Rebecca Lambert
AFCEC Liaison, Oklahoma-Texas Water Science Center
Education and Certifications
Master of Science - Geology (1986) - Texas A&M University
Bachelor of Science - Geology (1982) - Texas A&M University
Affiliations and Memberships*
Registered Profession Geoscientist - Geology -- State of Texas License #6539
Science and Products
Filter Total Items: 21
Hydrogeology of Webb County, Texas
IntroductionWebb County, in semiarid South Texas on the U.S.-Mexico border, is a region confronted by increasing stresses on natural resources. Laredo (fig. 1), the largest city in Webb County (population 193,000 in 2000), was one of the 10 fastest-growing metropolitan areas in the country during 1990-2000 (Perry and Mackun, 2001). Commercial and industrial activities have expanded throughout the
Authors
Rebecca B. Lambert
Hydrogeology, hydrologic budget, and water chemistry of the Medina Lake area, Texas
A three-phase study of the Medina Lake area in Texas was done to assess the hydrogeology and hydrology of Medina and Diversion Lakes combined (the lake system) and to determine what fraction of seepage losses from the lake system might enter the regional ground-water-flow system of the Edwards and (or) Trinity aquifers. Phase 1 consisted of revising the geologic framework for the Medina Lake area.
Authors
Rebecca B. Lambert, Kenneth C. Grimm, Roger W. Lee
Quality of ground water in Webb County, Texas, 1997-98
Rapid development and population growth are occurring in Webb County in south Texas (fig. 1). Water managers need information on the ground-water resources of the area to address the increased demand for water caused by the development. To help meet this need, the U.S. Geological Survey (USGS), in cooperation with the City of Laredo, began a study in 1997 to assess the ground-water resources of th
Authors
Rebecca B. Lambert, Charles A. Hartmann
Geologic framework and hydrogeologic characteristics of the outcrops of the Edwards and Trinity aquifers, Medina Lake area, Texas
The hydrogeologic subdivisions of the Edwards aquifer outcrop in the Medina Lake area in Medina and Bandera Counties generally are porous and permeable. The most porous and permeable appear to be hydrogeologic subdivision VI, the Kirschberg evaporite member of the Kainer Formation; and hydrogeologic subdivision III, the leached and collapsed members, undivided, of the Person Formation. The porosit
Authors
Ted A. Small, Rebecca B. Lambert
Water resources data, Iowa, water year 1992
No abstract available.
Authors
J.G. Gorman, C.J. Anderson, R.B. Lambert, D. Sneck-Fahrer, W. Wang
Water resources data, Iowa, water year 1991
Water resources data for the 1991 water year for Iowa consist of records of stage discharge,and water quality of streams; stage, contents, and water quality of lakes and reservoirs; ground water levels and water quality of ground-water wells. This report contains records of water discharge for 118 stream-gaging stations; stage or contents for 9 lakes and reservoirs; water quality for 6 stream-gagi
Authors
D. J. O'Connell, R.B. Lambert, W.J. Matthes, D. Sneck-Fahrer
The ground-water-level monitoring network in Iowa
The ground-water-level monitoring network in Iowa consists of 202 wells completed in the principal bedrock and surficial aquifers that supply ground water to numerous users throughout the State. The bedrock aquifers include the Cambrian-Ordovician aquifer system, the Silurian-Devonian aquifer, the Mississippian aquifer, localized Pennsylvanian aquifers, and the Dakota aquifer. The surficial aquife
Authors
R.B. Lambert
Water resources data, Iowa, water year 1990
Water resources data for the 1990 water year for Iowa consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; ground water levels and water quality of ground-water wells. This report contains records of water discharge for 117 stream-gaging stations; stage or contents for 9 lakes and reservoirs; water quality for 6 stream-ga
Authors
D. J. O'Connell, M. J. Liszewski, R.B. Lambert, W.J. Matthes
Water resources data, Iowa, water year 1989
Water resources data for the 1989 water year for Iowa consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; ground water levels and water quality of ground-water wells. This report contains records of water discharge for 117 stream-gaging stations; stage or contents for 8 lakes and reservoirs; water quality for 6 stream-ga
Authors
D. J. O'Connell, M. J. Liszewski, R.B. Lambert, W.J. Matthes
Science and Products
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Filter Total Items: 21
Hydrogeology of Webb County, Texas
IntroductionWebb County, in semiarid South Texas on the U.S.-Mexico border, is a region confronted by increasing stresses on natural resources. Laredo (fig. 1), the largest city in Webb County (population 193,000 in 2000), was one of the 10 fastest-growing metropolitan areas in the country during 1990-2000 (Perry and Mackun, 2001). Commercial and industrial activities have expanded throughout theAuthorsRebecca B. LambertHydrogeology, hydrologic budget, and water chemistry of the Medina Lake area, Texas
A three-phase study of the Medina Lake area in Texas was done to assess the hydrogeology and hydrology of Medina and Diversion Lakes combined (the lake system) and to determine what fraction of seepage losses from the lake system might enter the regional ground-water-flow system of the Edwards and (or) Trinity aquifers. Phase 1 consisted of revising the geologic framework for the Medina Lake area.AuthorsRebecca B. Lambert, Kenneth C. Grimm, Roger W. LeeQuality of ground water in Webb County, Texas, 1997-98
Rapid development and population growth are occurring in Webb County in south Texas (fig. 1). Water managers need information on the ground-water resources of the area to address the increased demand for water caused by the development. To help meet this need, the U.S. Geological Survey (USGS), in cooperation with the City of Laredo, began a study in 1997 to assess the ground-water resources of thAuthorsRebecca B. Lambert, Charles A. HartmannGeologic framework and hydrogeologic characteristics of the outcrops of the Edwards and Trinity aquifers, Medina Lake area, Texas
The hydrogeologic subdivisions of the Edwards aquifer outcrop in the Medina Lake area in Medina and Bandera Counties generally are porous and permeable. The most porous and permeable appear to be hydrogeologic subdivision VI, the Kirschberg evaporite member of the Kainer Formation; and hydrogeologic subdivision III, the leached and collapsed members, undivided, of the Person Formation. The porositAuthorsTed A. Small, Rebecca B. LambertWater resources data, Iowa, water year 1992
No abstract available.AuthorsJ.G. Gorman, C.J. Anderson, R.B. Lambert, D. Sneck-Fahrer, W. WangWater resources data, Iowa, water year 1991
Water resources data for the 1991 water year for Iowa consist of records of stage discharge,and water quality of streams; stage, contents, and water quality of lakes and reservoirs; ground water levels and water quality of ground-water wells. This report contains records of water discharge for 118 stream-gaging stations; stage or contents for 9 lakes and reservoirs; water quality for 6 stream-gagiAuthorsD. J. O'Connell, R.B. Lambert, W.J. Matthes, D. Sneck-FahrerThe ground-water-level monitoring network in Iowa
The ground-water-level monitoring network in Iowa consists of 202 wells completed in the principal bedrock and surficial aquifers that supply ground water to numerous users throughout the State. The bedrock aquifers include the Cambrian-Ordovician aquifer system, the Silurian-Devonian aquifer, the Mississippian aquifer, localized Pennsylvanian aquifers, and the Dakota aquifer. The surficial aquifeAuthorsR.B. LambertWater resources data, Iowa, water year 1990
Water resources data for the 1990 water year for Iowa consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; ground water levels and water quality of ground-water wells. This report contains records of water discharge for 117 stream-gaging stations; stage or contents for 9 lakes and reservoirs; water quality for 6 stream-gaAuthorsD. J. O'Connell, M. J. Liszewski, R.B. Lambert, W.J. MatthesWater resources data, Iowa, water year 1989
Water resources data for the 1989 water year for Iowa consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; ground water levels and water quality of ground-water wells. This report contains records of water discharge for 117 stream-gaging stations; stage or contents for 8 lakes and reservoirs; water quality for 6 stream-gaAuthorsD. J. O'Connell, M. J. Liszewski, R.B. Lambert, W.J. Matthes
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government