Eolian Depositional Systems
This page was created by Michael D.Vanden Berg, University
of Utah
Eolian processes in general
Complexities of the System
- Modeling problems, as in all system studies - however,
it is one of the best understood systems because the processes
occur rapidly enough that we can see them happening.
- Preservation - accumulation
space may not coincide with preservation space
- Factors that promote preservation
- Subsidence
- Rise in water table - stabilization due to increase in
vegetation
- Paleoclimate interpretation problems
- System may not be in equilibrium with current conditions
Remote Sensing of Arid
Lands
- New remote sensing systems are proving to be especially helpful
in the effort to understand arid lands. Landsat satellites provide
excellent data with which to monitor temporal variations in a
given area.
- Radar systems have been used to look under the sand at features
that are not visible in the field. This technology has been used
to find unknown archaeological sites in Egypt and the Sudan.
- The Desert Winds Project was set up by the USGS in order
to study climate conditions in the American southwest. The goal
is to study long-term changes produced by wind in deserts of
differing geologic and climatic types.
- Tigges, Richard, Carol S. Breed, and Paula J. Helm, 1999.
Design and operations of Geomet stations of the Desert Winds
Project. USGS Professional Paper, 1598; 133-153.
- USGS
Flagstaff Field Center website - provides information
on the Desert Winds Project and data collected from the American
deserts.
Eolian processes on Mars
- The Martian surface is greatly modified by the wind; atmospheric
dust storms, dust devils and possible tornado tracks were all
photographed by Viking.
- Other eolian features can be seen on the surface of Mars
such as dunes, yardings, wind ripples, and wind scour.
- To see great pictures of these features and more check out
these websites:
- Recent Mars eolian articles:
- Bridges, Nathan T. et al, 1999. Ventifacts at the
Pathfinder landing site. Journal of Geophysical Research.
104, 4; 8595-8615.
- Edgett, Kenneth S. and Michael C. Malin, 2000. New views
on Mars eolian activity, materials, and surface properties; three
vignettes from the Mars Global Surveyor and Mars Orbiter Camera.
Journal of Geophysical Research. 105, 1; 1623-1650.
- Edgett, Kenneth S. and Philip R. Christensen, 1997. Rocks
and Aeolian features in the Mars Pathfinder landing site region;
Viking infrared thermal mapper observations. Journal of Geophysical
Research. 102, 2; 4107-4116.
- Greeley, Ronald et al, 1999. Aeolian features and
processes at the Mars Pathfinder landing site. Journal of
Geophysical Research. 104, 4; 8573-8584.
- Kraft, Michael D. and Ronald Greeley, 2000. Rock coatings
and aeolian abrasion on Mars; application to the Pathfinder landing
site. Journal of Geophysical Research. 105, 6; 107-116.
- Also, the February 2001 issue of National Geographic has
a great article on Mars with extraordinary pictures.
Desertification
- Desertification is the degradation of the land in dry areas
caused by climatic changes and human activities. The result is
the destruction of topsoil followed by loss of the land's ability
to sustain crops, livestock or human activity.
- Humans have interfered with natural cycles and have increased
the susceptibility of land to become desert wastelands. Over-grazing,
land clearance, and over-cropping cultivated lands are all factors
that increase desertification.
- Increased wind blown dust from the desertification of Africa
has been linked to widespread destruction of Caribbean corals.
- Useful websites on desertification:
- Recent articles on desertification:
- Albaladejo, J. et al, 1998. Soil degradation and desertification
induced by vegetation removal in a semiarid environment. Soil
Use and Management. 14, 1; 1-5.
- Fonseca, R., F. Barriga, and W. Fyfe, 1998. Reversing desertification
by using dam reservoir sediments as agriculture soils. Episodes.
21, 4; 218-224.
- Lin Nianfeng, Tang Jie, Zhang Dianfa, 1999. The problem of
the Quaternary, geological environment and desertification. Environmental
Geology. 38, 1; 7-12.
Other references:
- Busch, Richard M. ed. 1992. Laboratory
Manual in Physical Geology. 4th edition. Prentice Hall.
- Kocurek G. and Havholm K.G. 1993. Eolian
sequence stratigraphy - a conceptual framework. In: Siliciclastic
Sequence Stratigraphy: Recent Developments and Applications.
pp. 393-409. Mem. Am. Ass. petrol. Geol., 58.
- Montgomery, Carla W. 1995. Environmental
Geology. 4th edition. Wm. C. Brown Publishers.
Last updated 9/10/01