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

(photo courtesy of Karen Vaughan, Univ. of Idaho)
 
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example 8

dysic, micro, frigid
Lithic Torrifolist

southern Idaho

This thin organic soil has formed on a 2,100-yr-old lava flow at Craters of the Moon National Monument and Preserve. It is composed of up to ~15 cm of slightly to highly decomposed plant debris from the vegetation growing at the site. Common parent vegetation includes Utah juniper, big mountain sagebrush, fernbush, and antelope bitterbrush.

At Craters of the Moon, Lithic Torrifolists form in cracks in lava ranging in age from 2,100 yrs to 15,000 yrs. This represents the initial phase of soil and plant community development on lava flows. The Folists provide vital nutrients and moisture for hardy, drought-tolerant vegetation and, as they increase in volume, eventually create habitat for more plants. Areas of Folists provide habitat for antelope, sage grouse, marmots, snakes, and insects.

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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.