LOCATION GILISPIE           MT+ID OR WY
Established Series
Rev. WDB-JAL
10/1999

GILISPIE SERIES


The Gilispie series consists of shallow, well drained soils formed in colluvium or residuum derived from andesite, ryolite or basalt. These soils are on hills and mountains. Slopes are 0 to 60 percent. Mean annual precipitation is about 17 inches, and mean annual temperature is about 43 degrees F.

TAXONOMIC CLASS: Loamy, mixed, superactive Lithic Argicryolls

TYPICAL PEDON: Gilispie gravelly loam, in rangeland (colors are for dry soil unless otherwise noted).

A1--0 to 3 inches; grayish brown (10YR 5/2) gravelly loam, very dark grayish brown (10YR 3/2) moist; weak medium platy structure parting to moderate fine granular; soft, very friable, slightly sticky and slightly plastic; many very fine roots and tubular pores; few skeletons on pebbles; 25 percent pebbles; neutral (pH 7.0); clear smooth boundary.

A2--3 to 6 inches; grayish brown (10YR 5/2) gravelly loam, very dark grayish brown (10YR 3/2) moist; moderate medium subangular blocky structure parting to strong fine granular; slightly hard, very friable, slightly sticky and slightly plastic; many very fine roots, many fine tubular pores; common skeletons on faces of peds; 20 percent pebbles; neutral (pH 7.2); clear smooth boundary. (combined A horizon is 5 to 8 inches thick)

Bt--6 to 14 inches; pale brown (10YR 6/3) gravelly clay loam, dark yellowish brown (10YR 4/4) moist; moderate medium angular blocky structure; hard, friable, moderately sticky and moderately plastic; common very fine roots and tubular pores; common faint clay films on faces of peds; 25 percent pebbles; slightly alkaline (pH 7.6); gradual smooth boundary. (6 to 12 inches thick)

BC--14 to 18 inches; pale brown (10YR 6/3) extremely cobbly clay loam, brown (10YR 4/3) moist; moderate fine subangular blocky structure; hard, friable, moderately sticky and moderately plastic; few very fine roots, few fine pores; 75 percent cobbles; neutral (pH 7.2); clear smooth boundary. (0 to 8 inches thick)

R--18 inches; hard andesite.

TYPE LOCATION: Granite County, Montana; 1,650 feet west and 150 feet north of SE corner of sec. 5, T. 9 N., R. 13 W.

RANGE IN CHARACTERISTICS:

Soil temperature - 44 to 47 degrees F.
Mollic epipedon thickness - 7 to 10 inches.
Depth to bedrock - 10 to 20 inches.

A1 horizon - Hue: 7.5YR, 10YR, or 2.5Y
Value: 4 or 5 dry; 2 or 3 moist
Chroma: 1 or 2
Clay content: 15 to 27 percent
Rock fragments: 15 to 35 percent--15 to 35 percent pebbles, 20 to 35 percent cobbles or stones
Reaction: pH 6.6 to 7.8

A2 horizon - Hue: 7.5YR, 10YR, or 2.5Y
Value: 4 or 5 dry; 2 or 3 moist
Chroma: 1 or 2
Clay content: 20 to 25 percent
Rock fragments: 15 to 35 percent--15 to 35 percent pebbles, 20 to 35 percent cobbles or stones
Reaction: pH 6.6 to 7.8

Bt horizon - Hue: 7.5YR, 10YR, or 2.5Y
Value: 5 or 6 dry; 4 or 5 moist
Chroma: 2, 3, or 4
Texture: loam or clay loam
Clay content: 25 to 35 percent
Rock fragments: 15 to 35 percent--0 to 10 percent cobbles; 15 to 35 percent pebbles
Reaction: pH 6.6 to 7.8

BC horizon - Hue: 7.5YR, 10YR, or 2.5Y
Value: 5 or 6 dry; 4 or 5 moist
Chroma: 2, 3, or 4
Texture: loam or clay loam
Clay content: 20 to 30 percent
Rock fragments: 60 to 80 percent--65 to 75 percent cobbles; 0 to 10 percent pebbles
Reaction: pH 6.6 to 7.3

COMPETING SERIES:

Carbol (CO) - has more than 35 percent fine or coarser sand in the Bt horizon.

Chittum (WY) - has hue of 5YR or redder in the Bt horizon.

Katseanes (ID) - has less than 15 percent coarse fragments in the particle-size control section.

Mahogee (NV) - has a xeric moisture regime.

GEOGRAPHIC SETTING:

Landform - hills and mountains.
Elevation - 4,000 to 6,500 feet.
Slope - 0 to 60 percent.
Parent material - colluvium or residuum derived from andesite, ryolite, or basalt.
Climate - long, cold winters; moist springs; and cool summers.
Mean annual precipitation - 15 to 22 inches.
Mean annual temperature - 40 to 45 degrees F.
Frost-free period - 30 to 70 days.

DRAINAGE AND PERMEABILITY: Well drained; moderately slow permeability.

USE AND VEGETATION: Gilispie soils are used mainly as rangeland. Potential native vegetation is mainly bluebunch wheatgrass, Sandberg bluegrass, big sagebrush, and prairie junegrass.

DISTRIBUTION AND EXTENT: Gilispie soils are of small extent in western Montana, eastern Idaho, Wyoming and Oregon.

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

SERIES ESTABLISHED: Granite County, Montana, 1972.

REMARKS: Soil Interpretation Records: MT0571 and MT0660.
Diagnostic horizons and features recognized in this pedon are: a mollic epipedon when mixed to 7 inches (A1 and A2 horizons); an argillic horizon which is the particle-size control section from 6 to 14 inches (Bt horizon); and a lithic contact at 18 inches (R horizon). Gilispie soils have a cryic temperature regime and an ustic moisture regime.


National Cooperative Soil Survey
U.S.A.