University of Idaho College of Agricultural and Life Sciences Plant, Soil & Entomological Sciences Soil & Land Resources
Home
Soil Orders
Maps
Soil Links
  Gelisols    Histosols    Spodosols    Andisols    Oxisols    Vertisols    Aridisols    Ultisols    Mollisols    Alfisols    Inceptisols    Entisols

Histosols

(Photo from University of Idaho)
>> view larger version of this image
>> how to save images
example 3

Haplosaprist landscape
Bonner Co., ID

Soils formed in these flat, low lying landscapes contain very little mineral material and are composed almost entirely of organic matter. They are very poorly drained and have a high water table for most or all of the year.

When drained and cultivated these soils produce high yields; however, once exposed to oxidizing conditions they begin to decompose rapidly and subsidence of the land surface will follow.

<< back to Soil Orders list associated soil >> 
  Examples:
1. Histosol landscape
North Carolina
2. Limnic Haplosaprist
southern Michigan
3. Haplosaprist landscape
northern Idaho
4. Typic Haplosaprist
northern Idaho
5. volume change
in drained organic material
6. subsidence in drained Histosol
Everglades, Florida

7. use of Histosol for fuel
Scotland

8. Lithic Torrifolist
southern Idaho
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.