Electrical Resistivity Tomography (ERT) data files collected near Quitobaquito Spring in Organ Pipe Cactus National Monument, 2023 and 2024
Direct-Current resistivity data were collected to characterize the hydrogeology and groundwater depth surrounding Quitobaquito Spring. Resistivity data are sensitive to water-content in the geologic unit in the subsurface. DC resistivity data were collected at six transects. One transect passes just south of the spring pool and runs east-west. One transect is located just southeast of the spring and runs east-west through a sandy wash that experience surface flow during high precipitation in the area. One transect cross potential faults as it runs southwest-northeast and is located northwest of the spring. One transect crosses directly over the spring discharge site and runs roughly north-south. One transect travels from the spring to the northeast rising along the elevation of the nearby hill. The final transect runs north-south through the sandy wash located east of the spring. This data includes the raw data and inverted resistivity models.
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Complete Metadata
| @type | dcat:Dataset |
|---|---|
| accessLevel | public |
| bureauCode |
[
"010:12"
]
|
| contactPoint |
{
"fn": "Jacob L. Conrad",
"@type": "vcard:Contact",
"hasEmail": "mailto:jlconrad@usgs.gov"
}
|
| description | Direct-Current resistivity data were collected to characterize the hydrogeology and groundwater depth surrounding Quitobaquito Spring. Resistivity data are sensitive to water-content in the geologic unit in the subsurface. DC resistivity data were collected at six transects. One transect passes just south of the spring pool and runs east-west. One transect is located just southeast of the spring and runs east-west through a sandy wash that experience surface flow during high precipitation in the area. One transect cross potential faults as it runs southwest-northeast and is located northwest of the spring. One transect crosses directly over the spring discharge site and runs roughly north-south. One transect travels from the spring to the northeast rising along the elevation of the nearby hill. The final transect runs north-south through the sandy wash located east of the spring. This data includes the raw data and inverted resistivity models. |
| distribution |
[
{
"@type": "dcat:Distribution",
"title": "Digital Data",
"format": "XML",
"accessURL": "https://doi.org/10.5066/P13COJJR",
"mediaType": "application/http",
"description": "Landing page for access to the data"
},
{
"@type": "dcat:Distribution",
"title": "Original Metadata",
"format": "XML",
"mediaType": "text/xml",
"description": "The metadata original format",
"downloadURL": "https://data.usgs.gov/datacatalog/metadata/USGS.68b71744d4be022efaf1cc9d.xml"
}
]
|
| identifier | http://datainventory.doi.gov/id/dataset/USGS_68b71744d4be022efaf1cc9d |
| keyword |
[
"Arizona",
"Arizona Water Science Center",
"Direct Current Resistivity",
"Geophysics",
"Groundwater",
"Hydrogeology",
"Hydrology",
"Organ Pipe Cactus National Monument",
"Pima County",
"Quitobaquito Spring",
"Resistivity",
"Sonoran Desert",
"USGS:68b71744d4be022efaf1cc9d"
]
|
| modified | 2026-03-18T00:00:00Z |
| publisher |
{
"name": "U.S. Geological Survey",
"@type": "org:Organization"
}
|
| spatial | -113.027200, 31.938400, -113.009000, 31.946000 |
| theme |
[
"geospatial"
]
|
| title | Electrical Resistivity Tomography (ERT) data files collected near Quitobaquito Spring in Organ Pipe Cactus National Monument, 2023 and 2024 |
