Titre de série :	United States Geological survey water supply paper, 2289
Titre :	Artesion pressures and water quality in paleozoic acquifer in the ten sleep area of the bighern basin, North-central Wyoming
Type de document :	texte imprimé
Auteurs :	Cooley, E. M.
Mention d'édition :	USGPO
Editeur :	USGPO
Année de publication :	1987
ISBN/ISSN/EAN :	CI-04014
Note générale :	The major paleozoic artesian acquifer, the acquifers most favorable for continued development, in the ten sleep area of the Bighorn basin of Wyoming are the tensleep sandstone, the madison limestone and bighorn dolomite. Most wells completed in the major and minor acquifer flow at the land surface. The initial test of one well completed in the madison -bighorn acquifer indicated flow rate of 15, 000 gallons per minute. Measurements of the pressure were made principally in 1953, 1962, 1970, and 1975-1978. Well water from the paleozoic acquifers generally contains minimal concentrations of dissolved solid and individual constituents but excessive hardness.
Langues :	Anglais (eng)
Mots-clés :	Hydrogéologie  Qualité de l'eau  Eau souterraine  Géologie  Nappe phréatique  PUITS  Paléontologie
Index. décimale :	551.48 Hydrologie :
Résumé :	The major paleozoic artesian acquifer, the acquifers most favorable for continued development, in the ten sleep area of the Bighorn basin of Wyoming are the tensleep sandstone, the madison limestone and bighorn dolomite. Most wells completed in the major and minor acquifer flow at the land surface. The initial test of one well completed in the madison -bighorn acquifer indicated flow rate of 15, 000 gallons per minute. Measurements of the pressure were made principally in 1953, 1962, 1970, and 1975-1978. Well water from the paleozoic acquifers generally contains minimal concentrations of dissolved solid and individual constituents but excessive hardness.
Note de contenu :	The major paleozoic artesian acquifer, the acquifers most favorable for continued development, in the ten sleep area of the Bighorn basin of Wyoming are the tensleep sandstone, the madison limestone and bighorn dolomite. Most wells completed in the major and minor acquifer flow at the land surface. The initial test of one well completed in the madison -bighorn acquifer indicated flow rate of 15, 000 gallons per minute. Measurements of the pressure were made principally in 1953, 1962, 1970, and 1975-1978. Well water from the paleozoic acquifers generally contains minimal concentrations of dissolved solid and individual constituents but excessive hardness.

United States Geological survey water supply paper, 2289. Artesion pressures and water quality in paleozoic acquifer in the ten sleep area of the bighern basin, North-central Wyoming [texte imprimé] / Cooley, E. M.  . -  USGPO . - USGPO, 1987.
ISSN : CI-04014
The major paleozoic artesian acquifer, the acquifers most favorable for continued development, in the ten sleep area of the Bighorn basin of Wyoming are the tensleep sandstone, the madison limestone and bighorn dolomite. Most wells completed in the major and minor acquifer flow at the land surface. The initial test of one well completed in the madison -bighorn acquifer indicated flow rate of 15, 000 gallons per minute. Measurements of the pressure were made principally in 1953, 1962, 1970, and 1975-1978. Well water from the paleozoic acquifers generally contains minimal concentrations of dissolved solid and individual constituents but excessive hardness.
Langues : Anglais (eng)

Mots-clés :	Hydrogéologie  Qualité de l'eau  Eau souterraine  Géologie  Nappe phréatique  PUITS  Paléontologie
Index. décimale :	551.48 Hydrologie :
Résumé :	The major paleozoic artesian acquifer, the acquifers most favorable for continued development, in the ten sleep area of the Bighorn basin of Wyoming are the tensleep sandstone, the madison limestone and bighorn dolomite. Most wells completed in the major and minor acquifer flow at the land surface. The initial test of one well completed in the madison -bighorn acquifer indicated flow rate of 15, 000 gallons per minute. Measurements of the pressure were made principally in 1953, 1962, 1970, and 1975-1978. Well water from the paleozoic acquifers generally contains minimal concentrations of dissolved solid and individual constituents but excessive hardness.
Note de contenu :	The major paleozoic artesian acquifer, the acquifers most favorable for continued development, in the ten sleep area of the Bighorn basin of Wyoming are the tensleep sandstone, the madison limestone and bighorn dolomite. Most wells completed in the major and minor acquifer flow at the land surface. The initial test of one well completed in the madison -bighorn acquifer indicated flow rate of 15, 000 gallons per minute. Measurements of the pressure were made principally in 1953, 1962, 1970, and 1975-1978. Well water from the paleozoic acquifers generally contains minimal concentrations of dissolved solid and individual constituents but excessive hardness.