An aquifer transmits ground water freely.
No, it is called ground water.
The top level of groundwater in an aquifer is called the water table.
Groundwater
Drift and/or till.
abrasion
Permeable rock layers or sediments that transmit groundwater freely are called aquifers. Aquifers can store and yield significant quantities of water, making them important sources of groundwater for wells and springs.
Layers that transmit groundwater are called aquifers. These layers are typically composed of porous and permeable materials such as sand, gravel, or rock that allow water to flow through them. Aquifers are important sources of freshwater for drinking and irrigation.
These underground water storage areas are typically referred to as aquifers. Aquifers are permeable rock layers or sediments that can hold and transmit groundwater. They are important sources of water for drinking, irrigation, and industrial use.
Permeable rock layers such as sandstone, limestone, and fractured volcanic rock can hold and transmit groundwater. Porous rock layers like sandstones, conglomerates, and fractured limestone allow for the storage and movement of groundwater due to their interconnected pore spaces.
groundwater
A permeable rock layer that transmits groundwater is called an aquifer. Aquifers hold and transmit water, allowing it to move through the rock or soil and provide a natural source of groundwater for wells and springs. It is essential for water supply and storage in underground reservoirs.
aquifer
It is called an aquifer.
An aquifer is a layer of permeable rock that contains water. It usually conducts groundwater and supplies the water for wells and springs.
Groundwater is located in the saturation zone of the ground where all the pores in the rock are filled with water. It moves slowly through the permeable rock called aquifers due to the force of gravity.
Water in rocks (or other porous material) below the ground is called ground water.
The water-filled spaces underground are called aquifers. Aquifers are underground rock formations or sediments that hold and transmit water. They are an important source of groundwater for drinking water and irrigation.