soil
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It is the movement of water in soil.
"Groundwater flow is the movement of water that travels and seeps through soil and rock underground. Stored in cavities and geologic pores of the earth's crust, confined groundwater is under a great deal of pressure. Its upper part is lower than the material in which it is confined. Unconfined groundwater is the term for an aquifer with an exposed water surface."
ground water Groundwater is located beneath the soil surface. A sustainable amount of ground water creates an aquifer. The point at which the soil and rocks become completely saturated is the water table. Groundwater will flow to the surface naturally. The study of groundwater is hydrogeology.
through flow is when infiltrated water moves through soil to the sea.
soil
yo mamas soil grows fastest
Through flow is the horizontal movement of water through the soil zone. Groundwater flow is the movement of water through the bedrock, which is typically an aquifer
In general the larger the pore space (the higher the porosity) the easier it is for water to flow through it (it is more permeable).
11234567890-=-09876543wawzsr
Throughflow is the tranfer of water through th soil. Surface runoff is the transfer of water where the soil is impermeable so the transfer of water is on top of the soil.
Yes because it travels faster
It is the movement of water in soil.
"Groundwater flow is the movement of water that travels and seeps through soil and rock underground. Stored in cavities and geologic pores of the earth's crust, confined groundwater is under a great deal of pressure. Its upper part is lower than the material in which it is confined. Unconfined groundwater is the term for an aquifer with an exposed water surface."
Gravity causes water to flow downwards. In porous ground the water will seep into the soil. If the water hits a non-porous layer (clay, for instance) the water will spread horizontally.
Water can flow into cracks in the rock, then freeze, expand, and crack the rock. This is part of the erosion process.