Potentiometric surface, Mississippi River Valley alluvial aquifer, spring 2016, raster format, in feet

A potentiometric surface map for spring 2016 was created for the Mississippi River Valley alluvial (MRVA) aquifer, which was referenced to the North American Vertical Datum of 1988 (NAVD 88), using most of the available groundwater-altitude data from wells and surface-water-altitude data from streamgages. Most of the wells were measured annually or one time, after installation, but some wells were measured more than one time in a year and a small number of wells were measured continually. Streamgages were typically operated continuously. The potentiometric surface map for 2016 was created as part of the U.S. Geological Survey (USGS) Water Availability and Use Science Program to support investigations that characterize the MRVA aquifer. The potentiometric contours ranged from 10 feet to 340 feet above NAVD 88. The regional direction of groundwater flow was generally towards the south-southwest, except in areas of groundwater-altitude depressions, where groundwater flows into the depressions, and near rivers, where groundwater flow generally parallels the flow in the rivers. There are large depressions in the potentiometric surface in the lower half of the Cache region and in most of the Grand Prairie and Delta regions.

Data and Resources

Field Value
accessLevel public
bureauCode {010:12}
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catalog_describedBy https://project-open-data.cio.gov/v1.1/schema/catalog.json
datagov_dedupe_retained 20220721212438
identifier USGS:5bc649c7e4b0fc368ebbebc0
metadata_type geospatial
modified 20200821
old-spatial {"type": "Polygon", "coordinates": [[[-92.793078813, 28.902555621], [-92.793078813, 37.412264775], [ -88.254169714, 37.412264775], [ -88.254169714, 28.902555621], [-92.793078813, 28.902555621]]]}
publisher U.S. Geological Survey
publisher_hierarchy Department of the Interior > U.S. Geological Survey
resource-type Dataset
source_datajson_identifier true
source_hash 953846727f8957f82e591bf2eef0caeb0e40c296
source_schema_version 1.1
spatial {"type": "Polygon", "coordinates": [[[-92.793078813, 28.902555621], [-92.793078813, 37.412264775], [ -88.254169714, 37.412264775], [ -88.254169714, 28.902555621], [-92.793078813, 28.902555621]]]}
theme {geospatial}
Groups
  • AmeriGEOSS
  • National Provider
  • North America
Tags
  • amerigeo
  • amerigeoss
  • aquifers
  • arkansas
  • ckan
  • geo
  • geoscientificinformation
  • geoss
  • ground-water
  • groundwater
  • groundwater-altitude
  • groundwater-levels
  • illinois
  • inlandwaters
  • kentucky
  • lmg
  • louisiana
  • lower-mississippi-gulf-water-science-center
  • map
  • mississippi
  • mississippi-alluvial-plain
  • mississippi-river-delta
  • mississippi-river-valley-alluvial-aquifer
  • missouri
  • mrva-aquifer
  • national
  • north-america
  • potentiometric-surface
  • surface-water-altitude
  • tennessee
  • u-s-geological-survey
  • united-states
  • usgs
  • usgs-5bc649c7e4b0fc368ebbebc0
  • water-availability-and-use-science-program
  • water-table
isopen False
license_id notspecified
license_title License not specified
maintainer V. L. McGuire
maintainer_email vlmcguir@usgs.gov
metadata_created 2025-11-20T09:33:09.866749
metadata_modified 2025-11-20T09:33:09.866753
notes A potentiometric surface map for spring 2016 was created for the Mississippi River Valley alluvial (MRVA) aquifer, which was referenced to the North American Vertical Datum of 1988 (NAVD 88), using most of the available groundwater-altitude data from wells and surface-water-altitude data from streamgages. Most of the wells were measured annually or one time, after installation, but some wells were measured more than one time in a year and a small number of wells were measured continually. Streamgages were typically operated continuously. The potentiometric surface map for 2016 was created as part of the U.S. Geological Survey (USGS) Water Availability and Use Science Program to support investigations that characterize the MRVA aquifer. The potentiometric contours ranged from 10 feet to 340 feet above NAVD 88. The regional direction of groundwater flow was generally towards the south-southwest, except in areas of groundwater-altitude depressions, where groundwater flows into the depressions, and near rivers, where groundwater flow generally parallels the flow in the rivers. There are large depressions in the potentiometric surface in the lower half of the Cache region and in most of the Grand Prairie and Delta regions.
num_resources 2
num_tags 36
title Potentiometric surface, Mississippi River Valley alluvial aquifer, spring 2016, raster format, in feet