Water will always find its own level. So gravity will cause rainwater to sink into the ground if the surface is porous enough. Water will run off into streams and rivers, more so if the soil is waterlogged already, or if the composition is clay-like.
gravity does do that
gravity does do that
Gravity
The flow of groundwater is an aquifer.
Through porous rock mostly. Also through caves and cracks in the rock.
From aquifers, through artesian basins, springs and wells.
Is surface water
groundwater. not clean though. has to go through processes and stuff
yes through surface run-off or groundwater flow
Yes. Geysers blast boiling groundwater above the surface of the land, taking some groundwater while the groundwater raises somewhere else, so the water cycles through everywhere.
Misconception: Groundwater is a non-renewable resource. Groundwater is constantly renewed by passing from atmospheric or surface water to groundwater in the hydrologic cycle. Misconception: Water from springs is safe without treatment. Although flow through the ground does have a purifying effect on water by filtering sediment, bacteria, and certain chemicals, the purification effect is limited. Large concentrations of chemicals may be too much to be completely removed, and certain chemicals may not be removed by the ground at all. Some groundwater is naturally unsuitable for drinking because of the minerals it has dissolved from the rock through which it flows. Misconception: Groundwater and surface water are separate. Groundwater, surface water, and atmospheric water are intimately related through the earth's water recycling machine, called the hydrologic cycle. Water passes repeatedly through all three parts of the cycle. Misconception: Groundwater flows in underground rivers. Little groundwater flows in open channels beneath the surface. Most flows through fractures in the rock, through millimeter sized opening between layers, and between the grains of the rock.
Groundwater is any water present below the earth's surface. An aquifer is a porous and permeable zone in a rock or soil through which ground water flows.