Clark County Planned Land Use. This data is maintained by the Clark County Comprehensive Planning Department.

Planning and Zoning includes: Planned Land Use, Zoning, Historic Neighborhood Overlay District, Hard Rural Neighborhood Preservation, ROIS, PC Overlay, RNP Boundary, Flood Control Layers

Vector polygon map data of property parcels from Las Vegas, Nevada, containing 794,465 features.

Property parcel GIS map data consists of detailed information about individual land parcels, including their boundaries, ownership details, and geographic coordinates.

Property parcel data can be used to analyze and visualize land-related information for purposes such as real estate assessment, urban planning, or environmental management.

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.

This dataset was provided as part of my UCLA MAGIST program for performing SQL queries on 1.4+ million record table (voters). I decided I wanted to try to emulate the same queries using Python and Pandas. I did remove any personally identifiable information (PII) fields before publishing here on Kaggle. You can download a full copy from this Web site.

https://www.clarkcountynv.gov/government/departments/elections/reports_data_maps/voter_list_data_files.php

The geospatial information was downloaded from the Clark County GIS Hub Site.

GIS Management Office (GISMO) (clarkcountynv.gov)

Short Term Rentals in Clark County, Nevada. Data sources are from City of Las Vegas and City of North Las Vegas.

A 1:24,000-scale, geologic map of the Meadview North 7.5' Quadrangle in Mohave County, Arizona and Clark County, Nevada, with description of 54 geologic units. 1:24,000-scale, geologic map of the Meadview North 7.5' Quadrangle in Mohave County, Arizona and Clark County, Nevada, with description of 54 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. To download and view this map resource, please see the link provided.

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.

50 meter contours for all of Clark County, NV

1:24,000 scale Geologic Map of the Iceberg Canyon Quadrangle, Clark County, Nevada and Mohave County, Arizona. Nevada Bureau of Mines and Geology Map 166. Detailed geologic mapping by Robert J. Brady, Joan E. Fryxell, and Brian P. Wernicke in 2011. Map includes description of 40 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. Includes results of geochemical analyses and age determinations of igneous rocks. The map, text, and GIS work are available for purchase at the links provided under online availability.

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.

Clark County School District's Kindergarten Elementary attendance boundaries. Elementary "K" boundaries are for grade K (Kindergarten) only. Kindergarten boundaries do not reflect typical elementary boundaries and should be utilized accordingly. Attendance boundaries are reviewed annually and are subject to change. All boundary changes will be implemented at the beginning of the school year, subsequent to approval by the CCSD Board of School Trustees.