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Auteur Takasaki, K. J. |
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U. S. Geological Survey Water Supply paper, 2217. Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu / Takasaki, K. J.
Titre de série : U. S. Geological Survey Water Supply paper, 2217 Titre : Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu Type de document : texte imprimé Auteurs : Takasaki, K. J. ; Mink, J. F. Mention d'édition : United State Government Printing Office Editeur : United State Government Printing Office Année de publication : 1985 ISBN/ISSN/EAN : CI-05065 Note générale : Ground-water reservoirs impounded by volcanic dikes receive a substantial part of the total recharge to ground water on the Island of Oahu because they generally underline the rainiest areas. These reservoirs accumulate the infliltration from rainfall, store it temporarily, and steadily leak it to abutting basal reservoirs or to streams cutting into them. The dike reservoirs have high hydraulic heads and are mostly isolated from saline water. The most important and productive of the dike-impounded reservoirs are in on area of about 135 square miles in the main fissure zone of the Koolau volcano where the top of the dike-impounded water reaches an altitude of at least 1,000 feet. Langues : Anglais (eng) Mots-clés : Eau souterraine Réservoir Hydrogéologie Volcanisme Index. décimale : 551 Géologie, météorologie, hydrologie générale Résumé : Ground-water reservoirs impounded by volcanic dikes receive a substantial part of the total recharge to ground water on the Island of Oahu because they generally underline the rainiest areas. These reservoirs accumulate the infliltration from rainfall, store it temporarily, and steadily leak it to abutting basal reservoirs or to streams cutting into them. The dike reservoirs have high hydraulic heads and are mostly isolated from saline water. The most important and productive of the dike-impounded reservoirs are in on area of about 135 square miles in the main fissure zone of the Koolau volcano where the top of the dike-impounded water reaches an altitude of at least 1,000 feet. Note de contenu : Ground-water reservoirs impounded by volcanic dikes receive a substantial part of the total recharge to ground water on the Island of Oahu because they generally underline the rainiest areas. These reservoirs accumulate the infliltration from rainfall, store it temporarily, and steadily leak it to abutting basal reservoirs or to streams cutting into them. The dike reservoirs have high hydraulic heads and are mostly isolated from saline water. The most important and productive of the dike-impounded reservoirs are in on area of about 135 square miles in the main fissure zone of the Koolau volcano where the top of the dike-impounded water reaches an altitude of at least 1,000 feet. U. S. Geological Survey Water Supply paper, 2217. Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu [texte imprimé] / Takasaki, K. J. ; Mink, J. F. . - United State Government Printing Office . - United State Government Printing Office, 1985.
ISSN : CI-05065
Ground-water reservoirs impounded by volcanic dikes receive a substantial part of the total recharge to ground water on the Island of Oahu because they generally underline the rainiest areas. These reservoirs accumulate the infliltration from rainfall, store it temporarily, and steadily leak it to abutting basal reservoirs or to streams cutting into them. The dike reservoirs have high hydraulic heads and are mostly isolated from saline water. The most important and productive of the dike-impounded reservoirs are in on area of about 135 square miles in the main fissure zone of the Koolau volcano where the top of the dike-impounded water reaches an altitude of at least 1,000 feet.
Langues : Anglais (eng)
Mots-clés : Eau souterraine Réservoir Hydrogéologie Volcanisme Index. décimale : 551 Géologie, météorologie, hydrologie générale Résumé : Ground-water reservoirs impounded by volcanic dikes receive a substantial part of the total recharge to ground water on the Island of Oahu because they generally underline the rainiest areas. These reservoirs accumulate the infliltration from rainfall, store it temporarily, and steadily leak it to abutting basal reservoirs or to streams cutting into them. The dike reservoirs have high hydraulic heads and are mostly isolated from saline water. The most important and productive of the dike-impounded reservoirs are in on area of about 135 square miles in the main fissure zone of the Koolau volcano where the top of the dike-impounded water reaches an altitude of at least 1,000 feet. Note de contenu : Ground-water reservoirs impounded by volcanic dikes receive a substantial part of the total recharge to ground water on the Island of Oahu because they generally underline the rainiest areas. These reservoirs accumulate the infliltration from rainfall, store it temporarily, and steadily leak it to abutting basal reservoirs or to streams cutting into them. The dike reservoirs have high hydraulic heads and are mostly isolated from saline water. The most important and productive of the dike-impounded reservoirs are in on area of about 135 square miles in the main fissure zone of the Koolau volcano where the top of the dike-impounded water reaches an altitude of at least 1,000 feet. Réservation
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