Tokio study area
Data and Resources
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Digital DataXML
Landing page for access to the data
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Original MetadataXML
The metadata original format
| Field | Value |
|---|---|
| accessLevel | public |
| bureauCode | {010:12} |
| catalog_@context | https://project-open-data.cio.gov/v1.1/schema/catalog.jsonld |
| catalog_@id | https://ddi.doi.gov/usgs-data.json |
| catalog_conformsTo | https://project-open-data.cio.gov/v1.1/schema |
| catalog_describedBy | https://project-open-data.cio.gov/v1.1/schema/catalog.json |
| identifier | http://datainventory.doi.gov/id/dataset/usgs-5926e24de4b0b7ff9fb48a28 |
| metadata_type | geospatial |
| modified | 2020-08-21T00:00:00Z |
| old-spatial | -94.265396119, 33.475123036, -92.876048896, 34.216705631 |
| publisher | U.S. Geological Survey |
| resource-type | Dataset |
| source_datajson_identifier | true |
| source_hash | 32cafee116947c762735d127295e3e2bb49fb2e0e0815e5a212c21a65ab1c1f0 |
| source_schema_version | 1.1 |
| spatial | {"type": "Polygon", "coordinates": [[[-94.265396119, 33.475123036], [-94.265396119, 34.216705631], [ -92.876048896, 34.216705631], [ -92.876048896, 33.475123036], [-94.265396119, 33.475123036]]]} |
| theme | {geospatial} |
| Groups |
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| Tags |
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| isopen | False |
| license_id | notspecified |
| license_title | License not specified |
| maintainer | William J. Wolfe |
| maintainer_email | wjwolfe@usgs.gov |
| metadata_created | 2025-09-24T06:32:53.730750 |
| metadata_modified | 2025-09-24T06:32:53.730760 |
| notes | The Tokio Formation in southwestern Arkansas, hereafter referred to as the Tokio aquifer, is a source of groundwater for agricultural, domestic, industrial, and public use in Clark, Hempstead, Little River, Miller, Pike, and Nevada counties. Water-level altitudes measured 42 wells completed in the Tokio aquifer during 2014 and 2015 were used to create a potentiometric-surface map. In southwestern Arkansas, potentiometric surfaces indicate that groundwater flow in the Tokio aquifer is towards the city of Hope. Northwest of the city of Hope, a cone of depression may exist. In southwestern Pike, northwestern Nevada, and northeastern Hempstead Counties, an area of artesian flow (water levels are at or above land surface) exists. |
| num_resources | 2 |
| num_tags | 13 |
| title | Tokio study area |