LOCATION FESSLER            MT 
Established Series
Rev. BDD-JAL
09/2000

FESSLER SERIES


The Fessler series consists of very deep, well drained soils that formed in colluvium derived from calcareous argillite. These soils are on mountains. Slopes are 15 to 60 percent. Mean annual precipitation is about 20 inches, and mean annual temperature is about 40 degrees F.

TAXONOMIC CLASS: Loamy-skeletal, mixed, superactive, frigid Pachic Argiustolls

TYPICAL PEDON: Fessler gravelly loam, forested (colors are for dry soil unless otherwise noted).

Oi-0 to 3 inches; slightly decomposed forest litter. (1 to 3 inches thick)

A1--3 to 7 inches; black (10YR 2/1) gravelly loam, black (10YR 2/1) moist; moderate fine granular structure; soft, very friable, slightly sticky and slightly plastic; many very fine, fine, and medium roots; many very fine irregular pores; 5 percent cobbles and 15 percent pebbles; slightly acid (pH 6.2); clear smooth boundary. (4 to 6 inches thick)

A2--7 to 13 inches; very dark gray (10YR 3/1) very gravelly clay loam, black (10YR 2/1) moist; moderate medium subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; many very fine, fine and medium roots and common coarse roots; many very fine irregular pores; 15 percent cobbles and 30 percent pebbles; slightly acid (pH 6.4); clear smooth boundary. (5 to 8 inches thick)

Bt1--13 to 32 inches; reddish brown (5YR 4/3) very cobbly clay loam, dark reddish brown (5YR 3/3) moist; moderate medium subangular blocky structure; hard, firm, slightly sticky and moderately plastic; many very fine and fine and common medium and coarse roots; many very fine tubular pores; many distinct clay flims on faces of peds and in pores; 25 percent cobbles and 30 percent pebbles; slightly acid (pH 6.4); clear wavy boundary. (7 to 19 inches thick)

Bt2--32 to 40 inches; reddish brown (5YR 5/3) very cobbly clay loam, reddish brown (5YR 4/3) moist; moderate medium subangular blocky structure; slightly hard, firm, slightly sticky and slightly plastic; common very fine and fine roots and few coarse roots; many very fine tubular pores and common fine tubular pores; common distinct clay films on faces of peds; 25 percent cobbles and 30 percent pebbles; neutral (pH 7.0); clear wavy boundary. (8 to 14 inches thick)

Bk--40 to 60 inches; light reddish brown (5YR 6/3) very cobbly sandy clay loam, reddish brown (5YR 5/3) moist; weak medium subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; common very fine and fine roots; common very fine tubular pores; few faint clay films on faces of peds; 25 percent cobbles and 25 percent pebbles; lime disseminated; few fine filaments of lime; few faint coatings of lime on surface of coarse fragments; slightly effervescent; slightly alkaline (pH 7.8).

TYPE LOCATION: Granite County, Montana; 1,200 feet west and 100 feet north of the SE corner of sec. 20, T. 11 N., R. 14 W.

RANGE IN CHARACTERISTICS:

Soil temperature - 41 to 46 degrees F.
Moisture control section - between 8 and 12 inches.
Mollic epipedon thickness - 16 to 30 inches

A1 horizon - Hue: 7.5YR or 10YR
Value: 2 or 3 dry; 2 or 3 moist
Clay content: 10 to 15 percent
Rock fragments: 15 to 35 percent--0 to 10 percent cobbles; 15 to 25 percent pebbles
Reaction: pH 6.1 to 7.3

A2 horizon - Hue: 7.5YR or 10YR
Value: 3 or 4 dry; 2 or 3 moist
Texture: loam or clay loam
Clay content: 20 to 30 percent
Rock fragments: 35 to 60 percent--0 to 5 percent stones; 5 to 15 percent cobbles; 30 to 40 percent pebbles
Reaction: pH 6.1 to 7.3

Bt1 horizon - Hue: 5YR, 7.5YR, or 10YR
Value: 4 or 5 dry; 2 or 3 moist
Chroma: 2 or 3
Texture: clay loam or sandy clay loam
Clay content: 27 to 35 percent
Rock fragments: 35 to 70 percent--0 to 5 percent stones; 5 to 25 percent cobbles; 30 to 40 percent pebbles
Reaction: pH 6.1 to 7.3

Bt2 horizon - Hue: 5YR, 7.5YR, or 10YR
Value: 4, 5, or 6 dry; 4 or 6 moist
Chroma: 3, 4, or 6
Texture: clay loam or sandy clay loam
Clay content: 27 to 35 percent
Rock fragments: 35 to 70 percent--0 to 5 percent stones; 5 to 25 percent cobbles; 30 to 40 percent pebbles
Reaction: pH 6.6 to 7.3

Bk horizon - Hue: 5YR, 7.5YR, or 10YR
Value: 6 or 7 dry; 5 or 6 moist
Chroma: 3, 4, or 6
Texture: sandy clay loam or clay loam
Clay content: 20 to 30 percent clay
Rock fragments: 35 to 75 percent--0 to 5 percent stones; 10 to 25 percent cobbles; 25 to 45 percent pebbles
Calcium carbonate equivalent: 1 to 5 percent
Reaction: pH 6.6 to 7.8

COMPETING SERIES:

Adellern (NM) - has transitional Bt/BC and BC/Bt horizons.

Braziel (MT) - does not have a Bk horizon.

Pastorius (CO) - does not have a Bk horizon.

Pastorpeak (AZ) - has less than 27 percent clay in the argillic horizon; has fragmental material at 60 to 80 inches.

Zillion (UT) - has a calcic horizon.

GEOGRAPHIC SETTING:

Landform - mountains.
Elevation - 3,600 to 6,400 feet.
Slope - 15 to 60 percent.
Parent material - colluvium derived from calcareous argillite.
Climate - long, cold winters; moist springs; warm summers.
Mean annual precipitation - 18 to 25 inches.
Mean annual air temperature - 38 to 42 degrees F.
Frost-free period - 70 to 90 days.

DRAINAGE AND PERMEABILITY: Well drained; moderately slow permeability.

USE AND VEGETATION: Fessler soils are used mainly for timber production, watershed, and for wildlife habitat. Potential native vegetation is mainly Douglas-fir, and ponderosa pine with an understory of common snowberry, pinegrass, mallow ninebark, elk sedge, and oregongrape.

DISTRIBUTION AND EXTENT: Fessler soils are of small extent in western Montana.

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

SERIES ESTABLISHED: Granite County Area, Montana, 1994.

REMARKS: Soil interpretations records: MT1480. Diagnostic horizons and features recognized in this pedon are: a mollic epipedon from 3 to 32 inches (A1, A2, and Bt1 horizons); an argillic horizon from 13 to 40 inches (Bt1 and Bt2 horizons); a horizon of secondary calcium carbonate accumulation from 40 to 60 inches (Bk horizon); a particle-size control section from 13 to 33 inches (Bt1 and Bt2 horizons). Fessler soils have a frigid temperature regime and an ustic moisture regime.


National Cooperative Soil Survey
U.S.A.