Web map of roadway data for Bowie, Cass, Delta, Franklin, Hopkins, Lamar, Morris, Red River, and Titus Counties within Texas, and Miller County, Arkansas.For questions, problems, or more information, contact gis@atcog.orghttps://atcog.org/

Municipal and county park polygon data for Bowie, Cass, Delta, Franklin, Hopkins, Lamar, Morris, Red River, and Titus Counties within Texas and Miller County, Arkansas.For questions, problems, or more information, contact gis@atcog.orghttps://atcog.org/

Map of city limits data for Bowie, Cass, Delta, Franklin, Hopkins, Lamar, Morris, Red River, and Titus Counties within Texas and Miller County, Arkansas.For questions, problems, or more information, contact gis@atcog.orghttps://atcog.org/

Road polyline data for Bowie, Cass, Delta, Franklin, Hopkins, Lamar, Morris, Red River, and Titus Counties within Texas and Miller County, Arkansas.For questions, problems, or more information, contact gis@atcog.orghttps://atcog.org/

Fire Department boundary polygon data for Bowie, Cass, Delta, Franklin, Hopkins, Lamar, Morris, Red River, and Titus Counties within Texas, and Miller County, Arkansas.For questions, problems, or more information, contact gis@atcog.orghttps://atcog.org/

Nevada Bureau of Mines and Geology FS Map-19; A 1:24,000 scale Geologic Map of the Mount Moriah Quadrangle, Nevada and Utah. Detailed geologic mapping by Jeffrey Lee, Elizabeth L. Miller, Phillip B. Gans, and Carey C Huggins in 1999.The Snake Range, in eastern White Pine County, Nevada, is a 150-km-long, north-trending mountain range in the northern Basin and Range province. Sacramento Pass divides the range into two main parts, the northern and southern Snake Range. The Mt Moriah Quadrangle is located on the central part of the Snake Range and includes the highest point in the range. The Snake Range is considered a classic example of a Cenozoic "metamorphic core complex" (for example, Coney, 1979). The most prominent structural feature of the range is the northern Snake Range decollement (NSRD), a low-angle fault. Map includes 1 cross section and description of 39 units. The GIS work was in support of the U. S. Geological Survey COGEOMAP program. The Geodatabase specifies feature datasets and feature classes, together with feature attributes, subtypes and domains, suitable for a variety of geologic maps. In addition to basic geology (lithology, contacts and faults, etc.), the maps may include metamorphic overprints, cross sections, and explanatory legend-graphics such as correlation charts, used to supplement columnar legends. Previous work includes Hose and Blake (1976) a 1 :250,000-scale geologic map of White Pine County which included the first published geologic map of all of the northern Snake Range; Nelson (1966, 1969) mapped the northern e,nd of the range as part of a regional mapping project that included the Kern Mountains and southern Deep Creek Range; studies in the northern Snake Range by geologists based at Stanford University began in 1981 by Miller and others (1983) and Gans and Miller (1983). Geologic mapping was supported by the Quadrangle mapping Program of the Geological Society of Nevada and by Echo Bay Minerals Company, Magma Nevada mining Company (now BHP), and the NBMG Mining Coop Fund. Base map: U. S. Geological Survey Mt Moriah 7.5-minute Quadrangle, 1986. To download and view this map resource, associated text, and GIS zipped data-set, please see the links provided.

1:24,000 scale Geologic Map of The Cove Quadrangle, Nevada and Utah. Detailed geologic mapping by Elizabeth L. Miller and Phillip B. Gans in 1999. Map includes 1 cross section and description of 38 units. The GIS work was in support of the U. S. Geological Survey COGEOMAP program. The Geodatabase specifies feature datasets and feature classes, together with feature attributes, subtypes and domains, suitable for a variety of geologic maps. In addition to basic geology (lithology, contacts and faults, etc.), the maps may include metamorphic overprints, cross sections, and explanatory legend-graphics such as correlation charts, used to supplement columnar legends. The Snake Range, in eastern White Pine County, Nevada, is a 150-km-long, north-trending mountain range in the northern Basin and Range province. Sacramento Pass divides the range into two main parts, the northern and southern Snake Range. The Cove Quadrangle is located on the southernmost flank of the Snake Range, bordering Snake Valley to the east. Includes two of the main drainages in the range, Hendry's Creek and Hampton Creek. The Snake Range is considered a classic example of a Cenozoic 'metamorphic core complex '(for example, Coney, 1979). The most prominent structural feature of the range is the northern Snake Range decollement (NSRD), a low-angle fault. Previous work includes Hose and Blake (1976) a 1 :250,000-scale geologic map of White Pine County which included the first published geologic map of all of the northern Snake Range; Nelson (1966, 1969) mapped the northern e,nd of the range as part of a regional mapping project that included the Kern Mountains and southern Deep Creek Range; studies in the northern Snake Range by geologists based at Stanford University began in 1981 by Miller and others (1983) and Gans and Miller (1983). Geologic mapping was supported by the Quadrangle mapping Program of the Geological Society of Nevada and by Echo Bay Minerals Company, Magma Nevada mining Company (now BHP), and the NBMG Mining Coop Fund. Base map: U. S. Geological Survey The Cove 7.5-minute Quadrangle, 1986. To download this map resource, and associated report and GIS zipped data sets, please see the links provided.

Law Enforcement boundary polygon data for Bowie, Cass, Delta, Franklin, Hopkins, Lamar, Morris, Red River, and Titus Counties within Texas, and Miller County, Arkansas.For questions, problems, or more information, contact gis@atcog.orghttps://atcog.org/

1:24,000 scale Geologic Map of the Little Horse Canyon Quadrangle, Nevada and Utah. Detailed geologic mapping by Phillip B. Gans, Elizabeth L. Miller, Carey C Huggins, and Jeffrey Lee in 1999. Map includes two cross sections and description of 35 units. One of the seven quadrangles in the north Snake Range mapped by Stanford University's Summer Field program. The GIS work was in support of the U. S. Geological Survey COGEOMAP program. The Snake Range, in eastern White Pine County, Nevada, is a 150-km-long, north-trending mountain range in the northern Basin and Range province. Sacramento Pass divides the range into two main parts, the northern and southern Snake Range. The Little Horse Canyon Quadrangle is located on the eastern flank of the northern Snake Range and includes portions of the Horse Canyon, little Horse Canyon, and Smith Creek drainages. The Snake Range is considered a classic example of a Cenozoic "metamorphic core complex" (for example, Coney, 1979). The most prominent structural feature of the range is the northern Snake Range decollement (NSRD), a low-angle fault. Previous work includes Hose and Blake (1976) a 1 :250,000-scale geologic map of White Pine County which included the first published geologic map of all of the northern Snake Range; Nelson (1966, 1969) mapped the northern e,nd of the range as part of a regional mapping project that included the Kern Mountains and southern Deep Creek Range; studies in the northern Snake Range by geologists based at Stanford University began in 1981 by Miller and others (1983) and Gans and Miller (1983). Geologic mapping was supported by the Quadrangle mapping Program of the Geological Society of Nevada and by Echo Bay Minerals Company, Magma Nevada mining Company (now BHP), and the NBMG Mining Coop Fund. Base map: U. S. Geological Survey Little Horse Canyon 7.5-minute Quadrangle, 1985. To download and view this map resource, associated text, and GIS zipped data-set, please see the links provided.

4 aerial photographs were taken along the Little Missouri River in 1982. All images were geo-referenced to the 1995 digital orthophoto quarter quadrangles as described by Miller and Friedman (2009). Both the flood plain and active channel of the river were delineated on the 1995 digital orthophoto quadrangles and overlaid on rectified photos. ArcGIS was used to draw the polygons that delineate the flood plain and active channel; the delineation was saved as a SHP file. The separate images (geoTIFFs) can be viewed as a composite along with that year's channel delineation (SHP file) using a geographic information system (GIS) application. Reference: Miller, J.R., and J.M. Friedman. 2009. Influence of flow variability on flood-plain formation and destruction, Little Missouri River, North Dakota. Geological Society of America Bulletin 121:752-759.

1:24,000 scale Geologic Map of the Old Mans Canyon Quadrangle, Nevada and Utah. Detailed geologic mapping by Elizabeth L. Miller, Phillip B. Gans, Susan P. Grier, Carey C Huggins, and Jeffrey Lee in 1999.The Snake Range, in eastern White Pine County, Nevada, is a 150-km-long, north-trending mountain range in the northern Basin and Range province. Sacramento Pass divides the range into two main parts, the northern and southern Snake Range. The Old Mans Canyon Quadrangle is located on the southern flank of the northern Snake Range and borders the Sacramento Pass. The Snake Range is considered a classic example of a Cenozoic 'metamorphic core complex '(for example, Coney, 1979). The most prominent structural feature of the range is the northern Snake Range decollement (NSRD), a low-angle fault. Previous work includes Hose and Blake (1976) a 1:250,000-scale geologic map of White Pine County which included the first published geologic map of all of the northern Snake Range; Nelson (1966, 1969) mapped the northern end of the range as part of a regional mapping project that included the Kern Mountains and southern Deep Creek Range; studies in the northern Snake Range by geologists based at Stanford University began in 1981 by Miller and others (1983) and Gans and Miller (1983). Geologic mapping was supported by the Quadrangle mapping Program of the Geological Society of Nevada and by Echo Bay Minerals Company, Magma Nevada mining Company (now BHP), and the NBMG Mining Coop Fund. Base map: U.S. Geological Survey Old Mans Canyon 7.5-minute Quadrangle, 1986. The GIS work was in support of the U.S. Geological Survey COGEOMAP program. To download and view this map resource, map text, and associated GIS zipped data-set, please see the links provided.

description: The geology of Spokane County and vicinity, Washington and Idaho was compiled from Carrara and others (1995), Joseph (1990), Kiver and others (1979), Miller (written communication, 1995), and Waggoner (1990a, b) for input into an Arc/Info geographic information system (GIS). The digital geologic map database can be queried in many ways to produce a variety of derivative geologic maps.; abstract: The geology of Spokane County and vicinity, Washington and Idaho was compiled from Carrara and others (1995), Joseph (1990), Kiver and others (1979), Miller (written communication, 1995), and Waggoner (1990a, b) for input into an Arc/Info geographic information system (GIS). The digital geologic map database can be queried in many ways to produce a variety of derivative geologic maps.

Attachment regarding a quasi-judicial public hearing for a request by Jennifer Miller-Farias, for a Conditional Use Permit for a Boarding Kennel, Parcel 64991 being approximately 6.75 acres, located at 5821 NC HWY 87, Hadley Township.

Feature symbolizing road centerlines in Porter County, IN.

Porter County makes no warranty of completeness of accuracy for this data feature. Data is provided ‘as is’ and is subject to continual update maintenance, revision and correction as needed. The burden for determining appropriateness for use rests solely on the user. This data does not represent a survey. No liability is assumed for this data.

Data is created and maintained by Porter County GIS staff using ESRI ArcGIS Desktop licensed software.For questions related to this data contact: Chuck Miller, Porter County GIS Manageremail: CMiller@porterco.orgphone: 219-465-3537.Porter County GISDepartment of Development &Stormwater Management155 Indiana Ave, Suite 311Valparaiso, IN 46383

Public boat ramps in the northeast Texas region and Miller County AR. Texas boat ramp location data sourced from the Texas Parks and Wildlife Department. Arkansas boat ramp location data sourced from the Arkansas Highway and Transportation Department & Arkansas GIS Office. Hydrographic features sourced from the United States Geological Survey National Hydrography Dataset.For questions, problems, or more information, contact gis@atcog.orghttps://atcog.org/

Aerial photographs were taken along the Little Missouri River in 2003, however the 2003 IKONOS satellite imagery is proprietary and therefore cannot be served here. The channel delineations for all years, including 2003, and the delineation of the outer flood-plain boundary are stored as shapefiles and are included in this data release. All images were geo-referenced to the 1995 digital orthophoto quarter quadrangles as described by Miller and Friedman (2009). Both the flood plain and active channel of the river were delineated on the 1995 digital orthophoto quadrangles and overlaid on rectified photos. ArcGIS was used to draw the polygons that delineate the flood plain and active channel; the delineation was saved as a SHP file. The separate images (geoTIFFs) can be viewed as a composite along with that year's channel delineation (SHP file) using a geographic information system (GIS) application. Reference: Miller, J.R., and J.M. Friedman. 2009. Influence of flow variability on flood-plain formation and destruction, Little Missouri River, North Dakota. Geological Society of America Bulletin 121:752-759.

Feature symbolizing regulated drain centerlines in Porter County, IN. Regulated Drain definition:"A regulated drain is an open drain, tiled drain or combination designated by the county surveyor as a drain in need of upkeep and maintenance and regulated by county govenment."Porter County makes no warranty of completeness of accuracy for this data feature. Data is provided ‘as is’ and is subject to continual update maintenance, revision and correction as needed. The burden for determining appropriateness for use rests solely on the user. This data does not represent a survey. No liability is assumed for this data.Data is created and maintained by Porter County GIS staff using ESRI ArcGIS Desktop licensed software. For questions related to this data contact Chuck Miller, Porter County GIS Manager email: CMiller@porterco.org phone: 219-465-3537.Porter County GISDepartment of Development &Stormwater Management155 Indiana Ave, Suite 311Valparaiso, IN 46383

Boundary describes the extent of the Spokane Valley-Rathdrum prairie aquifer from south end of lake Pend Oreille, Idaho - thru Rathdrum Prairie, the Spokane Valley, turning north to discharge at little Spokane River, and Spokane river north and west of the city of Spokane. Source data overview:Spokane Valley aquifer (WA State only) digitized in 1988 by Spokane Co. Engineer Dept from USGS 1977 hydrologic study of the Spokane Aquifer. This layer digitized from 1:24000 quad maps into the County's GDMS GIS. The USGS relied heavily on contour lines that described the valley floor to delineate the Spokane aquifer boundary. The original boundary had the Spokane River as it's west edge, but was revised (by Bea Leckaff Spokane County WQMP-GIS) in June, 1994, under the direction of Stan Miller to include the flood plain terraces on the west side of the river, down to the Little Spokane River confluence. The extent of the aquifer was revised again in March, 1995 to reflect new information from CH2MHill aquifer studies being done for the City of Spokane (to support Wellhead Protection). The revised aquifer extends the influence of impervious basalt outcroppings from the Spokane Falls area to the Trinity Triangle, (Drumheller Springs). The corrections were made by BBL from information provided by Stan Miller.

Idaho Portion of the Aquifer data came from Idaho Panhandle Public Health GIS SCALE: Idaho data digitized originally from 1:24000 USGS maps LAST UPDATED: March 1993- received Idaho data and matched to Spokane county aquifer data.

The Kickoff Meeting for Baker, Decatur, Grady, Miller, and Mitchell Counties was held on October 8, 2020. This meeting was coordinated by the Georgia Flood MAP Program as part of the Lower Flint Watershed Risk MAP Project.