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Mollisols
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1. Typic Endoaquoll
Nebraska
(Loup series)
These very deep soils have
formed in loamy and sandy alluvium and have a water table at or
near the surface for much of the year. Because of the high water
table, most of these soils remain in native grasses and are used
for hayland and grazing. The gray colors of the Cg horizons result
from prolonged periods of saturation in which iron is reduced to
more mobile, colorless forms.These soils belong to the Loup series,
which is extensive in the Nebraska sandhills and in parts of South
Dakota and Colorado. In WRB, this soil is classified as a Mollic
Gleysol.
For more information on Loup soils, 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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