Hydrogeology of shallow groundwater resources, Aurora and vicinity, Kane County, Illinois by Timothy H. Larson

Cover of: Hydrogeology of shallow groundwater resources, Aurora and vicinity, Kane County, Illinois | Timothy H. Larson

Published by Illinois State Geological Survey in Champaign, Ill .

Written in English

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Subjects:

  • Hydrogeology,
  • Groundwater

Edition Notes

Book details

Other titlesAurora and vicinity, Kane County, Illinois.
StatementTimothy H. Larson, Stephen S. McFadden, [and] Robert H. Gilkeson
SeriesOpen file series (Illinois State Geological Survey) -- 1991-12., Open file series (Illinois State Geological Survey) -- 1991-12.
ContributionsMcFadden, Stephen S., Gilkeson, Robert S., Illinois State Geological Survey
The Physical Object
Pagination19 p. :
Number of Pages19
ID Numbers
Open LibraryOL25458675M
OCLC/WorldCa28229653

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Books. An illustration of two cells of a film strip. Video An illustration of an audio speaker. Hydrogeology of shallow groundwater resources, Aurora and vicinity, Kane County, Illinois Item Preview remove-circle Share or Embed This : CONTENTS EXECUTIVESUMMARY 1 OVERVIEW 1 METHODS 1 FINDINGSOFTHEINVESTIGATION 2 LocationofWater-BearingDeposits 2 ACKNOWLEDGMENTS 4.

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HydrogeologyofShallowGroundwaterResources Geneva-BataviaTownship,KaneCounty,Illinois en on III' SU^V'eJ. Hydrogeology of shallow groundwater resources in the vicinity of St. Charles, Kane County, Illinois (Open file series) [Morse, Walter J] on *FREE* shipping on qualifying offers.

Hydrogeology of shallow groundwater resources in the vicinity of St. Charles, Kane County, Illinois (Open file series). OF SHALLOW GROUND-WATER RESOURCES IN KANE COUNTY, ILLINOIS by Adrian P. Visocky Prepared for Kane County, Illinois Illinois State Water Survey Griffith Drive Champaign, Illinois November An illustration of an open book.

Books. An illustration of two cells of a film strip. Video. An illustration of an audio speaker. Hydrogeology of shallow groundwater resources: Geneva-Batavia Township, Kane County, Illinois Item Preview remove-circle Share or Embed This Item.

ation of groundwater resources in buried bedrock valleys, northeastern Illinois: Proceed- ings of the Focus Conference on Midwestern Ground Water Issues, National Water Well Association, p. – Full text of "Hydrogeology of shallow groundwater resources: Geneva-Batavia Township, Kane County, Illinois" See other formats Uf^S^O^LM Hydrogeology of Shallow Groundwater Resources Geneva-Batavia Township, Kane County, Illinois Timothy H.

Larson Stephen S. McFadden Robert H. Gilkeson f Open File Series • ILLINOIS STATE GEOLOGICAL SURVEY V^ Morris W. to begin searching for sites for shallow high-capacity wells. The Major Quaternary Aquifers, Kane County, Illinois (Dey et al.

) is intended to be used for county-scale planning and as guide to exploration for develop-ing shallow groundwater resources. This map should not be used as a substitute for site-specific work. This report discusses an assessment of groundwater resources supplying water to Kane County, Illinois, a rapidly growing county on the west side of the greater Chicago metropolitan area.

This study assimilates the available data into a set of computer models of groundwater flow in regional and local aquifers, quantifying the components of the.

Internet Archive BookReader Hydrogeology of shallow groundwater resources in the vicinity of St. Charles, Kane County, Illinois. Several aquifers underlying Campton Township in Kane County, Illinois provide virtually all of the water supply to the residents of the township.

These aquifers consist of layers of unconsolidated sand and gravel in the glacial drift; dolomite and shale of the Alexandrian Series and the Maquoketa Group (the Silurian-Maquoketa aquifer); dolomite of the Platteville and Galena Groups (the Galena. Kane County supports the efforts of CMAP to implement the "Northeastern Illinois Regional Water Supply/Demand Plan - Water ", reinforces the water resource recommendations in the CMAP "Go to Plan", and emphasizes the need to integrate water resources with land use decision-making in the 11 county Northeastern Illinois Regional Water.

Hydrogeology, Water Use, and Simulated Ground-Water Flow and Availability in Campton Township, Kane County, Illinois. Scientific Investigations Report —ONLINE ONLY.

By Robert T. Kay, Leslie D. Arihood, Terri L. Arnold, and Kathleen K. Fowler. View Report. and thickness for each bedrock unit in the study area.

For example, figure 1 Hydrogeology of shallow groundwater resources, Kane County, Illinois: Illinois State Geological Survey, Contract/Grant Report37 p. Dey, W.S., A.M. Davis, C.C. Abert, B.B. Curry, and J.C. Sieving,Aurora Virgil Elburn West Dundee Sleepy Hollow.

The USGS annually monitors groundwater levels in thousands of wells in the United States. Groundwater level data are collected and stored as either discrete field-water-level measurements or as continuous time-series data from automated recorders. Data from some of the continuous record stations are relayed to USGS offices nationwide through telephone lines or by satellite transmissions.

Mapping Shallow Groundwater Levels in Kane County, Illinois Randall A. Locke II, P.G., Illinois State Water Survey, Center for Groundwater Science Figure 1.

Study Area Figure 2. Well Network Figure 4. High-capacity wells in Kane County Figure 5. Shallow bedrock aquifer head surface Figure 3. Shallow geologic materials in the study area. Kane County Government Center S.

Batavia Ave, Bldg A Geneva, IL Description of Study Area Kane County (Figure 1) is located in northeastern Illinois and shares borders with several other counties: north (McHenry County), west (De Kalb County), south (Kendall County), and east (Cook and DuPage Counties).

Aurora, the largest city in Kane County, also includes portions of DuPage, Kendall, and Will Counties. Water Resources of Kane County. There are two groundwater aquifers below the ground surface in Kane County.

The shallow aquifer formations are generally from 5 to about feet below the ground surface and consist of sands, gravels and the upper portions of fractured limestone or shale bedrock. A major study funded by Kane County and several communities produced a regional perspective of the shallow groundwater resources in the vicinity of the study area.

Much of the technical background provided in the final report for the Kane County project (Curry and Seaber ) is pertinent to Geneva-Batavia Township and thus is referenced in. Brunswick County is the southernmost coastal county in North Carolina and lies in the southeastern part of the Coastal Plain physiographic province.

In this report, geologic, hydrologic, and chemical data were used to investigate and delineate the hydrogeologic framework and ground-water quality of Brunswick County.

The major aquifers and their associated confining units delineated in the. Hydrogeology and Simulation of Groundwater Flow in Sauk County, Wisconsin Bulletin Hydrogeology and Simulation of Groundwater Flow in Sauk County, Wisconsin Madeline B.

Gotkowitz Kurt K. Zeiler Charles P. Dunning Judith C. Thomas Yu-Feng Lin Wisconsin Geological and Natural History Survey Bulletin | Baseline conditions for the sand and gravel aquifers (groundwater) in McHenry County, Illinois, were assessed using data from a countywide network of 44 monitoring wells collecting continuous water-level data from – Inwater-quality data were collected from 41 of the monitoring wells, along with five additional monitoring wells available from the U.S.

Geological Survey National. forms. Thiel (, p. ) described the occurrence of ground water in the glacial and bedrock formations in St. Louis County and gave the log of an Aurora city well that penetrated the iron-formation.

Cotter and Rogers () described the glacial geology and ground- water resources near Virginia, about 15 miles west of Aurora. The most important sources of groundwater in Bradford, Tioga, and Potter Counties are the stratified-drift aquifers.

Saturated sand and gravel primarily of outwash origin forms extensive unconfined aquifers in the valleys. Outwash is underlain in most major valleys by silt, clay, and very fine sand of lacustrine origin that comprise extensive confining units.

In order to continue Groundwater Watch operations after SeptemUSGS Water Resources Mission Area migrated Groundwater Watch off of non-compliant servers.

Because of limitations of the software components and the underlying hardware, the migration to the new infrastructure required a reduction in the number of networks served. Water Resources Specialist McHenry County Department of Planning & Development % G.

ROUNDWATER. Groundwater is stored in. underground aquifers: • Sand and Gravel • Limestone (shallow bedrock) Sandstone (deep bedrock) Constant, clean discharge flows, year round to sustain stable surface water hydrology with constant water. al chemistry of ground water determine the availability and suitability of ground-water resources for specific uses.

Ground-Water Resources Ground water is the part of precipitation that enters the ground and percolates downward through unconsolidated materials and openings in bedrock until it reaches the water table (figure 8).

The water table. Pleistocene Stratigraphy of Island County and Groundwater-Resources of Island County. USGS OFR, D.R. Cline, M.A. Jones, etal. Preliminary Survey of Ground-Water Resources for Island County, Washington. USGS WRIR, M.A. Jones. Occurrence of Ground Water and Potential for Seawater Intrusion, Island County, Washington.

Hydrogeology of parts of Pinellas County 4 Surficial aquifer system 4 Intermediate confining unit 5 Floridan aquifer system 5 Zone A 5 Semiconfining unit between zones A and B 6 Zone B 7 Water-quality data 8 Potential for development of brackish ground-water resources 8 Simulation of the effects of development on the quality of ground water.

Navajo Lake, whose entire outflow disappears underground, is on the high Markagurit Plateau where the average annual precipitation is more than 30 inches. It nestles among the headwaters of several streams that flow into arid regions where competition for municipal, industrial, and irrigation water sup- plies is very keen.

Several proposals for additional development and use of the water of. Hydrogeology of shallow basin-fill deposits in areas of Salt Lake Valley, Salt Lake County, Utah. U.S. GEOLOGICAL SURVEY was done from to in areas in which shallow ground water has the potential to move to a deeper aquifer that is used for public supply.

Thirty monitoring wells were drilled and sampled in as part of the study. A ground-water flow model of the shallow aquifer in the study area was developed using his­ torical data and the hydrologic data collected for this study.

The model quantified the water budget for the shallow aquifer in the study area. Aquifer properties were estimated for each cell, based on analysis of drillers' logs frorrrlrrigation wells and.

Groundwater Data. NEWS! Island County Well Data is now available via an Online Well-Viewer Application. With this application you can view wells in an area. Clicking on any well provides a link to more information about the well, including scanned well logs, water level, water quality (chemistry) and public water system information (where applicable and available).Hydrogeology, Water Use, and Simulated Ground-Water Flow and Availability in Campton Township, Kane County, Illinois By Robert T.

Kay, Leslie D. Arihood, Terri L. Arnold, and Kathleen K. Fowler.• The quality of shallow groundwater in most of Kane County is still good • Groundwater quality in the Eastern urban corridor of Kane County is degraded, and it has gotten worse since • Road salt runoff continues to be the major source of contamination that is increasing the salinity of groundwater.

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