Search Header Logo
Aquifers and Groundwater

Aquifers and Groundwater

Assessment

Presentation

Science

10th - 12th Grade

Hard

Created by

Joseph Anderson

FREE Resource

5 Slides • 8 Questions

1

Groundwater

Where is Groundwater Found?

Slide image

2

What is Groundwater?

  • Free water that occurs deep below the surface

  • Found in the "pore spaces" betweens gains of sediment or sedimentary rock.

  • May also accumulate in the fractures of impermeable rock.

  • Soluble rock like limestone, may dissolve and water occurs in subterranean caves.

3

Multiple Choice

Which of these is not a place in which groundwater accumulates?

1

Subterranean limestone caves

2

pore spaces of sedimentary rock

3

hollow spaces between minerals in granite

4

Interconnected fractures in rock

4

How Does Groundwater Accumulate?

  • When rain or snow melts it can seep into the subsurface through the unsaturated zone and be trapped in the saturated zone.

  • The upper boundary of the saturated zone is known as the water table.

  • If the water table intersects the surface it can form a lake, stream, swamp or spring.

5

Multiple Choice

Groundwater results from the infiltration of rain and snowmelt into the subsurface.

1

True

2

False

6

Multiple Choice

The upper limit of groundwater is referred to as the

1

unsaturated zone

2

saturated zone

3

water table

7

Porosity

  • Refers to the the amount of open space within a rock or sediment that can hold water.

  • Rounded sediment has greater porosity than angular sediment.

  • Sedimentary rocks, like shale and sandstone, tend to have high porosity

  • Whereas metamorphic & igneous rocks , like granite and gneiss, tend to have lower porosity.

8

Permeability

  • is a measure of the ability of a material to transmit a fluid.

  • Is related to the size and interconnectedness of the pore spaces.

  • higher porosity leads to high permeability.

  • fractures can also increase permeability.

  • Highly compacted clay particles reduce it's permeability.

  • conglomerate rock and sandstone are two examples of high-permeability rocks.

9

Multiple Choice

A measure of how much water a rock can hold

1

porosity

2

permeability

10

Multiple Choice

Sediment grain shape influences porosity in that ____ shape has greater porosity.

1

rounded

2

angular

11

Multiple Choice

Igneous and metamorphic rocks tend to have high porosity.

1

True

2

False

12

Multiple Choice

Which of these settings produces the lowest permeability?

1

rocks with many interconnected fractures

2

highly compacted clay particles

3

loosely cemented gravel and sand

13

Multiple Select

Check the two rocks that have high permeability and allows water to accumulate in large quantities as groundwater.

1

granite

2

sandstone

3

conglomerate

4

shale

Groundwater

Where is Groundwater Found?

Slide image

Show answer

Auto Play

Slide 1 / 13

SLIDE