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Landform Geography Groundwater and Karst Landscapes

Landform Geography Groundwater and Karst Landscapes

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Page 1: Landform Geography Groundwater and Karst Landscapes

Landform Geography

Groundwater and

Karst Landscapes

Page 2: Landform Geography Groundwater and Karst Landscapes

Movement & Storage of Groundwater

• Precipitation sinks into soil’s soil-water belt

• In dry soil, water is held tight by sediment grains as hygroscopic water – unavailable for plants

• When pore spaces within soil full of water, soil at Field Capacity – additional water flows down into unsaturated zone

• Water collects above an impermeable aquiclude to form saturated zone

• Large saturated zone is aquifer

Page 3: Landform Geography Groundwater and Karst Landscapes

Fate of Precipitation on Soil

Page 4: Landform Geography Groundwater and Karst Landscapes

Soil-Water Conditions

Page 5: Landform Geography Groundwater and Karst Landscapes

Saturated Zones & Aquicludes

Page 6: Landform Geography Groundwater and Karst Landscapes

High Plains (Ogallala) Aquifer

• Underlies much of Great Plains from TX to SD

• Water deposited in Ice Ages 1.6 M-10K yrs ago

Page 7: Landform Geography Groundwater and Karst Landscapes

• Heavy usage, esp. center-pivot irrigation

• Drawdown significant in parts of aquifer

High Plains (Ogallala) Aquifer

Center-Pivot Irrigation Drawdown

Page 8: Landform Geography Groundwater and Karst Landscapes

Artesian Wells and Springs• Natural

pressure brings water to surface in artesian well

Page 9: Landform Geography Groundwater and Karst Landscapes

Patterns of Groundwater Depletion• Cone of

Depression – cone-shaped depression in water table that occurs around a well

Page 10: Landform Geography Groundwater and Karst Landscapes

Subsidence

• Settling or sinking of a surface due to removal of water or sediment from below

• Worst around large cities such as Venice, Italy and agricultural regions such as the San Joaquin Valley of California

Page 11: Landform Geography Groundwater and Karst Landscapes

Groundwater Contamination• Dumped chemicals can be carried by moving

groundwater to sources of drinking water

• Recent federal rules have reduced uncontrolled dumping and contamination

Page 12: Landform Geography Groundwater and Karst Landscapes

Karst Landforms

• Caves, sinkholes and other soluble rock features

• Form in extensive, thick deposits of limestone

• Limestone 80%+ calcium carbonate – dissolves easily through carbonation

Page 13: Landform Geography Groundwater and Karst Landscapes

Caves and Caverns• Caves – underground

voids in rock big enough for people to enter

• Cavern – large cave system

• Form just below water table in limestone – when

water table falls, empty caverns are exposed

Page 14: Landform Geography Groundwater and Karst Landscapes

Karst Topography - Sinkholes

• Most common surface feature of karst is sinkhole

• Sinkhole – depression in regions of cavernous limestone – forms from collapse of cave

• Often found with disappearing streams that enter underground channels

• Some sinkholes fill with water, forming ponds

• Sinkholes can be hazards, collapsing under homes or roads

Page 15: Landform Geography Groundwater and Karst Landscapes

Sinkhole Landscape