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Soilscape of Icknuun soils; Anchorage area, Alaska

The Icknuun series (a hydric soil) consists of very deep, very poorly drained soils that formed in organic material interlayered with thin strata of mineral material. Icknuun soils are in depressions on till plains. Slopes range from 0 to 3 percent.

 

Hydric soils are formed under conditions of saturation, flooding, or ponding long enough during the growing season to develop anaerobic conditions in the upper part (Federal Register, 1994). Most hydric soils exhibit characteristic morphologies that result from repeated periods of saturation or inundation that last more than a few days.

 

To download the latest version of "Field Indicators of Hydric Soils" and additional technical references, visit:

www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/ref/?cid=s...

 

TAXONOMIC CLASS: Euic Fluvaquentic Cryohemists

 

USE AND VEGETATION: Wildlife habitat and recreation. The natural vegetation is mainly sedges, sphagnum moss, bog birch, Labrador tea, and other low-growing shrubs and forbs.

 

DISTRIBUTION AND EXTENT: Cook Inlet-Susitna Lowlands. The series is of small extent.

 

For a detailed description, visit:

soilseries.sc.egov.usda.gov/OSD_Docs/I/ICKNUUN.html

 

For geographic distribution, visit:

casoilresource.lawr.ucdavis.edu/see/#icknuun

 

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Uploaded on February 27, 2022
Taken on June 4, 2008