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Aquifer by rock type

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Sandstone and carbonate-rock aquifers

The flat to gently rolling plains of the Edwards Plateau are locally interrupted by steep canyon walls. This view in western Crockett County, Texas, is toward the southwest and the Pecos River Valley. The road cut exposes the Fort Lancaster Formation.

The principal water-yielding aquifers of North America can be grouped into five types: unconsolidated and semiconsolidated sand and gravel aquifers, sandstone aquifers, carbonate-rock aquifers, aquifers in interbedded sandstone and carbonate rocks, and aquifers in igneous and metamorphic rocks.

In scattered places in the United States, carbonate rocks are interbedded with almost equal amounts of water-yielding sandstone. In most places where these two rock types are interbedded, the carbonate rocks yield much more water than the sandstone.

Most carbonate rocks originate as sedimentary deposits in marine environments. Compaction, cementation, and dolomitization processes might act on the deposits as they lithify and greatly change their porosity and permeability. However, the principal postdepositional change in carbonate rocks is the dissolution of part of the rock by circulating, slightly acidic groundwater. Solution openings in carbonate rocks range from small tubes and widened joints to caverns that may be tens of meters wide and hundreds to thousands of meters long. Where they are saturated, carbonate rocks with well-connected networks of solution openings yield large amounts of water to wells that penetrate the openings, although the undissolved rock between the large openings may be almost impermeable.

This map of sandstone and carbonate-rock aquifers in the United States shows the shallowest principal aquifer. In some places, other, sometimes more productive, aquifers underlie those mapped. Only small areas of some aquifers may be shown on the map because they are covered in many places by other aquifers closer to the land surface. In other places, local aquifers, such as those along stream valleys, might overlie the aquifers mapped. Local aquifers are not shown because of the scale of the map. Some aquifers in sedimentary rocks are overlain by confining units, and the aquifers extend into the subsurface beyond the areas shown on the map.

colored block
Sandstone and carbonate-rock aquifers at or near the land surface
gray line
Limit of continental glaciation. North of this line, glacial sand and gravel aquifers overlie bedrock aquifers in many places  

Sandstone and carbonate-rock aquifers include:

See also: Sandstone aquifers

See also: Carbonate-rock aquifers

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Page Last Modified: Wednesday, 28-Dec-2016 01:27:56 EST