University of Idaho College of Agricultural and Life Sciences Plant, Soil & Entomological Sciences Soil & Land Resources
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Andisols

(Photo from University of Idaho)
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Reference: Thorsteinsson, I. 1977. Vegetation and land use (in Icelandic). Lesarkir Landverndar 2, Landvernd, Reykjavik, Iceland.
example 8

eroded Cryand landscape
Iceland

Many highland landscapes of Iceland originally consisted of deep Andisols overlying glacial till. However, centuries of overgrazing by sheep and the high susceptibility of these Andisols to wind erosion have resulted in landscapes such as the one illustrated in this photo. In the foreground, rocky glacial till has been exposed by erosion of the overlying Andisol, thereby promoting desertification. Only sparse vegetation is supported by the glacial till despite an annual precipitation of 1100 mm. An Andisol ~1.5 m thick can be seen (middle part of photo) supporting healthy vegetation. It has been estimated that the vegetative cover of Iceland has been reduced by >60% since settlement because of overgrazing and soil erosion

For more information on desertification in Iceland, visit
http://www.rala.is/desert/.

<< back to soils list associated soil   >> 
  Examples:
1. Hydrudand landscape
Hawaii
2. Acrudoxic Hydrudand
3. Melanudand landscape
Costa Rica
4. Melanudand
Costa Rica
5. Vitrixerand landscape
northern Idaho
6. Volcanic ash
Mt. Mazama Oregon
7. Typic Vitrixerand
northern Idaho
8. eroded Cryand landscape
Iceland
9. Cryand
Iceland
If you have any comments, suggestions, or questions about the 12 Soil Orders web site,
please contact
Dr. Paul McDaniel  at the Soil Science Division,
University of Idaho, Moscow, ID 83844-2339.