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Landform Geography

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Title: Slide 1 Author: Lawrence McGlinn Last modified by: COAS Created Date: 12/28/2006 2:09:16 AM Document presentation format: On-screen Show (4:3) – PowerPoint PPT presentation

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Title: Landform Geography


1
Landform Geography
Groundwater and Karst Landscapes
2
Movement Storage of Groundwater
  • Precipitation sinks into soils 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

3
Fate of Precipitation on Soil
4
Soil-Water Conditions
5
Saturated Zones Aquicludes
6
High Plains (Ogallala) Aquifer
  • Underlies much of Great Plains from TX to SD
  • Water deposited in Ice Ages 1.6 M-10K yrs ago

7
High Plains (Ogallala) Aquifer
  • Heavy usage, esp. center-pivot irrigation
  • Drawdown significant in parts of aquifer

Center-Pivot Irrigation
Drawdown
8
Artesian Wells and Springs
  • Natural pressure brings water to surface in
    artesian well

9
Patterns of Groundwater Depletion
  • Cone of Depression cone-shaped depression in
    water table that occurs around a well

10
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

11
Groundwater Contamination
  • Dumped chemicals can be carried by moving
    groundwater to sources of drinking water
  • Recent federal rules have reduced uncontrolled
    dumping and contamination

12
Karst Landforms
  • Caves, sinkholes and other soluble rock features
  • Form in extensive, thick deposits of limestone
  • Limestone 80 calcium carbonate dissolves
    easily through carbonation

13
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

14
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

15
Sinkhole Landscape
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