LOCATION MONAD              MT+CO
Established Series
Rev. HAL-GFB-JAL
07/2005

MONAD SERIES


The Monad series consists of very deep, well drained soils that formed in local alluvium, colluvium, and outwash mainly from argillites, sandstone, and quartzites. These soils are on alluvial fans, hills, ground moraines and mountains. Slopes are 2 to 60 percent. Mean annual precipitation is about 21 inches, and mean annual temperature is about 42 degrees F.

TAXONOMIC CLASS: Fine-loamy, mixed, superactive Alfic Argicryolls

TYPICAL PEDON: Monad loam, grassland (colors are for dry soil unless otherwise noted).

A1--0 to 9 inches; very dark gray (10YR 3/1) loam, black (10YR 2/1) moist; moderate fine granular structure; soft, very friable, slightly sticky and slightly plastic; many fine and very fine roots, few medium roots; 15 percent cobbles and gravel; slightly acid (pH 6.2); clear wavy boundary. (6 to 11 inches thick)

A2--9 to 14 inches; grayish brown (10YR 5/2) loam, very dark grayish brown (10YR 3/2) moist; moderate fine and very fine subangular blocky structure; hard, friable, moderately sticky and moderately plastic; many fine and very fine roots, few medium roots; many fine and very fine pores, few medium pores; very thin continuous gray (10YR 6/1) skeletans coating faces of peds; 15 percent channers; moderately acid (pH 5.8); gradual wavy boundary. (0 to 8 inches thick)

Bt/E--14 to 21 inches; Bt part (80 percent) brown (10YR 5/3) loam, brown (10YR 4/3) moist; E part (20 percent) gray (10YR 6/1) loam, dark gray (10YR 4/1) moist; weak medium prismatic structure parting to moderate fine subangular blocky structure; very hard, friable, moderately sticky and moderately plastic; common fine and very fine roots; many fine and very fine pores, few medium pores; very thin continuous gray (10YR 6/1) skeletans coating continuous faint clay films on faces of peds; 10 percent sandstone channers; moderately acid (pH 5.7); clear wavy boundary. (5 to 17 inches thick)

Bt1--21 to 49 inches; pale brown (10YR 6/3) clay loam, brown (10YR 4/3) moist; weak medium prismatic structure parting to moderate fine and medium blocky structure; extremely hard, firm, very sticky and moderately plastic; few fine and very fine roots; many fine and very fine pores, few medium pores; very thin gray (10YR 6/1) skeletans coating continuous distinct clay films on faces of peds; 10 percent sandstone channers; moderately acid (pH 5.8); gradual wavy boundary. (9 to 24 inches thick)

Bt2--49 to 74 inches; very pale brown (10YR 7/4) stony clay loam, brown (7.5YR 5/4) moist; strong medium and fine blocky structure; extremely hard, firm, very sticky and moderately plastic; many fine and very fine pores, few medium pores; continuous distinct clay films on faces of peds; 15 percent cobbles, 10 percent stones; slightly alkaline (pH 7.4).

TYPE LOCATION: Cascade County, Montana; 700 feet east and 1,340 feet south of the NW corner of the NE 1/4 of sec. 27, T. 17 N., R. 5 E.

RANGE IN CHARACTERISTICS:

Soil temperature - 35 to 41 degrees F.
Moisture control section - between 4 and 12 inches.
Mollic epipedon thickness - 10 to 16 inches.
Some pedons have an E/Bt horizon.

A horizons - Value: 3, 4 or 5 dry; 2 or 3 moist
Chroma: 1 or 2
Texture: loam or fine sandy loam
Clay content: 10 to 27 percent
Rock fragments: 0 to 35 percent--0 to 10 percent cobbles, 0 to 25 percent gravel
Reaction: pH 5.6 to 7.3

Bt/E horizon - Value: Bt part 4, 5, or 6 dry, 4 or 5 moist; E part 6 or 7 dry, 4 or 5 moist
Chroma: Bt part 2, 3 or 4, E part 1, 2 or 3
Texture: loam, clay loam, or sandy clay loam
Clay content: 22 to 35 percent
Rock fragments: 10 to 35 percent--0 to 5 percent cobbles and stones, 10 to 30 percent gravel or channers
Reaction: pH 5.6 to 7.3

Bt horizons - Hue: 10YR or 7.5YR
Value: 5, 6, or 7 dry; 4 or 5 moist
Chroma: 3, 4 or 6
Texture: clay loam, loam, or sandy clay loam
Clay content: 22 to 35 percent
Rock fragments: 10 to 35 percent0 to 15 percent stones, 0 to 15 percent cobbles, 0 to 25 percent gravel or channers
Reaction: pH 5.6 to 7.8

COMPETING SERIES:

Anvik (CO) - has 25 to 35 percent stones and cobbles at depths of 40 to 60 inches; rock fragments in the argillic horizon are stones and cobbles.

Bear Basin (UT) - has strongly or very strongly acid argillic and C horizons; very cobbly sandy loam below the argillic horizon.

Buffork (WY) has a paralithic contact at a depth of 20 to 40 inches.

Slipman (WY) - has a lithic contact of sandstone at depths of 40 to 60 inches.

GEOGRAPHIC SETTING:

Landform - alluvial fans; hills; ground moraines; mountains.
Elevation - 4,600 to 8,100 feet.
Slope - 2 to 60 percent.
Parent material - local alluvium, colluvium, and outwash mainly from argillites, sandstone, and quartzites.
Mean annual precipitation - 14 to 24 inches.
Mean annual temperature - 34 to 39 degrees F.
Frost-free period - 30 to 70 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Libeg, Loggert, and Tigeron soils. These soils contain more than 35 percent rock fragments in the particle-size control section. Loggert and Tigeron soils lack a mollic epipedon.

DRAINAGE AND PERMEABILITY: Well drained; moderately slow permeability.

USE AND VEGETATION: Monad soils are used mainly for rangeland. Potential native vegetation is mainly rough fescue, Idaho fescue, Richardson needlegrass, mountain brome, forbs, and shrubs.

DISTRIBUTION AND EXTENT: Monad soils are of moderate extent in west-central Montana and Colorado.

MLRA OFFICE RESPONSIBLE: Bozeman, Montana

SERIES ESTABLISHED: Cascade County, Montana, 1975.

REMARKS: Soil interpretations record: MT0115. Diagnostic horizons and features recognized in this pedon are: a mollic epipedon from the soil surface to 14 inches (A1, A2 horizons); a glossic horizon from 14 to 21 inches (Bt/E horizon); an argillic horizon from 14 to 74 inches (Bt/E, Bt1, Bt2 horizons); a particle-size control section from 14 to 34 inches (Bt/E, Bt1 horizons). Monad soils have a cryic temperature regime and an ustic moisture regime.


National Cooperative Soil Survey
U.S.A.