An underground place that doesn't hold water.
49% of the area of Germany has porous aquifers, partly with high yields. About 12% is made of fractured aquifers and some 6% karst aquifers. Approximately one-third of the country has only local aquifers with low potential.
Aquifers, which are underground layers of rock or sediment that hold water, and springs, which are natural sources of water that flow to the surface from underground, are two examples of groundwater.
Aquifers lose their porosity and thus making it not aquifers anymore.
evaporation within the earth
Wells tap into aquifers.
Water in aquifers depletes when people use the water faster than its replenishment rate. Some water is also lost due to evaporation.
there are exactly 273 aquifers in the world.
Aquifers are groundwater.
No, there is no aquifers in Texes.
Underground aquifers are the commonest source for well water.Underground aquifers are the commonest source.
Some water from the water cycle collects underground in aquifers.
Some of the largest aquifers in the US include the Ogallala Aquifer, the Edwards-Trinity Aquifer System, the Floridan Aquifer System, and the Great Basin Aquifer System. These aquifers are crucial sources of groundwater for drinking water and irrigation in their respective regions.