Download presentation
Presentation is loading. Please wait.
Published byHarold Cain Modified over 8 years ago
1
Ground Water
2
Much of the water in soil seeps downward until it reaches the zone of saturation Zone of Saturation Is the area where water fills all of the open spaces in sediment and rock. Groundwater is the water within this zone The upper limit is called the water table
4
Water within the ground does move The movement depends on the porosity of the soil Groundwater moves by twisting and turning through interconnected small openings The smaller the pores the slower the movement When an impermeable layer of rock exist underground it creates an aquifers that hold water These are used as a source of well water
5
Springs exist when the water table crosses the ground surface Springs are groundwater that moves it’s way to the surface Hot springs are a springs that are about 6-9 degrees warmer then the surface area Many of these springs are in center to western United States
6
Geyser is an intermittent hot spring or fountain in which a column of water shoots up with great force These tend to occur at consistent intervals Old Faithful in Yellowstone National Park These geysers usually have extensive caverns Geysers occur where extensive underground chambers exist within hot igneous rocks
8
1 st Groundwater sinks into the underground caverns 2 nd The water is then heated due to a close magma chamber 3 rd As the water is heated some of it turns to steam and increases the pressure 4 th The pressure is released through a crack in the surface
9
A well is a hole bored into the zone of saturation Irrigation for agriculture is by far the single greatest use of well water in the United States The water table level may change within one year As a large amount of water is used from a well it lowers the water table in that location Artesian wells occur when water is under great pressure and rise on their own
11
Sometimes wells can be overused and that will deplete the water table As it depletes irrigation may need to be found elsewhere This could also lead to the ground sinking due to compaction Runoff of pollution could sink into the ground and contaminate the water supply
12
As water runs through the ground it may dissolve some rocks (limestone) This leads to extensive limestone caverns A cavern is a naturally formed underground chamber The remaining rocks form due to evaporation of water with limestone being left behind These are called “drip stones” Stalactites & Stalagmites
14
Karst Topography occurs in areas that have extensive underground caverns If a cavern collapses from the top down this is what we call a sink hole
Similar presentations
© 2024 SlidePlayer.com. Inc.
All rights reserved.