Well, the "letting through" of any substance through an object is considered permeability. Therefore, I'd suppose that the rock's ability to let water pass through the voids is called permeability.
The process is called permeability, which refers to the ability of water to flow through the small spaces within a rock or soil. Permeable rocks allow water to move through them easily, while impermeable rocks do not allow water to pass through.
The process of water seeping or flowing into rocks is called infiltration. This occurs as water moves through the pores and cracks in the rock, eventually becoming groundwater.
When a rock allows water to pass through it, this property is referred to as "permeability." Permeable rocks have interconnected pores or fractures that enable the movement of water and other fluids. In contrast, rocks that do not permit water to flow through them are considered "impermeable."
Is surface water
Water can breakdown rocks mechanically through a process called hydraulic action, where water enters cracks and crevices in rocks. When this water freezes and expands, it exerts pressure on the rock, causing it to crack. Additionally, water can carry sediment and debris that effectively wear down rock surfaces through abrasion.
Permeability/ hydraulic conductivity.
The process is called permeability, which refers to the ability of water to flow through the small spaces within a rock or soil. Permeable rocks allow water to move through them easily, while impermeable rocks do not allow water to pass through.
Water that travels through soil and rocks is called groundwater. It is an important source of freshwater for drinking and irrigation.
Permeability/ hydraulic conductivity.
The ability of water to move through soil is called "percolation." It describes the process of water moving through soil due to gravity or pressure gradients. This movement helps distribute water, nutrients, and pollutants in the soil.
Water held in pores of rocks is called groundwater. It is an important natural resource that can be extracted through wells for various uses.
Permeable rocks, like sandstone or limestone, have the ability to allow water to pass through their pores and fractures. These rocks are important for groundwater storage and movement in aquifers.
This ability is called porous (with many holes).
It is called infiltration, which is the process of water entering and moving through soil and rocks. This is an important part of the water cycle as it replenishes groundwater and helps sustain plant life.
The ability of water to spread through fine pores is called capillary action. This phenomenon is due to the cohesive and adhesive properties of water molecules, allowing them to move through narrow spaces against the force of gravity.
The process of water seeping or flowing into rocks is called infiltration. This occurs as water moves through the pores and cracks in the rock, eventually becoming groundwater.
When a rock allows water to pass through it, this property is referred to as "permeability." Permeable rocks have interconnected pores or fractures that enable the movement of water and other fluids. In contrast, rocks that do not permit water to flow through them are considered "impermeable."