LOCATION FETTERMAN          WY
Tentative Series
BDM-MRL
06/2005

FETTERMAN SERIES


The Fetterman series consists of moderately deep, well drained soils that formed in slope alluvium over residuum derived from red calcareous sandstone. Fetterman soils are on bedrock controlled footslopes and toeslopes of scarps and hogbacks. Slopes range from 20 to 60 percent. Mean annual precipitation is about 16 inches and the mean annual air temperature is about 44 degrees F.

TAXONOMIC CLASS: Coarse-loamy, mixed, superactive, calcareous, frigid Aridic Ustorthents

TYPICAL PEDON: Fetterman paragravelly silt loam, on a southeast facing, linear-concave, 25 percent slope in bluebunch wheatgrass, threadleaf sedge, and ponderosa pine at an elevation of 5,839 feet. (Colors are for dry soil unless otherwise noted)

A--0 to 3 inches; yellowish red (5YR 5/6) paragravelly silt loam, yellowish red (5YR 4/6) moist; weak fine granular structure; loose, nonsticky and nonplastic; common very fine and fine roots; few very fine and fine vesicular and tubular pores; about 15 percent gravel and 20 percent paragravels; surface covered with about 5 percent gravel and 20 percent paragravels; violently effervescent; carbonates disseminated; moderately alkaline (pH 8.4); clear smooth boundary. (1 to 3 inches thick)

C1--3 to 12 inches; red (2.5YR 5/6) gravelly silt loam, red (2.5YR 4/6) moist; massive; loose, nonsticky and nonplastic; common very fine and fine roots; common very fine and fine vesicular and tubular pores; about 25 percent gravel and 50 percent paragravels; calcium carbonate disseminated; violently effervescent; strongly alkaline (pH 8.6); gradual wavy boundary.

C2--12 to 26 inches; red (2.5YR 5/8) gravelly silt loam, red (2.5YR 4/8) moist; massive; loose, nonsticky and nonplastic; few very fine roots; few very fine vesicular and tubular pores; about 25 percent gravel and 55 percent paragravels; violently effervescent; carbonates disseminated; strongly alkaline (pH 8.8); clear wavy boundary. (Combined C horizons 17 to 39 inches thick)

Cr--26 to 60 inches; soft, red calcareous sandstone.

TYPE LOCATION: Johnson County, Wyoming; About 1,600 feet south and 600 feet west of the northeast corner of Section 34, T. 49 N., R. 83 W.; lat. 44 degrees 10 minutes 40 seconds N. and long. 106 degrees 49 minutes 22 seconds W., NAD 1983. Klondike SW USGS topographic quadrangle.

RANGE IN CHARACTERISTICS:
Mean annual soil temperature: 44 to 47 degrees F.
Surface rock fragments: 5 to 10 percent sandstone gravels, 0 to 10 percent sandstone cobbles, and 0 to 25 percent sandstone paragravels.
Depth to paralithic contact: 20 to 40 inches to red calcareous sandstone.
Particle-size control section (weighted average):
Clay content: 8 to 18 percent.

A horizon:
Hue: 5YR or 7.5YR
Value: 4 or 5 dry; 3 or 4 moist
Chroma: 4 to 6
Texture: loam, silt loam, or fine sandy loam
Rock fragments: 0 to 30 percent sandstone gravel and cobbles; 0 to 35 percent sandstone paragravels
Reaction: slightly alkaline or moderately alkaline

C horizon:
Hue: 5YR or 2.5YR
Value: 4 to 6 dry; 3 to 5 moist
Chroma: 4 to 8
Texture: loam, silt loam, or fine sandy loam
Rock fragments: 0 to 30 percent sandstone gravel and cobbles; 0 to 60 percent sandstone paragravels
Reaction: moderately alkaline or strongly alkaline

COMPETING SERIES: These are the Lodore, Riedel, Sham and Shindy series.
Lodore: moderately deep to a lithic contact.
Riedel: hues of 2.5Y or 10YR.
Sham: very deep; hues of 5Y, 2.5Y or 10YR.
Shindy: very deep

GEOGRAPHIC SETTING:
Parent material: residuum and slope alluvium derived from red calcareous sandstone.
Landform: scarps and hogbacks.
Slopes: 20 to 60 percent.
Elevation: 5,500 to 6,000 feet.
Mean annual air temperature: 42 to 45 degrees F.
Mean annual precipitation: 15 to 19 inches.
Frost-free period: 70 to 105 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Abac (dry phase) and Bloodstone series.
Abac (dry phase) soils: are on backslopes of scarps and hogbacks; have a paralithic contact within 20 inches.
Bloodstone soils: are on backslopes of scarps and hogbacks; have a lithic contact within 20 inches.

DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Well drained; high to very high runoff; moderate saturated hydraulic conductivity.

USE AND VEGETATION: Livestock grazing and wildlife habitat. Native vegetation is bluebunch wheatgrass, threadleaf sedge, ponderosa pine and silver sagebrush. This soil has been correlated to the Loamy 15-19 Northern Plains R043BY422WY ecological site at the type location in Wyoming.

DISTRIBUTION AND EXTENT: Fetterman soils are of small extent in northeastern Wyoming.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Denver, Colorado.

SERIES PROPOSED: Johnson County (Northern Johnson Area), Wyoming, 2005. The name is from a fort in Wyoming.

REMARKS: Diagnostic horizons and features recognized in this pedon are:
Particle-size control section: The zone from 10 to 26 inches. (C1, C2 horizons)
Ochric epipedon: The zone from 0 to 3 inches. (A horizon)
Paralithic contact: The contact with sandstone at 26 inches. (Cr horizon)

Taxonomic version: Ninth edition to the Keys to Soil Taxonomy, 2003.


National Cooperative Soil Survey
U.S.A.