LOCATION BEANLAKE           MT 
Established Series
Rev. DES-JAL
7/98

BEANLAKE SERIES


The Beanlake series consists of very deep, well drained soils that formed in till or alluvium. These soils are on moraines, till plains, alluvial fans, stream terraces and escarpments. Slopes are 0 to 45 percent. Mean annual precipitation is about 16 inches, and mean annual temperature is about 43 degrees F.

TAXONOMIC CLASS: Fine-loamy, mixed, superactive, frigid Typic Calciustolls

TYPICAL PEDON: Beanlake stony loam, in native grassland (colors are for dry soil unless otherwise noted).

A--0 to 6 inches; dark grayish brown (10YR 4/2) stony loam, very dark grayish brown (10YR 3/2) moist; moderate very fine granular structure; soft, very friable, slightly sticky and slightly plastic; many very fine roots; 10 percent pebbles, 3 percent stones; slightly alkaline (pH 7.8); clear smooth boundary. (5 to 8 inches thick)

Bk--6 to 16 inches; very pale brown (10YR 7/3) loam, brown (10YR 5/3) moist; weak medium prismatic structure parting to weak medium and fine subangular blocky; slightly hard, very friable, moderately sticky and slightly plastic; common very fine roots; many very fine tubular and interstitial pores; 5 percent pebbles, 5 percent cobbles; disseminated lime, common fine masses and seams of lime; continuous faint lime casts on undersides of fragments; violently effervescent; moderately alkaline (pH 8.4); gradual smooth boundary. (5 to 15 inches thick)

Bky1--16 to 38 inches; very pale brown (10YR 7/3) loam, brown (10YR 5/3) moist; weak medium and fine subangular blocky structure; slightly hard, friable, moderately sticky and slightly plastic; common very fine roots; many very fine tubular and interstitial pores; 5 percent cobble-sized soft sandstone fragments, 5 percent pebbles, 5 percent cobbles; disseminated lime, common fine masses and seams of lime; continuous faint lime coatings and casts on undersides of fragments; common fine seams of gypsum; violently effervescent; common fine seams of gypsum; moderately alkaline (pH 8.4); gradual smooth boundary. (15 to 22 inches thick)

Bky2--38 to 60 inches; light gray (2.5Y 7/2) cobbly loam, brown (10YR 5/3) moist; weak medium and fine subangular blocky structure; hard, friable, moderately sticky and slightly plastic; few very fine roots; common very fine tubular and interstitial pores; 15 percent pebbles, 20 percent cobbles; disseminated lime, few fine masses and seams of lime; continuous faint lime casts on undersides of fragments; common fine seams and masses of gypsum; violently effervescent; strongly alkaline (pH 8.6).

TYPE LOCATION: Lewis and Clark County, Montana; 2,500 feet north and 2,200 feet east of the SW corner of sec. 19, T. 20 N., R. 7 W.

RANGE IN CHARACTERISTICS:

Soil temperature - 42 to 47 degrees F.

Moisture control section - between 4 and 12 inches.

Mollic epipedon thickness - 7 to 8 inches.

The surface layer is calcareous when mixed to 7 inches.

A horizon - Hue: 10YR

Value: 4 or 5 dry, 2 or 3 moist

Chroma: 1, 2 or 3

Texture: loam or silt loam

Clay content: 15 to 25 percent

Rock fragments: 10 to 30 percent--0 to 15 percent cobbles and stones, 0 to 15 percent pebbles

Reaction: pH 7.4 to 8.4

Bk horizon - Hue: 10YR

Value: 5, 6, 7, or 8 dry; 3, 4, 5, or 6 moist

Chroma: 2 or 3

Texture: loam or clay loam

Clay content: 18 to 30 percent

Calcium carbonate equivalent: 15 to 25 percent

Rock fragments: 10 to 35 percent--0 to 20 percent cobbles and stones, 5 to 15 percent pebbles

Reaction: pH 7.9 to 8.4

Bky1 horizon - Hue: 10YR or 2.5Y

Value: 7 or 8 dry, 5 or 6 moist

Chroma: 2 or 3

Texture: loam or clay loam

Clay content: 18 to 30 percent

EC: 0 to 4 mmhos/cm

Calcium carbonate equivalent: 15 to 35 percent

Gypsum content: 1 to 3 percent

Rock fragments: 10 to 35 percent--0 to 20 percent cobbles and stones, 5 to 15 percent pebbles

Reaction: pH 7.9 to 9.0

Bky2 horizon - Hue: 10YR or 2.5Y

Value: 6 or 7 dry, 4 or 5 moist

Chroma: 2 or 3

Texture: loam or clay loam

Clay content: 18 to 30 percent

EC: 0 to 4 mmhos/cm

Gypsum content: 1 to 3 percent

Calcium carbonate equivalent: 8 to 15 percent

Rock fragments: 15 to 40 percent--0 to 5 percent stones, 10 to 20 percent cobbles, 5 to 15 percent pebbles

Reaction: pH 7.9 to 9.0

Bulk density of more than 1.6 grams per cubic centimeter.

COMPETING SERIES:

Ipano (MT) - lithic contact at a depth of 20 to 40 inches.

Kiev (MT) - moderate permeability and a bulk density of less than 1.6 grams per cubic centimeter, formed in alluvium.

Mudcree (UT) - paralithic contact at a depth of 20 to 40 inches.

Rabbitex (CO) - deeper than 8 inches to the calcic horizon, lithic contact at a depth of 40 to 60 inches.

Roundor (MT) - paralithic contact at a depth of 20 to 40 inches.

Zahl (ND) - has less than 10 percent coarse fragments in the particle-size control section; does not have horizon of gypsum accumulation.

GEOGRAPHIC SETTING:

Landforms - moraines, till plains, alluvial fans, stream terraces and escarpments.

Elevation - 3,800 to 6,000 feet.

Slope- 0 to 45 percent.

Parent material - till or alluvium.

Climate - long, cold winters; moist springs; warm summers.

Mean annual precipitation - 12 to 19 inches, most of which falls as snow in winter or as snow or rain early in spring and in summer.

Mean annual air temperature - 40 to 45 degrees F.

Frost-free period - 70 to 120 days.

DRAINAGE AND PERMEABILITY: Well drained; moderate permeability.

USE AND VEGETATION: Beanlake soils are used mainly for rangeland. Potential native vegetation is mainly rough fescue, bluebunch wheatgrass, Idaho fescue, Columbia needlegrass, prairie junegrass, forbs, and shrubs; some areas support thin stands of limber pine, Rocky Mountain juniper, and Douglas fir.

DISTRIBUTION AND EXTENT: Beanlake soils are inextensive in west-central Montana along the eastern front of the Rocky Mountains.

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

SERIES ESTABLISHED: Choteau-Conrad Area, parts of Teton and Pondera Counties, Montana, 1991.

REMARKS: Soil interpretations record: MT0267, MT1320, MT1395. Diagnostic horizons and features recognized in this pedon are: a mollic epipedon from the surface to 7 inches (mixed) (A horizon); calcic horizon from 6 to 38 inches (Bk and Bky1 horizons); horzons of gypsum accumulation from 16 to 60 inches (Bky1 and Bky2 horizons); particle-size control section from 10 to 40 inches (Bk, Bky1 and Bky2 horizons). Beanlake soils have a frigid temperature regime and an ustic moisture regime.


National Cooperative Soil Survey
U.S.A.