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Mollisols
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15. Argixeroll
landscape
Benewah Co., ID
Soils on these gently rolling landscapes are
formed in thick deposits of loess. Much of this
once-forested land has been cleared for
agriculture. While these soils can be very
productive, erosion and drainage issues
associated with the loess parent material and
underlying argillic horizon, can present problems
for their managment.
For more
information on the Southwick series, click here.
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Examples:
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1.
Typic Endoaquoll
Nebraska |
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2. Argialboll
South Dakota |
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3.
Typic Argiudoll
Iowa |
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4.
Udoll-Aquoll landscape
central Iowa |
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5.
Typic Argiustoll
southeastern South Dakota |
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6. Rendoll
Minnesota |
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7.
Cryoll landscape
Lemhi Co., ID |
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8.
Pachic Argicryoll
Lemhi Co., ID |
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9.
Argixeroll landscape
Nez Perce Co., ID |
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10.
Lithic Argixeroll
Nez Perce Co., ID |
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11.
Haploxeroll landscape
Teton Co., ID |
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12.
Calcic Haploxeroll
Teton Co., ID |
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13.
Haploxeroll landscape
Latah Co., ID |
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14.
Pachic Ultic Haploxeroll
Latah Co., ID |
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15.
Argixeroll landscape
Benewah Co., ID |
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16.
Oxyaquic Argixeroll
Benewah Co., ID |
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