Commercial zoning map.

Zoning for all Entities in Southern Nevada. Clark County, Las Vegas, North Las Vegas, Boulder City, Mesquite and Henderson zoning are combined in this service.

Southeast sector zoning map.

Vector polygon map data of city limits from Las Vegas, Nevada containing 87 features.

City limits GIS (Geographic Information System) data provides valuable information about the boundaries of a city, which is crucial for various planning and decision-making processes. Urban planners and government officials use this data to understand the extent of their jurisdiction and to make informed decisions regarding zoning, land use, and infrastructure development within the city limits.

By overlaying city limits GIS data with other layers such as population density, land parcels, and environmental features, planners can analyze spatial patterns and identify areas for growth, conservation, or redevelopment. This data also aids in emergency management by defining the areas of responsibility for different emergency services, helping to streamline response efforts during crises..

This city limits data is available for viewing and sharing as a map in a Koordinates map viewer. This data is also available for export to DWG for CAD, PDF, KML, CSV, and GIS data formats, including Shapefile, MapInfo, and Geodatabase.

Southwest sector zoning map.

The boundaries of each zoning district are delineated and shown on the Official Zoning Map of the City of Las Vegas. The Official Zoning Map, together with all notations, references, dimensions, designations and other information shown on the map, is adopted and midpart of Title 19 by reference. The Official Zoning Map shall be stored, maintained, and kept current by the department of Planning.Last updated: May 22 2025

Geologic Map of the Las Vegas Manganese District, Clark County, Nevada.

1:100,000 scale Geologic Map of the Las Vegas Area, Clark County, Nevada, and Inyo County, California, USGS SIM2814. Detailed geologic mapping by William R. Page, Scott C. Lundstrom, Anita G. Harris, Victoria E. Langenheim, Jeremiah B. Workman, Shannon A. Mahan, James B. Paces, Gary L. Dixon, Peter D. Rowley, B.C. Burchfiel, John W. Bell, and Eugene I. Smith. Prepared in cooperation with the Southern Nevada Water Authority.

This digital geologic and tectonic database of the Death Valley ground-water model area, as well as its accompanying geophysical maps, are compiled at 1:250,000 scale. The map compilation presents new polygon, line, and point vector data for the Death Valley region. The map area is enclosed within a 3 degree X 3 degree area along the border of southern Nevada and southeastern California. In addition to the Death Valley National Park and Death Valley-Furnace Creek fault systems, the map area includes the Nevada Test Site, the southwest Nevada volcanic field, the southern end of the Walker Lane (from southern Esmeralda County, Nevada, to the Las Vegas Valley shear zone and Stateline fault system in Clark County, Nevada), the eastern California shear zone (in the Cottonwood and Panamint Mountains), the eastern end of the Garlock fault zone (Avawatz Mountains), and the southern basin and range (central Nye and western Lincoln Counties, Nevada). This geologic map improves on previous geologic mapping in the area by providing new and updated Quaternary and bedrock geology, new interpretation of mapped faults and regional structures, new geophysical interpretations of faults beneath the basins, and improved GIS coverages. The basic geologic database has tectonic interpretations imbedded within it through attributing of structure lines and unit polygons which emphasize significant and through-going structures and units. An emphasis has been put on features which have important impacts on ground-water flow. Concurrent publications to this one include a new isostatic gravity map (Ponce and others, 2001), a new aeromagnetic map (Ponce and Blakely, 2001), and contour map of depth to basement based on inversion of gravity data (Blakely and Ponce, 2001).

Active businesses within the Enhanced Medical District boundary in Downtown Las Vegas. Click "About" for attachment on field information.

Centennial Hills Zoning Map

1:24,000 scale Geologic Map of the Crater Flat Area, Nevada. Detailed geologic mapping by James E. Faulds, John W. Bell, Daniel L. Feuerbach, and Alan R. Ramelli in 1994. Map includes description of 42 geologic 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 the printed geologic map. 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. This geologic map generally includes previously unpublished data obtained by the authors. However the mapping of Pliocene basalts by Crowe and others (1983) and Paleozoic-Proterozoic rocks by Monsen and others (1992) was incorporated into the southern part of the map area. Partial financial support for field work and map preparation was provided by the Nevada Agency of Nuclear Projects through the Center for Volcanic and Tectonic Studies, University of Nevada, Las Vegas; the Center for Neotectonic Studies, University of Nevada, Reno; and NSF grant EAR9120383 (awarded to Faulds). Base map: U. S. Geological Survey Crater Flat 7.5-minute Quadrangle, 1986. To download the map resource and associated report, and GIS zipped data sets, please see the links provided.

1:24,000 scale Geologic Map of the Blue Diamond SE Quadrangle, Nevada. Detailed geologic mapping by Michael D. Carr, Cheryl McDonnell-Canan, and David L. Weide in 2000. Field work done from 1988 to 1997. This map illustrates the distribution of bedrock and surficial deposits in the Blue Diamond SE quadrangle, in the Las Vegas Nevada area. The field work was in support of the U. S. Geological Survey COGEOMAP program. Geologic mapping was supported by the University of Nevada, Las Vegas, Department of Geoscience. Previous work includes: Geologic map and description of structure and stratigraphy, La Madre Mountain, Spring Mountains (Axen, 1985); Geology of the Spring Mountains, Nevada (Burchfiel and others, 1974); Geology of the east-central part of the Spring Mountain range (Glock, 1929); Geology and ore deposits of the Goodsprings Quadrangle (Hewett, 1931); Geology and mineral deposits of Clark County (Longwell and others, 1965); Geology of the Little Colorado Valley (Ward, 1901). Base map: U.S. Geological Survey Blue Diamond SE 7.5' Quadrangle, 1983. To view this map or download the GIS zipped datasets, please see the links provided,

The Lake Mead Quadrangle exposes a tremendous range of strata, from Proterozoic-age crystalline rocks, Paleozoic and Mesozoic sedimentary rocks, Tertiary sediments, volcanics and plutons, and Late-Tertiary to Quaternary surficial deposits. Introduction The geologic map of the Lake Mead 30' x 60' quadrangle was completed for the U.S. Geological Survey's Las Vegas Urban Corridor Project and the National Parks Project, National Cooperative Geologic Mapping Program. Lake Mead, which occupies the northern part of the Lake Mead National Recreation Area (LAME), mostly lies within the Lake Mead quadrangle and provides recreation for about nine million visitors annually. The lake was formed by damming of the Colorado River by Hoover Dam in 1939. The recreation area and surrounding Bureau of Land Management lands face increasing public pressure from rapid urban growth in the Las Vegas area to the west. This report provides baseline earth science information that can be used in future studies of hazards, groundwater resources, mineral and aggregate resources, and of soils and vegetation distribution. The preliminary report presents a geologic map and GIS database of the Lake Mead quadrangle and a description and correlation of map units. The final report will include cross-sections and interpretive text. The geology was compiled from many sources, both published and unpublished, including significant new mapping that was conducted specifically for this compilation. Geochronologic data from published sources, as well as preliminary unpublished 40Ar/39Ar ages that were obtained for this report, have been used to refine the ages of formal Tertiary stratigraphic units and define new informal Tertiary sedimentary and volcanic units.

1:24,000 scale Geologic Map of the Government Wash Quadrangle, Clark County, Nevada. Detailed geologic mapping by Ernest M. Duebendorfer of the Northern Arizona University. Field work performed from 1990 to 1995. The Government Wash Quadrangle is located north of the western part of Lake Mead in southern Nevada. The Lake Mead area, between the Grand Wash Cliffs and Las Vegas, Nevada. This work was supported in part by grants to Duebendorfer from the Nevada Bureau of Mines and Geology, the National Science Foundation, and the donors of The Petroleum Research Fund, administered by the American Chemical Society. Office and field reviews of the map by R.E. Anderson, L.S. Beard, and J.E. Faulds. Steve Castor, Steve Rowland, and Jim Trexler also contributed to field review of the map. Gary O Brien and Ken Puhn assisted in map preparation. Base map: U.S. Geological Survey Government Wash Quadrangle, 1970. Stratigraphy and structural geology of the quadrangle are discussed in the accompanying text. The GIS work was in support of the U. S. Geological Survey COGEOMAP program. To download this map PDF resource and associated text, references and GIS zipped data-set, please see the links provided.

1:24,000 scale Geologic Map of the Nelson Quadrangle, Clark County, Nevada. Nevada Bureau of Mines Map 134. Detailed Geologic Mapping By Jame s E . Faulds, John W. Bell, and Eric L. Olson in 2002. Field work done 1999. Map includes two cross sections and 42 geologic units. The quadrangle includes part of the Highland range, Eldorado Valley, and Piute Valley. It contains excellent exposures of early to middle Miocene volcanic and sedimentary rocks, the upper part of the ~16.6 Ma Searchlight. Mining district. The Miocene section rests nonconformably on Early Proterozoic gneiss. As a result of the middle Miocene extension, Tertiary strata are moderately to steeply tilted and cut by complex arrays of normal faults. Flat-lying Quaternary alluvial-fan deposits dominate Eldorado and Piute Valleys and onlap tilted Miocene strata in the Highland Range. The GIS work was in support of the U.S. Geological Survey COGEOMAP program. Office Reviewers: Frank Hillemeyer, La Cuesta International, Inc., Kingman, AZ.; Jonathan Miller, Dept. of Geology, San Jose State University, San Jose, CA.; Alan Ramelli, NBMG; Eugene Smith, Dept. of Geoscience, UNLV. Field Reviewers: Frank Hillemeyer, La Cuesta International, Inc., Kingman, AZ.; Werner Hellmer, Dept. of Building, Clark County; Ryan Murphy, Dept. of Geological Sciences , University of Nevada; John Peck, Consulting Geologist, Las Vegas , NV.; Jonathan Price, NBMG; Alan Ramelli, NBMG. The geologic mapping was supported by the U.S. Geological Survey STATEMAP Program (Agreement No. HQ-AG-2036) and a grant from the National Science Foundation (E AR 98-96032). The 40Ar/39Ar dates were obtained through geochronology labs at the U.S. Geological Survey in Denver, for which we thank Steve Harlan, and the New Mexico Bureau of Mines, for which we thank Bill McIntosh and Matt Heizler. We greatly appreciated the hospitality of several landowners in the area, including Barney and Elaine Reagan, Gene Lambert, and John Kuyger. We also thank the Lake Mead National Recreation Area for providing housing during part of this study. Base map: U.S. Geological Survey Nelson SW 7.5' Quadrangle. To download and view this map resource, map text, and associated GIS zipped data-set, please see the links provided.

Hillside Overlay Map

1:24,000 scale Geologic Map of the Lamoille Quadrangle, Elko County, Nevada. Detailed geologic mapping by Keith A. Howard in 2000. Field work done in 1963-65,1996-1997, assisted by Lee Wilson, 1963. Office Review by: Jim Faulds (NBMG), Chris Henry (NBMG), Arthur Snoke (University of Wyoming), and Mike Wells University of Nevada, Las Vegas). Field Review by: Chris Henry (NBMG) and Jon Price (NBMG). The geologic mapping was supported by Yale-Binney and D.F. Hewett scholarships, National Science Foundation, a Newmont Mining Company grant to NBMG, and USGS National ooperative Geologic Mapping Program. The Ruby Mountains and adjoining East Humboldt Range form one of more than a score of North American Cordilleran metamorphic core complexes (Crittenden and others, 1980). The quadrangle lies within the area of a geologic map of the Ruby Mountains (Howard and others, 1979, 1:125,000-scale). Geologic maps of adjacent quadrangles can be found in Howard (1966, 1:24,000), Smith and Howard (1977, 1:62,500), and MacCready and others (1997, ~1:45,500). Base map: U.S. Geological Survey Lamoille 7.5' Quadrangle, 1990. Subject: 1:24,000 scale Geologic Map of the Lamoille Quadrangle. To download this Map PDF resource, associated text, and GIS zipped data-set, please see the links provided.

Ground-water flow through the region south and west of Frenchman Flat, in the Ash Meadows subbasin of the Death Valley ground-water flow system, is controlled mostly by faults which arrange the distribution of permeable and impermeable rocks. In addition, most permeability is along fractures caused by faulting in carbonate rocks. Large faults are more likely to reach the potentiometric surface as deep as 325 meters below the ground surface and are more likely to effect the flow path than small faults. This study concentrated on identifying large faults, especially where they cut carbonate rocks. Small faults, however, may develop as much permeability as large faults if they are penetrative and are part of an anastomosing fault zone. The overall pattern of faults and joints at the ground surface in the Spotted and Specter Ranges is an indication of the fracture system at the depth of the water table. Most of the faults in these ranges are west-southwest-striking, high-angle faults, 100 to 3,500 meters long, with 10 to 300 meters of displacement. Many of them, such as those in the Spotted Range and Rock Valley are left-lateral strike-slip faults that are conjugate to the NW-striking right-lateral faults of the Las Vegas Valley shear zone. These faults control the ground-water flow path, which runs west-southwest beneath the Spotted Range, Mercury Valley and the Specter Range. The Specter Range thrust is a significant geologic structure with respect to ground- water flow. This regional thrust fault emplaces siliceous clastic strata into the north central and western parts of the Specter Range. These rocks act as a barrier that confines ground- water flow to the southern part of the range, directing it southwestward toward springs at Ash Meadows. These siliceous clastic aquitard rocks and overlying Cenozoic deposits probably also block westward flow of ground-water in Rock Valley, diverting it southward to the flow path beneath the southern part of the Specter Range.

Provides information on location, pipe diameter, slope and length of pipe for existing sewer lines within the City of Las Vegas' sewer pipeline network.

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