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

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6. Rendoll
southeastern Minnesota

This shallow soil consists of very dark A horizons (mollic epipedon) directly overlying CaCO3-rich parent material of sedimentary origin. Mean annual precipitation is approximately 35 inches.

Rendolls occur in humid regions where they form in highly calcareous parent materials such as limestone and chalk. They are not extensive in the US.
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  Examples:
1. Typic Endoaquoll
Nebraska
2. Argialboll
South Dakota
3. Typic Argiudoll
Iowa
4. Udoll-Aquoll landscape
central Iowa
5. Typic Argiustoll
southeastern South Dakota
6. Rendoll
Minnesota
7. Cryoll landscape
Lemhi Co., ID
8. Pachic Argicryoll
Lemhi Co., ID
9. Argixeroll landscape
Nez Perce Co., ID
10. Lithic Argixeroll
Nez Perce Co., ID
11. Haploxeroll landscape
Teton Co., ID
12. Calcic Haploxeroll
Teton Co., ID
13. Haploxeroll landscape
Latah Co., ID
14. Pachic Ultic Haploxeroll
Latah Co., ID
15. Argixeroll landscape
Benewah Co., ID
16. Oxyaquic Argixeroll
Benewah Co., ID

 

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.