Geohydrology of the Cross-Florida Barge Canal Area: With Special Reference to the Ocala VicinityDIANE Publishing, 1970 - 222 من الصفحات |
عبارات ومصطلحات مألوفة
Alachua altitude artesian average Avon Park Limestone Barge Canal area canal route clayey sand Coastal concentration confining layer contaminants contour Cross-Florida Barge Canal depth discharge area dolomite Dosh Lock Dunnellon Lock east Eocene Eureka Pool excavation fault feet above mean Figure Floridan Aquifer fractures geohydrologic geologic ground water ground-water flow ground-water levels Gulf Hawthorn Formation hydrologic inflow Inglis Lock Inglis Pool Johns River Lake land surface lockage losses lower pools mean sea level mg/L miles Miocene Miocene-Pliocene Mount Dora natural potentiometric surface observation station Ocala Limestone Ocala Uplift Ocala vicinity occur Oklawaha River Oklawaha River valley Orange Springs overlying Pliocene Pool stage poorly permeable Preston formation Rainbow River Rainbow Springs rainfall range shallow aquifer Silver Springs Silver Springs drainage sinkhole specific conductance Springs drainage area Summit Pool surface runoff transmissivity tritium U. S. Geol upper water level water table Withlacoochee River Yankeetown zone of outflow
مقاطع مشهورة
الصفحة ii - The use of firm, trade, and brand names in this report is for identification purposes only and does not constitute endorsement by the US Geological Survey For additional information write to: District Chief US Geological Survey 333 W.
الصفحة 113 - Geologic features of areas of abnormal radioactivity south of Ocala, Marion County, Florida: US Geol.
الصفحة 114 - RK, 1969, Carbonate geochemistry of Superior deep test well, Andros Island, Bahamas: American Association of Petroleum Geologists Bulletin, v.
الصفحة 114 - Dctrital dolomite in Onondaga Limestone (Middle Devonian) of New York — Its implications to the "dolomite question": Am.
الصفحة 115 - Geological and ground-water conditions in Florida in their relation to the Atlantic-Gulf Ship Canal.
الصفحة 76 - Orstrand has computed that under normal conditions the temperature of ground water obtained at a depth of 30 to 60 feet will generally exceed by 2° or 3° the mean annual air temperature.
الصفحة 114 - The regional lithostratigraphy of the postEocene rocks of Florida: Southeastern Geol. Soc., 9th Field Trip, p. 75-113, 3 pi., 7 figs.
الصفحة 115 - Trainer, FW, and Ellison, RL, 1967, FRACTURE TRACES IN THE SHENANDOAH VALLEY: Photogrammetric Engineering, 33 (2), p.
الصفحة 93 - With the aid of geohydrologic maps showing variations in thickness and type of cover over the aquifer, estimates may be made of the areal variation in recharge. The method is illustrated by the following diagram: where BC and AD are flow lines, and AB and CD are equipotential lines.
الصفحة 113 - F., 1 1. (and LICHTLER, WF and JOYNER, BF) Control of lake levees in Orange County, Florida: Fla Geol Survey Inf Circ 47, 15 p, Tallahassee, 1965 Provides information that will increase the understanding of and better the use of the lakes of the area. ANDERSON, WB 1. (and KEMPER, WD) Corn growth as affected by aggregate stability, soil temperature, and soil moisture: Agronomy Jour, v 56, p 453-456, 1964 The effect of soil aggregate...