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Auteur Lewis, B. D. |
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Faire une suggestion Affiner la rechercheU.S. Geological Survey Water Supply paper, 2191. Hydrologic conditions at the Idaho National Engineering Laboratory, Idaho - Emphasis : 1977 - 1978 / Bamadough, J. T.
Titre de série : U.S. Geological Survey Water Supply paper, 2191 Titre : Hydrologic conditions at the Idaho National Engineering Laboratory, Idaho - Emphasis : 1977 - 1978 Type de document : texte imprimé Auteurs : Bamadough, J. T. ; Lewis, B. D. ; Jensen, R. G. Mention d'édition : U. S. Geological Survey Editeur : U. S. Geological Survey Année de publication : 1982 ISBN/ISSN/EAN : CI-05110 Note générale : The Idaho National Engineering Laboratory (INEL) site covers about 890 square miles of the eastern snake river plain and overlies the snake river plain aquifer. This report describes the water resources of the INEL and adjacent areas. Information was collected which depicted hydrogeologic conditions prior to any reactor operations at the laboratory. Current investigations serve to determine natural changes in the hydrogeology and also to determine national changes in the hydrogeology and also to determine changes resulting from activities at the laboratory. Langues : Anglais (eng) Mots-clés : Hydrologie Ressource en eau Hydrogéologie Eau de surface Eau souterraine Qualité de l'eau Pollution Index. décimale : 551.48 Hydrologie : Résumé : The Idaho National Engineering Laboratory (INEL) site covers about 890 square miles of the eastern snake river plain and overlies the snake river plain aquifer. This report describes the water resources of the INEL and adjacent areas. Information was collected which depicted hydrogeologic conditions prior to any reactor operations at the laboratory. Current investigations serve to determine natural changes in the hydrogeology and also to determine national changes in the hydrogeology and also to determine changes resulting from activities at the laboratory. Note de contenu : The Idaho National Engineering Laboratory (INEL) site covers about 890 square miles of the eastern snake river plain and overlies the snake river plain aquifer. This report describes the water resources of the INEL and adjacent areas. Information was collected which depicted hydrogeologic conditions prior to any reactor operations at the laboratory. Current investigations serve to determine natural changes in the hydrogeology and also to determine national changes in the hydrogeology and also to determine changes resulting from activities at the laboratory. U.S. Geological Survey Water Supply paper, 2191. Hydrologic conditions at the Idaho National Engineering Laboratory, Idaho - Emphasis : 1977 - 1978 [texte imprimé] / Bamadough, J. T. ; Lewis, B. D. ; Jensen, R. G. . - U. S. Geological Survey . - U. S. Geological Survey, 1982.
ISSN : CI-05110
The Idaho National Engineering Laboratory (INEL) site covers about 890 square miles of the eastern snake river plain and overlies the snake river plain aquifer. This report describes the water resources of the INEL and adjacent areas. Information was collected which depicted hydrogeologic conditions prior to any reactor operations at the laboratory. Current investigations serve to determine natural changes in the hydrogeology and also to determine national changes in the hydrogeology and also to determine changes resulting from activities at the laboratory.
Langues : Anglais (eng)
Mots-clés : Hydrologie Ressource en eau Hydrogéologie Eau de surface Eau souterraine Qualité de l'eau Pollution Index. décimale : 551.48 Hydrologie : Résumé : The Idaho National Engineering Laboratory (INEL) site covers about 890 square miles of the eastern snake river plain and overlies the snake river plain aquifer. This report describes the water resources of the INEL and adjacent areas. Information was collected which depicted hydrogeologic conditions prior to any reactor operations at the laboratory. Current investigations serve to determine natural changes in the hydrogeology and also to determine national changes in the hydrogeology and also to determine changes resulting from activities at the laboratory. Note de contenu : The Idaho National Engineering Laboratory (INEL) site covers about 890 square miles of the eastern snake river plain and overlies the snake river plain aquifer. This report describes the water resources of the INEL and adjacent areas. Information was collected which depicted hydrogeologic conditions prior to any reactor operations at the laboratory. Current investigations serve to determine natural changes in the hydrogeology and also to determine national changes in the hydrogeology and also to determine changes resulting from activities at the laboratory. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B110.92434 CI-05110 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B110.92433 CI-05110 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B110.92432 CI-05110 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B110.92431 CI-05110 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B110.92430 CI-05110 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B110.92427 CI-05110 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B110.92429 CI-05110 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B110.92428 CI-05110 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible
Titre de série : U.S. Geological Survey Water Supply paper, 2239 Titre : Ground-water resources and potential hydrologic effects of surface coal mining in the northern powder river basin, Southeastern Montana Type de document : texte imprimé Auteurs : Slagle, S. E. ; Lewis, B. D. ; Lee, R. W. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1985 ISBN/ISSN/EAN : CI-05059 Note générale : The shallow groundwater system in the northern powder river basin consists of upper cretaceous to holocene aquifers overlying the bearpaw shale-namely, the fox hills sandstone/ hell, creek, fort union, and wasatch formations/ terrace deposits, and alluvium. Ground-water flow above the bearfow shale can be divided into two general flow patterns. An upper flow pattern occurs in aquifers at depths of less than about 200 feet and occurs primarily as localized flow controlled by the surface topography. A lower flow pattern occurs in aquifer of depths from about 200 to 1,200 feet and exhibits a more regional flow, which is generally northward toward the yellowstone river with significant flow toward the powder and tongue rivers. Langues : Anglais (eng) Mots-clés : Eau souterraine Ressource en eau Hydrologie Géologie Bassin HYDROGEOLOGIE PRECIPITATIONS Irrigation Evapotranspiration Qualité de l'eau Index. décimale : 551 Géologie, météorologie, hydrologie générale Résumé : The shallow groundwater system in the northern powder river basin consists of upper cretaceous to holocene aquifers overlying the bearpaw shale-namely, the fox hills sandstone/ hell, creek, fort union, and wasatch formations/ terrace deposits, and alluvium. Ground-water flow above the bearfow shale can be divided into two general flow patterns. An upper flow pattern occurs in aquifers at depths of less than about 200 feet and occurs primarily as localized flow controlled by the surface topography. A lower flow pattern occurs in aquifer of depths from about 200 to 1,200 feet and exhibits a more regional flow, which is generally northward toward the yellowstone river with significant flow toward the powder and tongue rivers. Note de contenu : The shallow groundwater system in the northern powder river basin consists of upper cretaceous to holocene aquifers overlying the bearpaw shale-namely, the fox hills sandstone/ hell, creek, fort union, and wasatch formations/ terrace deposits, and alluvium. Ground-water flow above the bearfow shale can be divided into two general flow patterns. An upper flow pattern occurs in aquifers at depths of less than about 200 feet and occurs primarily as localized flow controlled by the surface topography. A lower flow pattern occurs in aquifer of depths from about 200 to 1,200 feet and exhibits a more regional flow, which is generally northward toward the yellowstone river with significant flow toward the powder and tongue rivers. U.S. Geological Survey Water Supply paper, 2239. Ground-water resources and potential hydrologic effects of surface coal mining in the northern powder river basin, Southeastern Montana [texte imprimé] / Slagle, S. E. ; Lewis, B. D. ; Lee, R. W. . - United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1985.
ISSN : CI-05059
The shallow groundwater system in the northern powder river basin consists of upper cretaceous to holocene aquifers overlying the bearpaw shale-namely, the fox hills sandstone/ hell, creek, fort union, and wasatch formations/ terrace deposits, and alluvium. Ground-water flow above the bearfow shale can be divided into two general flow patterns. An upper flow pattern occurs in aquifers at depths of less than about 200 feet and occurs primarily as localized flow controlled by the surface topography. A lower flow pattern occurs in aquifer of depths from about 200 to 1,200 feet and exhibits a more regional flow, which is generally northward toward the yellowstone river with significant flow toward the powder and tongue rivers.
Langues : Anglais (eng)
Mots-clés : Eau souterraine Ressource en eau Hydrologie Géologie Bassin HYDROGEOLOGIE PRECIPITATIONS Irrigation Evapotranspiration Qualité de l'eau Index. décimale : 551 Géologie, météorologie, hydrologie générale Résumé : The shallow groundwater system in the northern powder river basin consists of upper cretaceous to holocene aquifers overlying the bearpaw shale-namely, the fox hills sandstone/ hell, creek, fort union, and wasatch formations/ terrace deposits, and alluvium. Ground-water flow above the bearfow shale can be divided into two general flow patterns. An upper flow pattern occurs in aquifers at depths of less than about 200 feet and occurs primarily as localized flow controlled by the surface topography. A lower flow pattern occurs in aquifer of depths from about 200 to 1,200 feet and exhibits a more regional flow, which is generally northward toward the yellowstone river with significant flow toward the powder and tongue rivers. Note de contenu : The shallow groundwater system in the northern powder river basin consists of upper cretaceous to holocene aquifers overlying the bearpaw shale-namely, the fox hills sandstone/ hell, creek, fort union, and wasatch formations/ terrace deposits, and alluvium. Ground-water flow above the bearfow shale can be divided into two general flow patterns. An upper flow pattern occurs in aquifers at depths of less than about 200 feet and occurs primarily as localized flow controlled by the surface topography. A lower flow pattern occurs in aquifer of depths from about 200 to 1,200 feet and exhibits a more regional flow, which is generally northward toward the yellowstone river with significant flow toward the powder and tongue rivers. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B059.77730 CI-05059 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B059.77729 CI-05059 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B059.77728 CI-05059 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B059.77727 CI-05059 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B059.77726 CI-05059 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B059.77725 CI-05059 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B059.77724 CI-05059 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B059.77723 CI-05059 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible
