Ohio Department of Natural Resources Paul N Spahr 4/01/2000 vector digital data withheld ODNR_Glacial_Aquifers Unconsolidated Aquifers of Ohio Polygon coverage depicting the geographic extent, yield, drift thickness, hydrogeologic setting, lithology, and aquifer name for the unconsolidated aquifers of Ohio To define, evaluate, quantify and delineate the ground water resources of the sand and gravel aquifers of Ohio en The year (and optionally month, or month and day) for which the data set corresponds to the ground. REQUIRED. The basis on which the time period of content information is determined. REQUIRED. Complete Unknown -84.918183 -80.479651 41.993654 38.380145 1310321.825853 2518356.534434 146827.812505 1455119.108955 Reference to a formally registered thesaurus or a similar authoritative source of theme keywords. REQUIRED. Unconsolidated Aquifers glacial aquifer ONDR lithology drift thickness yields Restrictions and legal prerequisites for accessing the data set. REQUIRED. Restrictions and legal prerequisites for using the data set after access is granted. REQUIRED. Mike P Hallfrisch Ohio Department of Natural Resources Supervisor mailing address

Division of WATER Water Resources 1939 Fountain Square

COLUMBUS OH 43224 USA 614-265-6745 614-265-6767 mike.hallfrisch@dnr.state.oh.us Ohio Department of Natural Resources, Paul N Spahr ESRI ArcCatalog 9.0.0.535 File Geodatabase Feature Class ODNR, Div of Water, 4/1/00 v ODNR, Div of Water, 4/01/2000 map various scales ODNR, Div of Geo Survey, 4/01/2000 map map scale 1:24,000 Metadata imported. withheld Metadata imported. withheld Metadata imported. withheld 20050321 15243100 Vector G-polygon 6262 Label point 6263 GT-polygon composed of chains 6262 Point 946 Simple Polygon FALSE 6262 TRUE FALSE coordinate pair 0.002048 0.002048 survey feet State Plane Coordinate System 1983 3402 38.733333 40.033333 -82.500000 38.000000 1968500.000000 0.000000 North American Datum of 1983 Geodetic Reference System 80 6378137.000000 298.257222 GCS_North_American_1983 NAD_1983_StatePlane_Ohio_South_FIPS_3402_Feet 1.000000 Explicit elevation coordinate included with horizontal coordinates NAME Concatenation of the Local field and the Setting field OEPA.aquifers_glacial_ODNR Feature Class 6262 OBJECTID Internal feature number. ESRI Sequential unique whole numbers that are automatically generated. LITH Primary composition of glacial deposits T= till S=sand G=gravel F=fines(undifferentiated) C = confining Predominant material - Upper case letters, secondary material - lower case letters SGc Primary composition of glacial deposits is sand and gravel with a confining layer Limited to portions of the Great Miami River Valley where the probability of encountering a confining or semi-confining zone within the aquifer is high. Such a confining layer would split the sand and gravel into upper and lower aquifers. The thickness and continuity of the confining layer may vary considerably in the mapped area. Tsg Primary composition of glacial deposits is Till with sand and gravel Predominantly till, contains sand and gravel lenses of varying thicknesses. These lenses may or may not be interconnected. Wells are developed in these lenses. T Primary composition of glacial deposits is Till Predominantly till, water well logs typically lack indication of sand and gravel lenses. Wells are typically finished in the underlying bedrock. Wells commonly are developed at or near the drift/bedrock contact. Shallow dug wells may still be used on a limited basis. Shallow monitor wells may be completed in this unit. Many of these mapped areas are shallow to bedrock; mapping may include small areas where bedrock comes to ground surface. SGt Primary composition of glacial deposits is sand and gravel with till Predominantly sand and gravel with thin covering of till or thin interbedded layers of till. Commonly associated with ice-contact features, i.e. kames, eskers, some moraines, etc. It is also associated where thin beach ridges directly overly till. SGf Primary composition of glacial deposits is snad and gravel with fines Predominantly sand and gravel with minor fines. Typically represents thick sequences of outwash/valley train deposits with minor alluvium, lacustrine deposits, etc. F Primary composition of glacial deposits is fines Fsg Primary composition of glacial deposits is fines with sand and gravel Predominantly fines with sand and gravel lenses. This setting is commonly found in valleys. Fines include alluvium, minor lacustrine (slackwater) deposits, till and colluvium. NA Not applicable - Drift removed, disturbed or not present SG Primary composition of glacial deposits is sand and gravel Predominantly sand and gravel with minor, insignificant fines. Fines may not be reported in well log records. Most common in the Ohio River Valley and Hocking River Valley. THICK Labels for drift thickness(thickcode) THICKCODE Code for drift thickness YIELD Labels for yields of unconsolidated aquifers(yieldcode) < 5 Aquifer yield is less than 5 gallons per minute 5 - 25 Aquifer yield is between 5 and 25 gallons per minute 25 - 100 Aquifer yield is between 25 and 100 gallons per minute 100 - 500 Aquifer yield is between 100 and 500 gallons per minute > 500 Aquifer yield is greater than 500 gallon per minute YIELDCODE Code for aquifer yields 99 Not Applicable - no aquifer presenet 5 Aquifer yield is greater than 500 gallons per minute 4 Aquifer yield is between 100 and 500 gallons per minute 3 Aquifer yield is between 25 and 100 gallons per minute 2 Aquifer yield is between 5 and 25 gallons per minute 1 Aquifer yield is less than 5 gallons per minute LOCAL Delineation of localized aquifers Alliance Large area in northeastern Ohio, primarily in Mahoning, Trumbull, and Stark Counties. A relatively flat-lying upland area. Very clayey till with minor sand and gravel lenses. Commonly shallow (<25') or moderate (25-100') to bedrock. Wells finished in sand and gravel lenses have low (<5gpm) to moderate (5-25gpm) yields. Alum Creek Alum Creek Tributary of the Scioto River in Delaware and Franklin Counties. To the north is an alluvial aquifer containing predominantly fines with some sand and gravel. Moderate thickness (25-100') and low to moderate yields (5-25 gpm). To the south the deposits thicken, becoming a buried valley setting. Deposits become coarser and yields increase significantly to the south. Amanda Amanda Small area in southwestern Fairfield County. Area is a thick drift complex containing mostly dense till with minor sand and gravel lenses. Yields range from 5-25 gpm to 25-100 gpm. Complex is a tributary to the much larger Baltimore buried valley system. Anderson Large area in southwestern Ohio. An upland area to the east of Cincinnati and between the Ohio River and East Fork. Includes parts of Clermont, Brown, and Adams Counties. An upland area of thin Illinoian-age glacial till and loess. Drift is typically less than 25' thick and yields less than 5 gpm. Apple Valley Apple Valley - Area north and east of the Kokosing River in eastern Knox County and western Coshocton County. To the west the area is ground moraine with 25-100' of till. Yields of 5-25 gpm are developed from thin sand and gravel lenses. To the east, the till thins and the area becomes thin upland settings. The relief increases and yields become less than 5gpm in the thin upland areas. Arcanum Arcanum - Relatively flat-lying area in southwestern Ohio between the Farmersville Moraine and Union City Moraine and west of the Stillwater River. Area covers much of Darke County. The area contains variable thickness of till containing lenses of sand and gravel. Settings in the western part are commonly thick drift complex and thickness averages over 100'. In the central part of the area, ground moraine settings are common and drift ranges from 25-100'. In the eastern part of the area, the drift thins to less than 25' and the setting becomes thin uplands. Yields for most of the area are 5-25 gpm except for where the drift becomes very thin. Auglaize River Auglaize River - Major tributary of the Maumee River which drains much of Allen, Paulding, Van Wert, and Putnam Counties. Drift is typically 25-100' thick. Shallow wells are developed in sandy zones within the fine alluvium. Deeper wells are completed in sand and gravel lenses in the till underlying the alluvium. The streams help to supply additional recharge. Yields typically fall into the 5-25 gpm range. Baltimore Baltimore - A large area of thick drift which extends from Buckeye Lake to the Scioto River in northern Fairfield County and parts of Pickaway and Franklin Counties. The eastern and southern portions are a thick drift complex containing till with lenses of sand and gravel. Yields range from 5-25 gpm to 25-100 gpm. To the west the deposits occupy a major buried valley system. Deposits include fines, till, and thicker sequences of sand and gravel. Yields increase up to 100-500 gpm closer to the Scioto River and Big Walnut. Beavercreek Beavercreek - A small tributary of the northern part of the L. Miami River which occupies a small divide between the Mad River and the L. Miami River. The area is northeast of the town of Fairborn. Thickness averages 25-100'. Shallow wells are developed in sand and gravel zones in the fine-grained alluvium. Deeper wells are finished in sand and gravel lenses in the underlying till. Yields are commonly 5-25 gpm. Bellefontaine Bellefontaine - A large area east of the Mad River which covers a large part of Logan County. This area includes the Bellefontaine Outlier and surrounding areas. Thickness varies considerably; drift is typically thinnest in the southern part where bedrock from the Bellefontaine Outlier is close to the surface. Northwards the area is comprised of ground moraine and thick drift complex, with thickness of 25-100' and greater than 100' respectively. Wells are completed in thin sand and gravel lenses interbedded in the thick till sequences. Yields are commonly 5-25 gpm. Big Darby Big Darby - A major tributary of the Scioto River. The stream extends along much of the Madison Co.-Franklin Co. line into Pickaway County where it merges with the Scioto River. The northern part of the Big Darby consists of alluvial aquifers. Drift thickness is in the 25-100' range and wells are completed in sand and gravel lenses interbedded with fine alluvium or underlying till. Yields are 5-25 gpm or 25-100 gpm. Farther south, drift thickens and the Big Darby overlies buried valley aquifers. Wells are developed in fairly coarse, continuous outwash deposits. Yields up to 100-500 gpm can be developed in these areas. Big Island Big Island - A small, flat-lying, poorly-drained area along the Scioto River in western Marion County. This marshy area was formerly a shallow lake impounded between end moraines. Yields of 5-25 gpm are developed from sandy layers interbedded with silty to clayey lacustrine deposits and till. Drift thickness typically averages 40' to 50'. Comparable to the larger Killdeer Plains located further north. Big Walnut Big Walnut - A tributary of the Scioto River which drains much of eastern Delaware and Franklin Counties. The northern portion of this stream contains alluvial settings. Wells are completed in sand and gravel lenses interbedded in fine alluvium or underlying till. Drift thickness is 25-100' and yields are 5-25 gpm. Further south, the drift thickens and Big Walnut overlies a deep buried valley. Wells are finished in thick, continuous sand and gravel outwash deposits. Yields of 100-500 gpm can be obtained and, near the Scioto River, yields greater than 500 gpm are possible. The Division of Water and USGS have extensive data on these high-yielding aquifers. Black River Black River - A tributary of Lake Erie that drains parts of Medina and Lorain Counties. This local includes the alluvial settings associated with the river and some immediately adjacent short buried valleys and thick drift complexes. In the headwaters, drift roughly averages 40' to 50'. Near the town of Oberlin, the stream roughly follows a buried valley and thick drift complex. Drift averages over 120' in this area. Farther north, the stream reaches the Lake Plain. In this area the floodplain narrows and the drift thins appreciably. Yields throughout the local average 5-25 gpm. Wells are developed in sand and gravel lenses interbedded in the fine alluvium or underlying till. Blanchard River Blanchard River - A tributary of the Auglaize River which flows westward from the town of Findlay into Allen County. The river roughly follows the southern margin of the Defiance Moraine in this area. Drift in this alluvial setting averages between 25-100' thick. Yields are commonly 5-25 gpm. Wells are developed in thin sand and gravel lenses interbedded in the fine-grained alluvium or underlying till. Blanchester Blanchester - An upland area roughly encircled by the L. Miami River and East Fork in central Warren County. The local is predominantly comprised of thin upland settings with thickness ranging from less than 25' of till to 25-100'of till. Yields are less than 5 gpm in these areas. The central part of this area contains one narrow thick drift complex that may have corresponded to an ancestral stream valley. Yields of 5 to 25 gpm are developed from wells completed in thin sand and gravel lenses interbedded in till in this feature. Bloomingburg Bloomingburg - Area which roughly corresponds to the Bloomingburg End Moraine which extends across parts of Madison, Fayette, and Pickaway Counties. Thicknesses are typically in the upper part of the 25-100' thickness range. Yields of 5-25 gpm are derived from thin sand and gravel lenses interbedded in the till. Bokengehalas Bokengehalas - Area lies to the west of the Bellefontaine Outlier and is in the vicinity of Indian Lake. This local is primarily thick drift complex which lies in the drainage divide between the headwaters of the Miami River and the Mad River. Drift thickness varies from 25-100' to greater than 100'. Wells are completed in sand and gavel lenses interbedded in thick sequences of loamy till. Yields range from 5-25gpm to 25-100gpm. Bokes Creek Bokes Creek - Tributary of the Scioto River located in northern Union County. This alluvial setting contains 25-100' of drift. Wells are completed in sand and gravel lenses interbedded in the finer alluvium or the underlying till. Yields are in the 5-25gpm range. Brecksville Brecksville - Large area in northeastern Ohio covering much of Cuyahoga County, Lorain County, and northern Summit County. This area is characterized by steep, highly stream-dissected uplands. The Cuyahoga River, Chagrin River and Rocky River drain this area. Clayey till commonly forms a thin cover over the highly eroded shale bedrock. Yields are generally less than 5gpm. In a few areas where drift is in the 25-100' range, wells completed in thin sand lenses may yield 5-25gpm. Broadway Broadway - Area in northern Union and Delaware Counties which roughly corresponds to the Broadway End Moraine. Drift in this feature is in the upper part of the 25-100' range and is much thicker than in the surrounding ground moraine and thin uplands. Wells are completed in thin sand and gravel lenses interbedded in the clayey till. Yields are in the 5-25 gpm range. Cable Cable - Area in eastern Champaign and Clark Counties which roughly corresponds to the Cable End Moraine. This area forms a thick drift complex along the eastern margin of the Mad River buried valley system. In the northern part of the local, the drift ranges from the thicker end of the 25-100' range to just over 100' thick. Wells are completed in thin sand and gravel lenses interbedded in till. Yields are in the 5-25gpm range. Farther south the thickness increases to well over 100'. Sand and gravel layers become thicker, more abundant, and more continuous. Yields average in the 25-100gpm range. Caesar Ck Caesar Ck - A major tributary of the L. Miami River which drains parts of Greene, Warren, and Clinton Counties. Shallow wells are completed in thin sand and gravel lenses interbedded in the finer alluvium. Yields tend to be in the 5-25 gpm range. Deeper wells are finished in thin sand and gravel lenses interbedded in the underlying loamy till. Yields in these wells typically are in the 5-25 gpm range. Camden Camden - Area in southern Preble County which roughly corresponds to the Camden End Moraine. The local is primarily end moraines with some thick drift complex. Drift thickness is commonly greater than 100' or in the upper part of the 25-100' range. The drift in the moraine is commonly much thicker than in adjacent ground moraine and thin upland settings. Wells are developed in thin sand and gravel lenses interbedded in thick loamy till. Yields are commonly 5-25gpm. Captina Creek Captina Creek - Small tributary of the Ohio River which drains southern Belmont County. Drift thickness is commomnly les than 25'. Minimal yields may be obtained from the fine-grained alluvium in the floodplain. Chagrin Chagrin - An important tributary of Lake Erie in eastern Cuyahoga County and western Geauga County. The Chagrin River flows over highly variable thickness of drift and occupies various settings. The local includes both buried valley and alluvial settings and some adjacent areas of thick drift complex. For alluvial areas, drift is generally in the 25-100' range but is less than 25' in some narrow, bedrock- dominated areas. Drift is over 100' thick in the buried valley and neighboring thick drift complex areas. Shallow wells are developed in sand and gravel lenses interbedded with the alluvium. Yields are commonly 5-25 gpm. Deeper wells are developed in sand and gravel units in the underlying till or lacustrine materials. In some areas, the sand and gravel layers are thicker and more laterally extensive. Yields in these areas range from 25-100 gpm . Chardon Chardon - Large area covering most of Geauga County and portions of Portage and Lake Counties. The local is characterized by steep, highly dissected topography dominated by resistant sandstone ridges. Drift thickness is usually less than 25'.The sandy till is typically very thin and highly-weathered. Yields are less than 5gpm, some yield may be obtained at the till/bedrock interface. In some of the less steep valleys, drift thickness ranges from 25-100'. Yields of 5-25gpm may be obtained from sand and gravel lenses in these thicker sequences. Chillicothe Chillicothe - Upland area in central Ross County which is highly dissected by Paint Ck and it's tributaries. The area is characterized by steep bedrock uplands. The till is typically thin, less than 25'. Yields are typically less than 5 gpm if wells can be developed at all. Drift in some of the less steep valleys is in the 25-100' thickness range. Small yields are available from thin sand lenses interbedded in weathered till, colluvium, or lacustrine sediments. Chippewa Chippewa - A large tributary of the Tuscarawas River which drains southern Medina County and northern Wayne County. The local is primarily part of a large buried valley system. Drift thickness is commonly greater than 100' with some tributaries in the 25-100' thickness range. In tributary valleys, wells are completed in sand and gravel lenses interbedded in finer alluvium or underlying till. Yields for these wells are in the 5-25 gpm or 25-100'gpm range. In the large trunk valleys, thick sequences of sand and gravel outwash provide yields of 100-500 gpm to greater than 500gpm for large diameter, properly-constructed wells. Test drilling may be necessary to determine the best-yielding deposits. Coldwater Coldwater - An area in southern Mercer County in the vicinity of Grand Lake St. Mary's. The local is just north of the St. Johns Moraine and is divided by the main trunk of the Teays River Valley. The local is characterized by flat-lying ground moraine which has an average thickness midway in the 25-100' range. Portions adjacent to the Teays River Valley system have greater than 100' of drift and are considered to be thick drift complexes. Wells are finished in sand and gravel lenses which are interbedded in thick sequences of clayey till. Yields are commonly in the 5-25gpm range. Conotton Cr Conotton Cr - A tributary of the Tuscarawas River which drains parts of Tuscarawas, Caroll, and Harrison Counties. A broad, trunk buried valley underlies much of the modern stream. Thinner, alluvial aquifers are found in tributary valleys and in the headwaters. Shallow wells are completed in sand and gravel lenses interbedded in finer alluvium. Deeper wells are completed in sand and gravel lenses interbedded in older floodplain, colluvial, and lacustrine deposits. Yields are usually 5-25 gpm. Cross Creek Cross Creek - A tributary of the Ohio River which flows just south of Steubenville in central Jefferson County. The stream contains alluvial deposits in the lower part of the 25-100' range. Yields of 5-25gpm are obtained from wells completed in sandy layers interbedded with the finer alluvial deposits. Cuba Cuba - An area roughly corresponding to the Cuba End Moraine which extends across Greene, Clinton, and Highland Counties. The moraine typically has over 100' of drift or is in the upper part of the 25-100' range. The moraine contains appreciably thicker drift than the surrounding ground moraine and thin upland areas. Wells are completed in thin sand and gravel lenses interbedded with thick sequences of silty till. Yields are usually in the 5-25 gpm range. Cuyahoga Cuyahoga - An extremely variable local which occupies much of northeastern Ohio. The local includes both current and ancestral channels and tributaries of the Cuyahoga and Little Cuyahoga Rivers. Included are areas of alluvial, buried valley, and thick drift complexes. Smaller tributaries are typically alluvial settings containing less than 25' of drift to 25-100' of drift. Yields in these areas vary from less than 5 gpm to 5-25gpm depending upon the availability of sand and gravel lenses within the finer alluvium. The composition of the thick drift in the buried valley and thick drift complex settings is highly variable. In central Geauga and western Portage Counties, the buried valley deposits contain thick sequences of sand and gravel outwash. Yields for larger diameter wells range from 100-500 gpm to greater than 500gpm. In northern Summit County and southern Cuyahoga County, the present and ancestral channels of the Cuyahoga are filled with thick sequences of very fine-grained till, lacustrine, and colluvium. Yields are commonly less than 5gpm or in the lower 5-25gpm range. Near the mouth of the Cuyahoga River in Cleveland, the deposits begin to coarsen. Fine-grained sands near the surface yield 5-25 gpm to 25-100gpm. Thicker sand and gravel may be encountered at greater depths. Test drilling is needed to locate the best of these deposits, which may yield up to 100-500 gpm. The Division of Water and the USGS have abundant information on these aquifers, especially in Portage County. Deer Ck Deer Ck - A tributary of the Scioto River which drains parts of Madison, Pickaway, and Ross Counties. The main trunk part of the stream overlies a buried valley containing over 100' of drift in most segments. In the northern end of the valley, wells are developed in sand and gravel lenses interbedded in finer alluvium or the underlying till. Yields are 5-25 gpm to 25-100gpm. Further south, closer to the confluence of the Scioto River, layers of sand and gravel outwash become thicker and more laterally extensive and yields increase to 25-100 gpm and 100-500 gpm. Tributaries and the headwaters of Deer Ck are alluvial settings containing 25-100' of drift. Yields of 5-25 gpm are obtained from thin sand and gravel lenses interbedded with finer alluvium or underlying till. Defiance Defiance - An area which corresponds to the Defiance End Moraine in parts of Putnam, Hancock, Seneca, and Huron Counties. The moraine separates the Lake Plain to the north and the thinner drift in the ground moraine and thin drift uplands to the south. The moraine contains relatively thick (upper portion of the 25-100' range to greater than 100' of drift) clayey till. Wells are developed in thin sand and gravel lenses interbedded in the till. Yields are usually in the 5-25 gpm range. E. Columbus E. Columbus - Area flanking the eastern margin of the Scioto River Valley in eastern Franklin County. Drift in this local is typically greater than 100'. To the north, the local is a thick drift complex setting containing thick sequences of till and minor lenses of sand and gravel. Yields developed from these lenses are in the 5-25 gpm to 25-100gpm range. Further south, the local is part of a buried valley system which contains relatively thick sequences of sand and gravel underlying the till. Wells completed in these sequences develop up to 100-500 gpm. E. Delaware E. Delaware - Area in northern Franklin County and southern Delaware County which is to the east of the Olentangy River and west of the Powell Moraine. The local is roughly split in half by northern Alum Creek. The local is a combination of thin drift upland and ground moraine settings. Drift is usually less than 25' thick or in the lower end of the 25-100' range. Yields are typically less than 5gpm. Isolated sand and gravel lenses provide up to 5-25 gpm. Eagle Creek Eagle Creek - Minor tributary of the Ohio River in southern Brown and Adams Counties. Drift in this alluvial setting is commonly less than 25' to the lower end of the 25-100' range. Yields of 5-25 gpm are obtained from thin sand lenses interbedded in the fine alluvium. East Fork East Fork - Major tributary of the L. Miami River which drains most of Clermont County. Drift in this alluvial setting is usually in the 25-100' range. Near the confluence with the L. Miami River, East Fork overlies a buried valley with a drift thickness greater than 100'. Further from the confluence, yields of 5-25 gpm are developed from wells completed in sand and gravel lenses interbedded in the finer alluvium or underlying till. Near the confluence, the sand and gravel lenses become thicker and more continuous, yields increase to 25-100 gpm. Eaton Eaton - Area in central Preble County located to the north of the Camden End Moraine and south of the Farmersville End Moraine. Sevenmile Creek divides the area in half. Local contains ground moraine and thick drift complex settings. Drift thickness is 25-100' to the north and greater than 100' to the south. Yields of 5-25 gpm are derived from sand and gravel lenses interbedded in thick sequences of loamy till. Esboro Esboro - Area in Fayette County which roughly corresponds to the Esboro End Moraine. This local also includes the ground moraine between the Esboro End Moraine and the Bloomingburg End Moraine to the east. Drift thickness in the end moraine and thick drift complex settings within this local are commonly greater than 100'. Thickness in the ground moraine areas is within th 25-100' range. Yields of 5-25 gpm are developed from wells completed in sand and gravel lenses interbedded with till. Fairborn Fairborn - Area on the east side of the City of Dayton, southeast of the G. Miami River and Mad River. Local includes both ground moraine and thick drift complex settings with drift thickness of 25-100' and greater than 100' respectively. Yields of 5-25 gpm to 25-100gpm are derived from sand and gavel lenses interbedded with the till. Farmersville Farmersville - Area roughly corresponding to the Farmersville End Moraine as it extends across Preble and Montgomery Counties. The local is divided roughly in half by Twin Creek. The local contains both end moraine and thick drift complex settings with drift thickness ranging from 25-100' to greater than 100' respectively. Drift thickness and yields tend to increase east of Twin Creek. Yields vary from 5-25 gpm to 25-100gpm depending upon the thickness and extent of sand and gravel lenses interbedded within the till. Federal Creek Federal Creek - Tributary of the Hocking River in northeastern Athens County. Drift in this alluvial Findlay Findlay - Thin upland area located in central Hancock County near the city of Findlay. Entire local is Fort Ancient Fort Ancient - Area lying between the Cuba End Moraine and the L. Miami River in eastern Warren County Four Mile Ck Four Mile Ck - A tributary of Sevenmile Ck and G. Miami River in the vicinity of Oxford in northwestern Frankfort Frankfort - Area in northwestern Ross County that is transitional between the thicker drift of the SETCODE Code for hydrogeologic settings 2 Ground Moraine hydrogeologic setting 8 Outwash/Kame hydrogeologic setting 7 Beach Ridge hydrogeologic setting 6 Alluvial hydrogeologic setting 5 Thin Upland hydrogeologic setting 10 Valley Fill hydrogeologic setting 3 End Moraine hydrogeologic setting 99 Not Applicable - Non glaciated, no aquifer 1 Buried Valley hydrogeologic setting 4 Lacustrine hydrogeologic setting 9 Complex hydrogeologic setting SHAPE I Coordinates defining the features. Shape Shape Geometry 0 0 0 Feature geometry. ESRI Coordinates defining the features. AREA AREA Double 8 0 0 LEN LEN Double 8 0 0 SETTING Labels for hydrogeologic settings(setcode) Valley Fill Valley Fill Hydrogeological Setting Ground Moraine Ground Moraine Hydrogeological Setting Thin Upland Thin Upland Hydrogeological Setting Outwash/Kame Outwash/Kame Hydrogeological Setting Lacustrine Lacustrine Hydrogeological Setting End Moraine End Moraine Hydrogeological Setting Complex Complex Hydrogeological Setting Buried Valley Buried Valley Hydrogeological Setting Beach Ridge Beach Ridge Hydrogeological Setting Alluvial Alluvial Hydrogeological Setting NA Not Applicable (non glaciated, no aquifer) Shape_Length Shape_Length Double 8 0 0 Length of feature in internal units. ESRI Positive real numbers that are automatically generated. Shape_Area Shape_Area Double 8 0 0 Area of feature in internal units squared. ESRI Positive real numbers that are automatically generated. Downloadable Data The Ohio Department of Natural Resources (DNR) provides this geographic data "as is." DNR makes no guarantee or warranty concerning the accuracy of information contained in the geographic data. DNR further makes no warranties, either expressed or implied, as to the condition of the product, or its fitness for any particular purpose. The burden for determining fitness for use lies entirely with the user. Although these data have been processed successfully on computers of DNR, no warranty, expressed or implied, is made by DNR regarding the use of these data on any other system, nor does the fact of distribution constitute or imply any such warranty. In no event shall the DNR have any liability whatsoever for payment of any consequential, incidental, indirect, special, or tort damages of any kind, including, but not limited to, any loss of profits arising out of use of or reliance on the geographic data. ARCE no compression applied 16.426 Local area network 20050321 The organization responsible for the metadata information. REQUIRED. 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FGDC Content Standards for Digital Geospatial Metadata FGDC-STD-001-1998 local time http://www.esri.com/metadata/esriprof80.html ESRI Metadata Profile en http://www.esri.com/metadata/esriprof80.html ESRI Metadata Profile 20190821 11161000 FALSE 20070827 06292000 20070827 06292000 1.0 ISO 19139 Metadata Implementation Specification ESRI ArcCatalog 9.2.1.1332 ODNR_Glacial_Aquifers 1310321.825853 2518356.534434 1455119.108955 146827.812505 1 -84.918183 -80.479651 41.993654 38.380145 1 ISO 19115 Geographic Information - Metadata DIS_ESRI1.0 dataset 002 withheld Local Area Network File Geodatabase Feature Class NAD_1983_StatePlane_Ohio_South_FIPS_3402_Feet 6262 20070827