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| Type: | Resource | |
| Storage: | The size of this resource is 1.5 KB | |
| Created: | Feb 07, 2023 at 8:11 p.m. | |
| Last updated: | Feb 07, 2023 at 8:12 p.m. | |
| Citation: | See how to cite this resource |
| Sharing Status: | Public |
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| Views: | 235 |
| Downloads: | 199 |
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Abstract
A digital simulation model was used to analyze regional ground-water flow in the Madison Group aquifer in the Powder River Basin in Montana and Wyoming and adjacent areas. Most recharge to the aquifer originates in or near the outcrop areas of the Madison in the Bighorn Mountains and Black Hills, and most discharge occurs through springs and wells. Flow through the aquifer in the modeled areas was approximately 200 cubic feet per second. The aquifer can probably sustain increased ground-water withdrawals of up to several tens of cubic feet per second, but these withdrawals probably would significantly lower the potentiometric surface in the Madison aquifer in a large part of the basin. (Woodard-USGS)
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Additional Metadata
| Name | Value |
|---|---|
| DOI | 10.3133/wri7563 |
| Depth | |
| Scale | 10 001 - 100 000 km² |
| Layers | 1 layer |
| Purpose | Groundwater resources |
| GroMoPo_ID | 128 |
| IsVerified | True |
| Model Code | Unknown |
| Model Link | https://doi.org/10.3133/wri7563 |
| Model Time | |
| Model Year | 1976 |
| Model Authors | L. Konikow |
| Model Country | United States |
| Data Available | Report/paper only |
| Developer Email | |
| Dominant Geology | Unsure |
| Developer Country | USA |
| Publication Title | Preliminary digital model of ground-water flow in the Madison Group, Powder River Basin and adjacent areas, Wyoming, Montana, South Dakota, North Dakota, and Nebraska |
| Original Developer | No |
| Additional Information | |
| Integration or Coupling | |
| Evaluation or Calibration | Static water levels |
| Geologic Data Availability |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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