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Desert Landscapes
Dominated by Wind
“We don’t survive the desert,
  we live here”
   - Pima Indian
Deserts: where & why
 Earth’s dry regions: 30% of all land
 2 climate types of dry regions:
    ◦ desert (arid)
    ◦ steppe (semi-arid, surrounds deserts)
   Question:How much rain do deserts get
    every year?
    ◦ Sahara Desert receives as little as 2mm and as
      much as 100mm of precipitation per year
Climate Graphs – Semi-arid and Arid
What do you notice about the minimum and maximum temperatures?
What do you notice about the amount of precipitation?
Deserts: where & why
 What causes deserts?
 Global distribution of
    ◦ air pressure
    ◦ wind


   Relationship between
    ◦ rainfall
    ◦ evaporation
Deserts: where & why
   Low-latitude deserts
    ◦ Tropic of Cancer
    ◦ Tropic of Capricorn


   In contrast….
    ◦ Equator:
       hot air
       rises to 15-20 km
       low pressure belt
Deserts: where & why
Deserts: where & why
Deserts: where & why
Deserts: where & why
Deserts: where & why
   Middle-latitude deserts (ie. 45°N)
    ◦ exist in rain shadows.
Deserts: where & why
Middle-latitude deserts
The Great Basin
   Basin (valley) and
    Range (mountains)
    topography
    ◦ mountainous desert
      landscape
    ◦ Nevada, Arizona,
      California, Utah
    ◦ Death Valley,
      Mojave Desert,
      Great Salt Lake
Great Salt Lake, Utah
Evaporation > Precipitation
   Playa: ephemeral (not existing all year
    long) lake beds that consist of salt and
    mud flats




        Spotted Lake, just outside of Osoyoos, BC
Wind erosion + deposition
 Wind erosion: Important in arid
  environments
 Example…Sand dune shape depends
  on:
    ◦   Flat or hilly?
    ◦   How much sand?
    ◦   Winds steady or intermittent?
    ◦   Wind direction constant?
    ◦   Vegetation present?
Wind erosion
   Desert pavement
Wind erosion
   Deflation: the process of wind
    removing silt and sand-sized particles
Wind erosion + deposition
   Ergs: seas of dunes
Wind erosion + deposition
   Sand dune formation
Wind erosion
   Ventifacts: rocks abraded, pitted,
    polished by windblown sand
Wind Deposition
   Loess from Aeolian
    (or Eolian)
    transportation:
    ◦ Deposit of wind-
      blown silt and clay in
      angular grains and
      weakly cemented by
      calcite
    ◦ Develop rich, fertile
      soils
Water Erosion
   Wadi: a dried up river bed that only
    has water during rainy season




                               Town of WadiTiwi,
                               Oman
Water Erosion
                                    Hoodoos (or fairy
                                     chimneys): column
                                     of soft sedimentary
                                     rock often with
                                     resistant layer of
                                     “cap” rock on top
                                    Water flows
                                     through badlands
                                     causing further
                                     erosion to the
Bryce Canyon National Park, Utah
                                     spires
Water Erosion
Fairy chimneys that people still live inside in Cappadocia,
Turkey
Water Erosion
                 Antelope Slot
                  Canyons, Page,
                  AZ
                 Flash floods from
                  localized
                  thunderstorms
                  carry sediments
                  that abrade and
                  polish the
                  sandstone
Water Erosion
Mesa: a flat-topped “table” formed by
differential erosion of softer rock
underneath a layer of “cap” rock
Water Erosion
  Butte: a smaller version of a mesa
Water Erosion
                   Pedestal rock:
                    softer rock erodes
                    quicker than
                    resistant “cap” rock
Water Deposition
Alluvial Fan: deposition of sediments as rivers or flash
floods leave mountain ranges and spread into the
valley
Water Deposition
   Bajada: several adjacent alluvial fans
    that have merged together
Desert landscapes dominated by wind

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Desert landscapes dominated by wind

  • 2. “We don’t survive the desert, we live here” - Pima Indian
  • 3.
  • 4.
  • 5. Deserts: where & why  Earth’s dry regions: 30% of all land  2 climate types of dry regions: ◦ desert (arid) ◦ steppe (semi-arid, surrounds deserts)  Question:How much rain do deserts get every year? ◦ Sahara Desert receives as little as 2mm and as much as 100mm of precipitation per year
  • 6. Climate Graphs – Semi-arid and Arid What do you notice about the minimum and maximum temperatures? What do you notice about the amount of precipitation?
  • 7. Deserts: where & why  What causes deserts?  Global distribution of ◦ air pressure ◦ wind  Relationship between ◦ rainfall ◦ evaporation
  • 8. Deserts: where & why  Low-latitude deserts ◦ Tropic of Cancer ◦ Tropic of Capricorn  In contrast…. ◦ Equator:  hot air  rises to 15-20 km  low pressure belt
  • 13. Deserts: where & why  Middle-latitude deserts (ie. 45°N) ◦ exist in rain shadows.
  • 14. Deserts: where & why Middle-latitude deserts
  • 15. The Great Basin  Basin (valley) and Range (mountains) topography ◦ mountainous desert landscape ◦ Nevada, Arizona, California, Utah ◦ Death Valley, Mojave Desert, Great Salt Lake
  • 17. Evaporation > Precipitation  Playa: ephemeral (not existing all year long) lake beds that consist of salt and mud flats Spotted Lake, just outside of Osoyoos, BC
  • 18.
  • 19. Wind erosion + deposition  Wind erosion: Important in arid environments  Example…Sand dune shape depends on: ◦ Flat or hilly? ◦ How much sand? ◦ Winds steady or intermittent? ◦ Wind direction constant? ◦ Vegetation present?
  • 20. Wind erosion  Desert pavement
  • 21. Wind erosion  Deflation: the process of wind removing silt and sand-sized particles
  • 22. Wind erosion + deposition  Ergs: seas of dunes
  • 23.
  • 24. Wind erosion + deposition  Sand dune formation
  • 25.
  • 26.
  • 27. Wind erosion  Ventifacts: rocks abraded, pitted, polished by windblown sand
  • 28. Wind Deposition  Loess from Aeolian (or Eolian) transportation: ◦ Deposit of wind- blown silt and clay in angular grains and weakly cemented by calcite ◦ Develop rich, fertile soils
  • 29. Water Erosion  Wadi: a dried up river bed that only has water during rainy season Town of WadiTiwi, Oman
  • 30.
  • 31.
  • 32. Water Erosion  Hoodoos (or fairy chimneys): column of soft sedimentary rock often with resistant layer of “cap” rock on top  Water flows through badlands causing further erosion to the Bryce Canyon National Park, Utah spires
  • 33. Water Erosion Fairy chimneys that people still live inside in Cappadocia, Turkey
  • 34. Water Erosion  Antelope Slot Canyons, Page, AZ  Flash floods from localized thunderstorms carry sediments that abrade and polish the sandstone
  • 35. Water Erosion Mesa: a flat-topped “table” formed by differential erosion of softer rock underneath a layer of “cap” rock
  • 36. Water Erosion Butte: a smaller version of a mesa
  • 37. Water Erosion  Pedestal rock: softer rock erodes quicker than resistant “cap” rock
  • 38. Water Deposition Alluvial Fan: deposition of sediments as rivers or flash floods leave mountain ranges and spread into the valley
  • 39. Water Deposition  Bajada: several adjacent alluvial fans that have merged together