ground water
The transfer of water through the ground and back to the sea is called precipitation.
Groundwater.
The vertical movement of water through ground layers is called infiltration. This process involves water soaking into the soil and moving downwards through the layers of earth.
Water can infiltrate the ground through precipitation, such as rain or snowmelt, seeping through the soil. It can also enter the ground through surface water bodies like lakes, rivers, or streams, being absorbed into the ground through a process called groundwater recharge.
The water that soaks in ground called as ground water .
The water that soaks in ground called as ground water .
Precipitation seeping through cracks and holes in the ground.
When water passes through a rock, it's called infiltration. This process involves water seeping into the ground and moving through the tiny spaces within the rock.
The process of water moving down through the soil is called infiltration. It refers to the movement of water from the ground surface into the soil.
A place where water trickles through the ground is called a seep. It is a slow and steady flow of water that emerges from the ground due to underground water pressure or saturation. Seeps can create wet patches or small streams on the surface.
A layer of impermeable rock, such as clay or shale, can prevent the flow of groundwater through it due to its tightly packed structure and low porosity. This impermeable layer acts as a barrier, restricting the movement of water vertically through the rock formation.
When rain falls, some of the water soaks into the ground. Plants use some of it, but much of the water sinks deeper into the soil. Gravity draws it through rocks that contain small holes or what is s. As it seeps through this porous rock, the water continues on until it reaches a level of total saturation. That level is called a water table.