LOCATION WHITECROSS         CO
Established Series
Rev. JPP/GB/TWH
07/2002

WHITECROSS SERIES


The Whitecross series consists of shallow or very shallow, well drained soils that formed in slope alluvium and colluvium derived from rhyolite, tuff, and similar volcanic rocks. Whitecross soils are on alpine valley floors, mountain slopes, and ridges. Slopes range from 15 to 75 percent. The mean annual precipitation is about 39 inches and the mean annual air temperature is about 32 degrees F.

TAXONOMIC CLASS: Loamy-skeletal, isotic Lithic Dystrocryepts

TYPICAL PEDON: Whitecross very stony sandy loam, on a south facing, 60 percent slope in alpine tundra at an elevation of 12,300 feet. (Colors are for dry soil unless otherwise noted.) When described on July 21,1983 the soil was moist throughout. The surface is covered by tundra.

Oi--0 to 1 inch; slightly decomposed organic material, principally roots, stems, and leaves. (1 to 3 inches thick)

A--1 to 4 inches; brown (7.5YR 5/2) very stony sandy loam, brown (7.5YR 4/2) moist; weak fine granular structure; soft, very friable, nonsticky and nonplastic; 20 percent gravel, 10 percent cobbles, 15 percent stones; moderately acid (pH 6.0); clear smooth boundary. (2 to 4 inches thick)

Bw1--4 to 10 inches; reddish brown (5YR 5/3) very gravelly loam, reddish brown (5YR 4/3) moist; weak fine granular structure; soft, very friable, nonsticky and nonplastic; 25 percent gravel, 10 percent cobbles, 5 percent stones; strongly acid (pH 5.4); gradual wavy boundary. (2 to 6 inches thick)

Bw2--10 to 19 inches; light reddish brown (5YR 6/4) extremely gravelly sandy loam, reddish brown (5YR 4/4) moist; moderate medium granular structure; soft, very friable, nonsticky and nonplastic; 40 percent gravel, 15 percent cobbles, 10 percent stones; strongly acid (pH 5.2); abrupt wavy boundary. (3 to 10 inches thick)

R--19 inches; fractured rhyolite.

TYPE LOCATION: San Juan County, Colorado; along trail in Kendall Gulch approximately 2 miles southeast of Silverton, Colorado; located in an unsectionized area about 600 feet east and 50 feet north of the projected southwest corner of Sec. 22, T. 42 N., R. 7 W. Silverton USGS quad.; lat. 37 degrees, 47 minutes, 22 seconds N., and long. 107 degrees, 37 minutes, 48 seconds W., NAD 27

RANGE IN CHARACTERISTICS: (depths given are measured from the mineral soil surface)
Soil moisture regime: udic; dry in some part of the moisture control section for less than 45 cumulative days (typic udic subclass)..
Mean annual soil temperature: 32 to 38 degrees F.
Mean summer soil temperature: 38 to 44 degrees F. with an O horizon
Depth to lithic contact: 7 to 20 inches
Base saturation: 30 to 60 percent (estimated)

Particle-size control section:
Clay content: 10 to 18 percent
Rock fragment content: 35 to 80 percent

A horizon:
Hue: 5YR or 7.5YR
Value: 5 to 7 dry, 3 or 4 moist
Chroma: 2 or 3, dry and moist
Texture (fine earth fraction): SL, L
Reaction: strongly acid or moderately acid

Bw horizon:
Hue: 5YR or 7.5YR
Value: 5 or 6 dry, 4 or 5 moist
Chroma: 3 to 6, dry and moist
Texture (fine earth fraction): L or SL
Rock fragments: 35 to 80 percent
Reaction: very strongly acid to moderately acid

COMPETING SERIES: These are the Discovery, Luckiamute, Shanty, and Winberry Series.
In addition, this soil may be a competitor when the classification is updated: Hechtman.

Discovery soils: have hue of 10YR or yellower.
Hechtman soils: have an albic horizon with hue yellower than 7.5YR
Luckiamute soils: have 27 to 35 percent clay in the particle-size control section.
Shanty: have hue of 10YR.
Winberry soils: have mean annual soil temperature greater than 38 degrees F and border a xeric moisture regime.

GEOGRAPHIC SETTING:
Parent material: slope alluvium and colluvium derived from rhyolite, tuff, and similar volcanic rocks.
Landform: alpine valley floors, mountain slopes, and ridges.
Slopes: 15 to 75 percent
Elevation: 10,800 to 13,800 feet
Mean annual air temperature: 26 to 34 degrees F.
Mean annual precipitation: 33 to 60 inches.
Wettest months: July and August receive slight more precipitation than other months.
Driest months: May and June receive the least precipitation, however the soils are still snow covered through mid June.
Frost-free period: 20 to 40 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Henson, Telluride, and Moran series. All are on mountain slopes.

Henson and Moran soils are very deep, and are in valley fill positions.
Telluride soils have umbric epipedons, and are also on ridges and on valley floors.

DRAINAGE AND PERMEABILITY: Well drained, medium runoff, moderately rapid permeability.

USE AND VEGETATION: These soils are used for recreation, wildlife habitat, and summer sheep grazing. Native vegetation is kobresia, alpine bluegrass, alpine fescue, tufted hairgrass, Ross' avens, and sedges.

DISTRIBUTION AND EXTENT: Alpine areas of the southern Rocky Mountains of Colorado. LRR E, MLRA 48A. The series is of moderate extent.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Bozeman, Montana

SERIES ESTABLISHED: Ouray Soil Survey Area, Colorado, 1998. The type location is in the Animas-Dolores Soil Survey Area, Colorado.

REMARKS: Diagnostic horizons and features recognized in this pedon are:
Ochric epipedon: The zone from 1 to 4 inches. (A horizon)
Cambic horizon: The zone from 4 to 19 inches. (Bw horizons)
Particle-size control section: The zone from 11 to 19 inches (part of the Bw2 horizon)
Lithic contact: Hard rhyolite at 19 inches.

Keys to Soil Taxonomy: Series classified according to Eighth Edition, 1998.


National Cooperative Soil Survey
U.S.A.