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Clues For Finding Groundwater Ask locals where they currently get their water. Sand or gravel areas in the bottom of valleys will often be home to groundwater. Natural springs usually indicate groundwater is nearby. If there are streams in the area, look for sections where the flow is greater.
Sand or gravel areas in the bottom of valleys will often be home to groundwater. These layers can be covered by clay or silt, so its prudent to check these areas thoroughly. Natural springs usually indicate groundwater is nearby. A spring that flows year-round will likely reveal a productive aquifer.
As a first step in locating ground water, the hydrologist prepares a geologic map showing where the different kinds of rock come to the land surface. Some of the rocks may be so cracked and broken that they provide good openings to carry water underground.
Its critical to understand that groundwater does not flow in underground streams, nor does it form underground lakes. With the exception of karst areas, with caves in limestone, groundwater flows very slowly through granular sediments, or through solid rock that has fractures in it.
Shallow ground water is more likely to occur in larger quantities under valleys than under hills, because ground water obeys the law of gravity and flows downward just as surface water does. In arid regions the presence of water-loving plants is an indication of ground water at shallow depth.
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What is Groundwater? Groundwater is the water found underground in the cracks and spaces in soil, sand and rock. It is stored in and moves slowly through geologic formations of soil, sand and rocks called aquifers.
Alabama has enough ground water to cover the entire state to a depth of about 50 feet. WHAT IS GROUND WATER? A film of water clings to each particle in the unsaturated zone even when it may seem dry.
Groundwater is found in two zones. The unsaturated zone, immediately below the land surface, contains water and air in the open spaces, or pores. The saturated zone, a zone in which all the pores and rock fractures are filled with water, underlies the unsaturated zone.

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