Hydrogeologic framework of the Michigan basin regional aquifier system.

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Pagination47 p.
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the shallow aquifer system beneath the city and to bet-ter understand the distribution of fresh ground water, its potential use, and its susceptibility to contamination (Johnson, ). Purpose and scope A revision of the conceptual hydrogeologic framework of the shallow aquifer system at Virginia Beach is presented in this report. Introduction. Regional‐scale classification of groundwater systems provides a basis for understanding and management of groundwater resources (Barthel ; Dennehy et al. ).In the United States (U.S.), two classification systems have been widely used: an approach developed by Heath (, , ), and subsequent work by the U.S. Geological Survey . Hydrogeologic framework of the study area. (A) Subcrop formations and major structures present in the Michigan Basin—Lower Peninsula of Michigan (after Dorr & Eschman ; Fisher et al. A Regional Hydrogeologic Assessment (RHA) is a systematic study of a multi-county region's geologic and ground-water resources. Geologic studies focus on near-surface deposits. Ground-water studies include flow systems, aquifer capacity, ground-water chemistry, and sand and gravel deposits. Sensitivity of near ground-water systems is estimated.

The purpose of this project is to provide site-specific hydrogeologic data on the Floridan aquifer system (FAS) at three sites in support of the Lake Okeechobee ASR Pilot collected from the testing and monitoring of these test wells will be instrumental in site selection for. EXW-1 was left idle until a planned hour APT could be conducted at the site. HYDROGEOLOGIC FRAMEWORK Two major aquifer systems underlie this site: the Surficial Aquifer System (SAS), the intermediate confining unit, and the Floridan Aquifer System (FAS) with the FAS being the focus of this test well program. For the Middle Rio Grande-Santa Fe Group aquifer system, the in- formation needed to formulate sustainable policies requires a reliable quantitative description of the regional groundwater flow system, in- cluding the hydrogeologic framework as well as patterns and trends in extraction and recharge. tapping the Upper Floridan aquifer southeast of Lake Seminole, Decatur County, Georgia. Well is feet deep and was used in an aquifer-performance test. Photo by Lynn J. Torak, USGS. Typical center-pivot spray-irrigation system used in the lower Apalachicola – Chattahoochee – Flint River Basin, southwestern Georgia.

Glen Canyon aquifer underlying the Sand Flats region. This hydrologic system, referred to as the Glen Canyon Group Mill Creek (GCMC) hydrologic system, was chosen in Phase 2 of the project as the setting for the quantification of the water resources available to the City, resulting in a preliminary global water budget of the GCMC hydrologic system. B R A I N A R D - V A L P A R A I S O A R E A H Y D R O G E O L O G I C A S S E S S M E N T - L P S N R D E X P L O R A T I O N R E S O U R C E S I N T E R N A T I O N A L i Decem Hydrogeologic Assessment and Framework Development of the Aquifers beneath the Brainard-Valparaiso Area of the Lower Platte South Natural Resources District in Eastern. and Smith, ). The hydrogeologic framework underlying the study area consists of Eocene or younger-age rocks and makes up the surficial aquifer system, the intermediate confining unit, and the Flori-dan aquifer system (fig. 2). This multilayered system consists of several permeable zones interbedded with. Four types of bedrock aquifers in 12 water-management basins identified by the Indiana Natural Resources Commission (INRC) in Indiana were identified by the USGS in U.S. Geological Survey Water-Resources Investigations Report (Fenelon and others, ). The source scale of the maps depicting aquifers was , Aquifer maps are based on information from hydrogeologic .

Hydrogeologic framework of the Michigan basin regional aquifier system. Download PDF EPUB FB2

Mississippian and younger geologic units form a regional system of aquifers and confining units in the central Lower Peninsula of Michigan. The area of the regional aquifer system is ab square miles.

The aquifer system consists of three bedrock aquifers, which are separated by Hydrogeologic framework of the Michigan basin regional aquifier system. book units. Bedrock aquifers and confining units are overlain by surficial glaciofluvial aquifers.

Get this from a library. Hydrogeologic framework of the Michigan basin regional aquifer system. [D B Westjohn; T L Weaver]. The Saginaw Aquifer is a bedrock aquifer located in central Michigan in the United States.

It is part of an aquifer system found in Mississippian or younger stratigraphic units in the Michigan Basin.

The aquifer covers approximat square miles (28, km 2) and is estimated to contain 4 cubic miles (17 km 3) of water, approximately 50 feet (15 m) to feet ( m). Get this from a library. Hydrogeologic framework of Mississippian rocks in the central Lower Peninsula of Michigan. [D B Westjohn; T L Weaver; Geological Survey (U.S.); Michigan Basin Regional Aquifer System Analysis.].

Westjohn, D.B. and Weaver, T.L.,Hydrogeologic Framework of the Michigan Basin Regional Aquifer System, U.S. Geological Survey Professional Paper Hydrogeologic framework of the Michigan basin regional aquifer system / by: Westjohn, D.

B., et al. Published: () In old Virginia: slavery, farming, and society in the journal of John Walker / by: Bushman, Claudia L. Published: ().

The Yakima River basin aquifer system underlies about 6, square miles in south-central Washington. The aquifer system consists of basin-fill deposits occurring in six structural-sedimentary basins, the Columbia River Basalt Group (CRBG), and generally older bedrock.

The basin-fill deposits were divided into 19 hydrogeologic units, the CRBG was divided into three. Synthesis of hydrogeologic, hydrochemical, and isotopic data suggests that an area of at least 4, square miles (including 10 intermontane valleys) is hydraulically integrated into one ground-water basin, the Ash Meadows basin, by interbasin movement of ground water through the widespread carbonate aquifer.

Geologic units that form the Michigan Basin regional aquifer system are Early Mississippian through Jurassic age bedrock units, and unconsolidated glacial deposits of Pleistocene age. The aquifer system consists of six formations that have formal stratigraphic names and three geologic units that have informal names (figs.

2 and 3). The Michigan Basin is also an important area for underground waste injection including brine disposal into deep saline aquifers.

Current work suggests that the Michigan Basin has the potential for significant CO 2 sequestration in deep saline aquifers. Detailed Description. Hydrogeologic Framework of the Long Island Aquifer System: The figure above shows a hydrologic section of the Long Island aquifer system in western Nassau County, NY as delineated by Smolensky and others in This framework was developed using existing driller’s logs and well records.

aquifer system has been characterized as: (1) strongly influenced by primary framework geologic controls (intraflow structure, stratigraphy, folds, faults, and feeder dikes) and strataform, or layered, in nature resulting in stratigraphic and cross‐strata controls and.

Delineation of the Hydrogeologic Framework of the Big Sioux Aquifer near Sioux Falls, South Dakota, Using Airborne Electromagnetic Data By Kristen J. Valseth, Gregory C. Delzer, and Curtis V.

Price Big Sioux River Big Sioux River Big Sioux River TUM IS GEODETIC REFERENCE SYSTEM TION x10 NE SW METERS Sioux Quartzite. Hydrogeologic framework of the study area. (A) Bedrock geology map of Paleozoic basins in the Great Lakes region of the United States, highlighting regional aquifers and shale confining units in relation to Pleistocene glacial limits.

Hydrogeologic properties of Michigan Basin aquifer systems and confining units used in the mathematical. in the basin include reports on the hydrogeology of Delaware County (Hoggatt and others, ), Madison County (Wayne, ), Marion County (Herring, ), and Hamilton County (Gillies, ).

The study by Gillies () included modeling of an aquifer system adjacent to the White River near Carmel, Ind., and evaluation of the effects. A study of the water resources of the unconsolidated groundwater system of the Chamokane Creek basin was conducted to determine the hydrogeologic framework, interactions of shallow and deep parts of the groundwater system with each other and the surface-water system, changes in land use and land cover, and water-use : Sue C.

Kahle, William A. Taylor, Sonja Lin. Hydrogeologic Framework of the Michigan Basin Regional Aquifer System: Hydrogeologic Framework of the Michigan Basin Regional Aquifer System: Citing Books via.

Google Scholar. Related Articles. Detrital zircons from fluvial Jurassic strata of the Michigan basin: Implications for the transcontinental Jurassic paleoriver hypothesis: REPLY.

Hydrogeologic framework of bedrock units and initial salinity distribution for a simulation of groundwater flow for the Lake Michigan Basin by: Lampe, David C.

Published: () Hydrogeologic framework and geochemistry of ground water and petroleum in the Silurian-Devonian carbonate aquifer, south-central Louisville, Kentucky Published: (). Hydrogeologic Framework of the Michigan Basin Regional Aquifer System - Physical and chemical data for ground water in the Michigan basin - Nomenclature of geologic units in the Michigan Basin - Stratigraphic relations of the Parma Sandstone and Saginaw Formation: Basal Pennsylvanian sandstones in the Michigan Basin.

Hydrogeologic Framework of The Michigan Basin Regional Aquifer System HN Geologic Studies in Alaska by the U.S. Geological Survey, JULIE IN JOHN Ground -Water Hydrology and Simulated Effects of Development in the Milford Area, An Arid Basin in Southwestern Utah MEHMET CELEBI The. Westjohn, D.B., and Weaver, T.L.,Hydrogeologic framework of the Michigan Basin regional aquifer system: U.S.

Geological Survey Professional Paper47 p. 1 Terms defined in the glossary are in bold print where they are first used in the main body of the report. Developing a 3D Hydrogeologic Framework Development and testing of a regional hydrogeologic framework Permian- Pennsylvanian- and Mississippian-age aquifers of the Appalachian Plateaus cover portions of seven states and contains large amounts of coal, oil, and gas reserves with a long history of production.

This presentation describes development of a digital hydrogeologic‐framework model of basin‐fill and bedrock aquifer systems in the San Francisco River (SFrnRv) basin of the west‐central New Mexico border region. The SFrnRv is the only perennial tributary to the Upper Gila River, with a confluence.

Hydrogeologic Assessment and Simulation of Stream-Aquifer Relations in the Lower Apalachicola-Chattahoochee-Flint River Basin. Project Chief: Lynn Torak Cooperators: Georgia Department of Natural Resources, Environmental Protection Division Year started: THIS PROJECT HAS BEEN COMPLETED AND IS BEING ARCHIVED IN ITS FINAL.

Hydrogeologic Framework and Estimates of Ground-Water Volumes in Tertiary and Upper Cretaceous Hydrogeologic Units in the Powder River Basin, Wyoming By Kurt Hinaman The PDF for the report is 4, kb Table of Contents. Abstract. Introduction. Hydrogeologic Framework. Methods Used to Estimate Ground-Water Volumes.

Estimates of Ground-Water. hydrogeologic report that meets the requirements of this rule. The hydrogeologic study should: 1) Describe the regional hydrogeologic conditions. 2) Identify whether the discharge will occur within a designated wellhead protection area. 3) Determine whether the discharge is to a usable aquifer, an unusable aquifer, or groundwater not in an aquifer.

The files listed below are supplemental to the USGS SIR SIR – titled “Hydrogeologic Framework of the Uppermost Principal Aquifer Systems in the Williston and Powder River Structural Basins, United States and Canada” and should not be used without an understanding of what the files represent.

The model domain was laterally bound by a continuous specified‐head boundary, formed from lakes Michigan, Huron, St. Clair, and Erie, with the St. Clair and Detroit River connecting channels. The model was developed to quantify regional ground water flow in the aquifer systems using independently determined recharge estimates.

The sedimentary rock aquifers are good storage areas that can be drilled for domestic and industrial water supplies. Because the sandstone and porous limestone layers of Michigan are in a saucerlike basin (i.e., the Michigan Basin), most of the Lower Peninsula does have the potential for springs and artesian, or naturally flowing, wells.

As the. The relation of major aquifers and aquitards along basin margins is an important control on fluid migration. Figure 4 compares the hydrostratigraphy of regional aquifers and aquitards in the Illinois and Michigan basins, highlighting the Late Devonian black shales.

Along the eastern margin of the Illinois Basin, the New Albany Shale is a regional confining unit. Howard W. Reeves is a Research Hydrologist with the U.S. Geological Survey (USGS) in the Michigan-Ohio Water Science Center. Recent work includes regional assessment of groundwater availability for the U.S.

Great Lakes Basin and the glacial aquifer system.following sections describe the hydrogeologic framework used. much as 1, ft where the units dip into the Michigan Basin. the regional sandstone aquifer system were based on .The Michigan Basin aquifer system is a major source of ground water in the central Lower Peninsula of Michigan.

Ground-water flow in the aquifer system is directly linked to areal recharge, stream baseflow, and Great Lakes direct riparian discharge. An initial simulation of the RASA study area assumed a fixed water table.