the Western United States need new or expanded water resources because of both population growth and increased development. Any tools or data that can help in the evaluation of an area's potential water resources must be considered for this increasingly critical need. Remotely sensed satellite images and subsequent digital image processing have been under-utilize
Authors
Pat S. Chavez, Miguel G. Velasco, Jo-Ann Bowell, Stuart C. Sides, Rosendo R. Gonzalez, Deborah L. Soltesz
Controlled Flooding of the Colorado River in Grand Canyon: the Rationale and Data-Collection Planned
No abstract available.
Authors
Mark T. Anderson, Julia B. Graf, G. Richard Marzolf
Ground-water, surface-water, and water-chemistry data, Black Mesa area, northeastern Arizona, 1995
No abstract available.
Authors
G. R. Littin, S. A. Monroe
Physical, chemical, biological, and toxicity data from the study of urban stormwater and ephemeral streams, Maricopa County, Arizona, water years 1992-95
No abstract available.
Authors
K. D. Fossum, R.G. Davis
When the blue-green waters turn red: Historical flooding in Havasu Creek, Arizona
Havasu Creek, the second largest tributary of the Colorado River in Grand Canyon National Park, attracts numerous visitors each year owing to its spectacular scenery. Perennial streamflow seldom exceeds 2 cubic meters per second (m3/s), but supports important stands of riparian vegetation, forms unique travertine pools, and spills over spectacular waterfalls. Havasu Canyon is home to the Havasupai
Authors
Theodore S. Melis, William M. Phillips, Robert H. Webb, Douglas J. Bills