By William Back and D.A. Stephenson (Eds.)
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Additional info for Contemporary Hydrogeology: The George Burke Maxey Memorial Volume
The main hydrogeologic factors which are prerequisites for assessing lake environments are: (1)regime dominance (the relative magnitude of groundwater in the water budget of a lake); ( 2 )system 35 efficiency (a term describing the rate aspects of surface and groundwater movement through a lake system); and (3) position within a groundwater flow system. We have indicated the significance of measuring these descriptive characteristics, and have provided “type” examples of each hydrogeologic category.
O. D. C. Winter. and proofed the manuscript. The authors share equal responsibility for this paper. 1 Reference (A) Lakes which have received the most intensive hydrogeologic analysis [this group includes: (a) lakes f o r which the groundwater flow system has been accurately defined, and/or ( b ) lakes for which the groundwater component o f the water budget has been accurately determined] : Basin A Basin B Basin E Deep Lake East Twin Lake Jyme Lake Lenore, Lake Little St. Germain Lake Mirror Lake Muskellunge Lake Pickerel Lake Sallie, Lake Shadow Lake Slough No.
Wis. , S. Dak. ,Wis. 1 881 -10,000 4,800 53 -15 14 1,019 13 26 1,270 -30 206 20 Kingsbury Pond Legend Lakes Norfolk, Mass. , Wis. , Wis. , Wis. , Wis. , Minn. l) near Woods Hole, 62 20 MW. 8 near St. Paul, Minn. , S. Dak. 9,800 15 (includes smaller nearby lake) near Buchanan, -40 N. Dak. 5 0-2? , <2 N. Dak. ,Wis. , Wis. ,Ill. , Wis. Pitcher Lake Poinsett, Lake Pothole C-1 -1 11 -5 8 Oakes et al. M. R. Williams (1967) Hoffman and Meland (1971); Born and Stephenson (1974) Sharkawy and Graaskamp (1971) Cline (1965) Oakes et al.
Contemporary Hydrogeology: The George Burke Maxey Memorial Volume by William Back and D.A. Stephenson (Eds.)