Ground water is formed when water fully saturates pores/cracks in the soil filling the ground with water and creating a mass of water underground. The main minerals in groundwater are sodium, calcium, magnesium, potassium, chloride, bicarbonate, and sulfate.
when water percolates down through the soil
Ap#x
tired of these explanations that don't get us anywhere.
When water percolates down through the soil.
when water percolates down through the soil
When water percolates down through the soil. (APEX)
yes it can be formed
Because there is dirt on the ground and when dirt and water are mixed it turns into mud.
1. A mineral can be formed through evaporating salt water which is when salt water evaporates. you can do this at home with a bottle and mix salt and water together and see what happens when it dries up. Examples: Gypsum and Halite 2. A mineral can also be formed through hot water solutions which is when ground water works its way down and is boiled by ground magma. Examples are Gold, copper sulfur pyrite and galena.
Swamps are low-lying areas of uncultivated ground near larger bodies of water. They are formed due to the accumulation of water and poor drainage system.
Extrusive igneous rocks and some sedimentary rocks are formed above ground.
When water percolates down through the soil.
Air frost - or ground frost
when there is a crack in the ground ,the ground exerts pressure and makes the water squirt from the ground forming a spring.
To the best of my knowledge, the water under the surface was formed when the oceans were formed, or thereafter. In simple terms, cracks in the ground allows water to leak below ground into large open voids.
either dew or fog
yes it can be formed
condensation from the ceiling drops water onto the ground and over the years it drops more and more water and the water dries and the minerals in it build up until it rises out of the ground .... stalagmites are rare as they come from the ground ... normally you find stalactites
i dint know.
4 land forms
ground water is formed by the percolation action of the soil where the water seeps through the porous top soil until it settles upon the surface of the bed rock which is nonporous in many cases. this collection of the percolating water causes ground water
Karst caves, and it is the majority of caves; formed by acidic ground-water dissolving the limestone.
well's occurs when the water underground meets the surface