Landform Geography Lecture 5 - PowerPoint PPT Presentation

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Landform Geography Lecture 5

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Lecture 5 Mass Wasting Events Groundwater * * * * * * * If spread across the U.S. the aquifer would cover all 50 states with 1.5 feet of water If drained, it would ... – PowerPoint PPT presentation

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Title: Landform Geography Lecture 5


1
Landform GeographyLecture 5
Mass Wasting Events Groundwater
2
Mass Wasting
  • Large volumes of sediment moving down hill slopes
    under force of gravity
  • Types

3
Solifluction
  • Form of soil creep in tundra landscapes
  • Surface of permafrost melts soil sags down
    slope in uneven lobes

4
Earth Flow
  • Slow-to-rapid movement of wet soil other loose
    sediment over a broad surface
  • One of 3 types of Flow mass movement of wet
    sediment

5
Mudflow
  • Fine textured sediments that move very quickly
    down slope occur after heavy rainfall
  • Lahar Indonesian word for volcanic mudflow

6
Debris Flow
  • Mud, boulders, trees, etc. flowing down slope
    after heavy rainfall very dangerous

La Conchita, CA Debris Flow
7
Slump
  • Slide where rock sediment rotates moves down
    slope along plane concave to surface
  • Happens on slopes w/ soft deposits rich in clay
    and shale

8
Debris Slide
  • Type of Landslide mass of rock, regolith soil
    that flows downhill
  • Slope failure along a plane roughly parallel to
    the slope

Madison Slide, Montana
9
Soil Creep
  • Slowest mass wasting process
  • Force of gravity slowly pulls soil particles down
    hill features of hill shift down hill, as well

10
Rockfall
  • Process in which rocks break free from cliff
    faces rapidly tumble into valley below

11
Avalanche
  • Large mass of snow or rock that suddenly slides
    down a mountainside

Weathering and Mass Movements
12
Groundwater and Karst Landscapes
  • Movement Storage of groundwater
  • High Plains aquifer
  • Subsidence
  • Groundwater contamination
  • Karst Landforms Landscapes
  • Caves Caverns
  • Karst topography

13
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

14
Fate of Precipitation on Soil
15
Soil-Water Conditions
16
Saturated Zones Aquicludes
Hydrologic Cycle and Groundwater
17
High Plains (Ogallala) Aquifer
  • Underlies much of Great Plains from TX to SD
  • Water deposited in Ice Ages 1.6 M-10K yrs ago

18
High Plains (Ogallala) Aquifer
  • Heavy usage, esp. center-pivot irrigation
  • Drawdown significant in parts of aquifer

Center-Pivot Irrigation
Drawdown
19
Artesian Wells and Springs
  • Natural pressure brings water to surface in
    artesian well

20
Patterns of Groundwater Depletion
  • Cone of Depression cone-shaped depression in
    water table that occurs around a well

21
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

22
Groundwater Contamination
  • Dumped chemicals can be carried by moving
    groundwater to sources of drinking water
  • Recent federal rules have reduced uncontrolled
    dumping and contamination
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