LOCATION STIPE              ID
Established Series
Rev. RG/MD/CLM
10/2002

STIPE SERIES


The Stipe series consists of moderately deep, well drained soils on basalt plains. These soils have formed in eolian deposits from mixed sources. Permeability is moderate. Slopes range from 1 to 8 percent. Average annual precipitation is about 15 inches and the average annual temperature is about 38 degrees F.

TAXONOMIC CLASS: Coarse-loamy, mixed, superactive, frigid Calcic Pachic Haploxerolls

TYPICAL PEDON: Stipe fine sandy loam - on a 1 percent slope. When described on May 21, 1980, the profile was moist throughout. (Colors are for dry soil unless otherwise noted.)

A--0 to 12 inches; brown (10YR 4/3) fine sandy loam, very dark grayish brown (10YR 3/2) moist; massive; slightly hard, very friable; common fine and very fine roots; common fine and very fine tubular pores; 5 percent pebbles; mildly alkaline (pH 7.7); gradual wavy boundary. (5 to 15 inches thick)

Bw1--12 to 18 inches; brown (10YR 4/3) very fine sandy loam, very dark grayish brown (10YR 3/2) moist; weak medium subangular blocky structure; slightly hard, very friable, slightly plastic; few very fine roots; few very fine tubular pores; 5 percent pebbles; mildly alkaline (pH 7.7); gradual wavy boundary. (6 to 19 inches thick)

Bw2--18 to 34 inches; brown (10YR 5/3) very fine sandy loam, dark brown (10YR 3/3) moist; weak medium and coarse subangular blocky structure; slightly hard, very friable, slightly sticky; few fine roots; few fine tubular pores; 5 percent pebbles, 5 percent cobbles, and 4 percent stones; moderately alkaline (pH 7.9); abrupt wavy boundary. (7 to 19 inches thick)

Bk--34 to 36 inches; light gray (10YR 7/2) very fine sandy loam, grayish brown (10YR 5/2) moist; moderate medium and coarse subangular blocky structure; soft, friable, slightly plastic; violently effervescent; many soft accumulations of calcium carbonate; moderately alkaline (pH 8.0); abrupt irregular boundary. (2 to 8 inches thick)

2R--36 inches; unweathered, vesicular basalt.

TYPE LOCATION: Fremont County, Idaho; 8 miles north of Parker; 530 feet east and 260 feet south of the northwest corner of sec. 33, T.9N., R.40.

RANGE IN CHARACTERISTICS:

Depth to bedrock - 20 to 40 inches
Thickness of mollic epipedon - 25 to 34 inches
Average annual soil temperature - 39 to 44 degrees F.
Rock fragments - 0 to 10 percent

A horizon
Color value, dry - 4 or 5
Value, moist - 2 or 3
Chroma - 2 or 3 dry or moist

Bw horizon
Color value, dry - 4 or 5
Value, moist - 2 or 3
Chroma - 2 through 4 dry or moist
Texture - fine sandy loam or very fine sandy loam
Clay content - 11 to 18 percent
Reaction - mildly alkaline or moderately alkaline

Bk horizon
Color value, dry - 6 or 7
Value, moist - 2 or 3
Chroma - 2 through 4 dry or moist
Texture - fine sandy loam or very fine sandy loam
Clay content - 13 to 19 percent
Calcium carbonate equivalent - 1 to 5 percent
Reaction - mildly alkaline or moderately alkaline

COMPETING SERIES: This is the Jipper series. Jipper soils are deep or very deep.

GEOGRAPHIC SETTING: Stipe soils are on basalt plains. They formed in wind blown material from mixed sources. Slopes range from 1 to 8 percent. Elevation ranges from 5,000 to 5,800 feet. Average annual temperature is 37 to 42 degrees F and the average precipitation is 13 to 16 inches, including 3 to 6 feet of snowfall. Average summer temperature ranges from 61 to 63 degrees F. The frost-free season ranges from 80 to 100 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Blacknoll(T), Jipper(T), Katseanes(T), Nayrib(T), Pinebutte(T), Snowshoe(T), Vadnais(T), and Wolverine soils. Blacknoll soils lack a mollic epipedon. Jipper soils are deep to basalt. Katseanes soils are shallow and have an argillic horizon. Nayrib soils are very shallow and are on pressure ridges of the basalt plain. Pinebutte soils have an argillic horizon. Vadnais soils have an argillic horizon. Snowshoe soils are coarse textured windblown deposits over finer textured material and are more than 60 inches deep. Wolverine soils are on stabilized dunes and lack a cambic horizon. The Katseanes and Pinebutte soils are in areas of higher elevation with more precipitation. Snowshoe and Wolverine soils are on stabilized sandunes.

DRAINAGE AND PERMEABILITY: Well drained; moderate permeability.

USE AND VEGETATION: Rangeland, cropland, and wildlife habitat. Principal native vegetation is mountain big sagebrush, antelope bitterbrush, and bunchgrasses.

DISTRIBUTION AND EXTENT: Stipe soils are inextensive in eastern Idaho.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Portland, Oregon

SERIES ESTABLISHED: Fremont County, Idaho, 1989.

REMARKS: Diagnostic horizons and features recognized in this soil are:

Mollic epipedon - 0 to 34 inches (A, Bw1, and Bw2 horizons).

Calcic feature - 34 to 36 inches (Bk horizon).

Particle-size control section - 10 to 36 inches (part of the A, Bw1, Bw2, and Bk).


National Cooperative Soil Survey
U.S.A.