| Titre de série : |
U.S. Geological Survey Water Supply paper, 2219 |
| Titre : |
Hydrogeologic setting and the potentiometric surfaces of regional aquifers in the Hollandale embayment, southeastern Minnesota, 1970 - 80 |
| Type de document : |
texte imprimé |
| Auteurs : |
Delin, G. N. ; Woodward, D. G. |
| Mention d'édition : |
United States Gouvernment Printing Office |
| Editeur : |
United States Gouvernment Printing Office |
| Année de publication : |
1984 |
| ISBN/ISSN/EAN : |
CI-05067 |
| Note générale : |
Sedimentary paleozoic rocks in the Hollandale embayment in southeastern Minnesota are as thick as 2,000 ft. This sedimentary sequence, together with the proterozoic hinckley sandstone and the quaternary drift, is divided into six regional aquifers : undifferentiated drift, upper carbonate, St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley. Potentiometric-surface maps for each aquifer indicate that mouvement of ground water is predominatly toward the major rivers. The St. Croix, Minnesota, and Mississipu rivers constitute regional discharge boundaries for ground water flow. A majoor ground-water divide in the St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley aquifers in the south-central part of the Hollandale embayment separates ground-water flow northward toward the twin cities area and southward toward Iowa. |
| Langues : |
Anglais (eng) |
| Mots-clés : |
Hydrogéologie Bassin versant Eau souterraine PRECIPITATIONS |
| Index. décimale : |
551.48 Hydrologie : |
| Résumé : |
Sedimentary paleozoic rocks in the Hollandale embayment in southeastern Minnesota are as thick as 2,000 ft. This sedimentary sequence, together with the proterozoic hinckley sandstone and the quaternary drift, is divided into six regional aquifers : undifferentiated drift, upper carbonate, St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley. Potentiometric-surface maps for each aquifer indicate that mouvement of ground water is predominatly toward the major rivers. The St. Croix, Minnesota, and Mississipu rivers constitute regional discharge boundaries for ground water flow. A majoor ground-water divide in the St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley aquifers in the south-central part of the Hollandale embayment separates ground-water flow northward toward the twin cities area and southward toward Iowa. |
| Note de contenu : |
Sedimentary paleozoic rocks in the Hollandale embayment in southeastern Minnesota are as thick as 2,000 ft. This sedimentary sequence, together with the proterozoic hinckley sandstone and the quaternary drift, is divided into six regional aquifers : undifferentiated drift, upper carbonate, St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley. Potentiometric-surface maps for each aquifer indicate that mouvement of ground water is predominatly toward the major rivers. The St. Croix, Minnesota, and Mississipu rivers constitute regional discharge boundaries for ground water flow. A majoor ground-water divide in the St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley aquifers in the south-central part of the Hollandale embayment separates ground-water flow northward toward the twin cities area and southward toward Iowa. |
U.S. Geological Survey Water Supply paper, 2219. Hydrogeologic setting and the potentiometric surfaces of regional aquifers in the Hollandale embayment, southeastern Minnesota, 1970 - 80 [texte imprimé] / Delin, G. N. ; Woodward, D. G. . - United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1984. ISSN : CI-05067 Sedimentary paleozoic rocks in the Hollandale embayment in southeastern Minnesota are as thick as 2,000 ft. This sedimentary sequence, together with the proterozoic hinckley sandstone and the quaternary drift, is divided into six regional aquifers : undifferentiated drift, upper carbonate, St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley. Potentiometric-surface maps for each aquifer indicate that mouvement of ground water is predominatly toward the major rivers. The St. Croix, Minnesota, and Mississipu rivers constitute regional discharge boundaries for ground water flow. A majoor ground-water divide in the St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley aquifers in the south-central part of the Hollandale embayment separates ground-water flow northward toward the twin cities area and southward toward Iowa. Langues : Anglais ( eng)
| Mots-clés : |
Hydrogéologie Bassin versant Eau souterraine PRECIPITATIONS |
| Index. décimale : |
551.48 Hydrologie : |
| Résumé : |
Sedimentary paleozoic rocks in the Hollandale embayment in southeastern Minnesota are as thick as 2,000 ft. This sedimentary sequence, together with the proterozoic hinckley sandstone and the quaternary drift, is divided into six regional aquifers : undifferentiated drift, upper carbonate, St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley. Potentiometric-surface maps for each aquifer indicate that mouvement of ground water is predominatly toward the major rivers. The St. Croix, Minnesota, and Mississipu rivers constitute regional discharge boundaries for ground water flow. A majoor ground-water divide in the St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley aquifers in the south-central part of the Hollandale embayment separates ground-water flow northward toward the twin cities area and southward toward Iowa. |
| Note de contenu : |
Sedimentary paleozoic rocks in the Hollandale embayment in southeastern Minnesota are as thick as 2,000 ft. This sedimentary sequence, together with the proterozoic hinckley sandstone and the quaternary drift, is divided into six regional aquifers : undifferentiated drift, upper carbonate, St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley. Potentiometric-surface maps for each aquifer indicate that mouvement of ground water is predominatly toward the major rivers. The St. Croix, Minnesota, and Mississipu rivers constitute regional discharge boundaries for ground water flow. A majoor ground-water divide in the St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley aquifers in the south-central part of the Hollandale embayment separates ground-water flow northward toward the twin cities area and southward toward Iowa. |
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