Download presentation
1
Arid region geomorphology...
What causes the erosion and deposition? - Wind, Water, and Gravity
2
Badlands topography with terraces
3
Types of streams in Arid and semi-Arid locales
Exotic streams- begin in areas that are not arid and flow into the desert. Ex. Nile River, Colorado River, Okavango River Local streams (Arroyos) - begin in the arid region, and often end there as well. There are many streams of this type…
4
A dry stream channel (arroyo)
Note the scale of the boulders
5
Nile River- An exotic stream
6
Colorado River-Dammed
7
Alluvial fans & Bajadas in Death Valley Graben
8
Playa lake, Owens Valley, CA
11
Sand Dunes in Colorado Great Sand Dunes National Monument
12
Star Dune in Mexico
13
Star Dune
14
Linear Dunes With an exotic stream wind
15
Barchanoid dunes with smaller transverse & barchanoid dunes superimposed on them
16
Transverse dunes in Namibia- oblique aerial view
17
Transverse dunes in Namibia- ground view
19
Barchan dunes Wind direction Slip face
20
Barchan dunes Wind direction
21
Parabolic dunes -on a topo map
22
Parabolic dunes
24
Erosional landforms vs. Depositional landforms
Erosional forms include... Pediment - bedrock ramp that leads up to the mountain front Plateau- large flat undeformed area that is topographically higher than the surrounding region Mesa- Smaller than the plateau, but basically the same feature Buttes- smaller than the Mesa, but basically the same feature Spires (a.k.a. Hoodoos)- smaller than the buttes
25
Piedmont in Colorado Piedmont is a geographic designation relating to the slope and or foothills leading to a mountain range
26
Colorado Plateau with Grand Canyon
27
A Mesa
28
Buttes and Spires in Monument Valley, Utah
29
Spires, Hoodoos, goblins...
30
Yardangs on Mars
31
Yardang
32
Boulders (foreground) collected from desert pavement (background)
33
Desert Pavement and Desert Varnish
34
Ventifact
35
ventifacts
36
Walking Boulders
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.