WATER UNDERGROUND

Underground Water

Underground water comes from precipitation that soaks into the ground.

The water underground trickles down between particles of soil and through cracks and spaces in layers of rock – pore spaces

Permeable Different types of rock

and soil have different-sized spaces, or pores, between their particles.

Materials that allow water to pass through easily are called permeable.

When water soaks down into the ground, it passes through permeable materials.

Eventually it reaches an impermeable layer.

There, it stops trickling down and begins to fill the spaces in the permeable layer above it.

Impermeable Materials that do not allow water to pass through easily are called impermeable.

A news report from 2011 states

An underground river has now been discovered beneath the mighty Amazon River, flowing miles below the surface.

Scientists detected this river after they analyzed data from 241 oil wells that were drilled in the 1970s and 1980s.

The river was unofficially named the Hamza by scientists at Brazil's National Observatory in honor of their colleague, geophysicist Valiya Hamza.

This is the Amazon River Basin

Hamza River

US Aquifers

Aquifers in Georgia

Ogallala Aquifer

The aquifer was first tapped for irrigation in 1911.

Large-scale use for irrigation began in the 1930s and continued through the 1950s, due to the availability of electric power to rural farming communities and the development of cheap

irrigation

Is adding water to crops to help them grow

Saturated thickness of the Ogallala Aquifer in 1997 after several decades of intensive withdrawals: The breadth

and depth of the aquifer generally decrease from north to south

Groundwater withdrawal rates (fresh water, all sources) in 2000.

Image of fields in Kansas watered by the Ogallala aquifer using center pivot

irrigation systems

Water Table The permeable layer that becomes

filled with water is called the saturated zone.

The level of the top of the water in the saturated zone is called the water table.

The layer of rocks and soil above the water table is called the unsaturated zone (permeable zone)

Spring A spring is a place where groundwater bubbles or flows out of cracks in the rock.

Aquifer An aquifer is an

underground layer of rock or sediment where water has collected.

The water in an aquifer seeps through the permeable rock layers where it is stored.

People can obtain groundwater from an aquifer by drilling a well below the water table.

If a hole is drilled in the impermeable layer above it, the water flows out of the aquifer without being pumped.

Artesian Well A well in which water rises because of pressure within the aquifer

Geyser The water in some springs

is warm or even hot. The water is heated by hot

rocks deep underground.

A geyser is a hot spring in which the water is under pressure.

From time to time, the pressure causes the hot water and steam to erupt into the air.

Yellowstone caldera

http://www.nps.gov/features/yell/live/live4.htm

https://www.youtube.com/watch?v=X4zA_YPCyHs

https://www.youtube.com/watch?v=wE8NDuzt8eg

Questions to Answer

1.How does water move through underground layers of soil and rock?

2.How do people obtain water from an aquifer?