LOCATION HERM               CO+UT
Established Series
Rev. JPP/DKR/TWH
03/2005

HERM SERIES


The Herm series consists of very deep, well drained soils that formed in slope alluvium derived principally from interbedded sandstone and shale and in some pedons have eolian influence in the upper layers. Herm soils are on mountain slopes, hillslopes, structural benches, ridges, mesas, and cuestas. Slopes range from 0 to 50 percent. The mean annual precipitation is about 20 inches and the mean annual temperature is about 40 degrees F.

TAXONOMIC CLASS: Fine, smectitic, frigid Typic Argiustolls

TYPICAL PEDON: Herm loam, on a west facing, simple, 5 percent slope in rangeland at an elevation of 8,100 feet. (Colors are for dry soil unless otherwise noted.) Described on October 1,1986.

A--0 to 6 inches; dark grayish brown (10YR 4/2) loam, black (10YR 2/1) moist; moderate medium granular structure; soft, friable, slightly sticky and slightly plastic; common fine and few medium roots; few very fine pores; neutral (pH 6.8); clear smooth boundary. (3 to 10 inches thick)

AB--6 to 13 inches; dark brown (10YR 3/3) clay loam, very dark gray (10YR 3/1) moist; moderate medium subangular blocky structure parting to moderate medium granular; hard, firm, sticky and plastic; common fine and few medium roots; few very fine pores; neutral (pH 6.6); clear smooth boundary. (0 to 8 inches thick)

Bt1--13 to 17 inches; grayish brown (10YR 5/2) clay loam, dark grayish brown (10YR 4/2) moist; strong medium angular and subangular blocky structure; hard, firm, very sticky and very plastic; few distinct clay films on faces of peds; few fine and few medium roots; few very fine pores; neutral (pH 6.6); gradual wavy boundary.

Bt2--17 to 45 inches; brown (10YR 5/3) clay loam, brown (10YR 4/3) moist; strong medium angular and subangular blocky structure; very hard, very firm, very sticky and very plastic; many prominent clay films on faces of peds; common very fine and few fine roots; neutral (pH 6.6); gradual wavy boundary. (combined thickness of the Bt horizons is 20 to 50 inches)

BC--45 to 60 inches; grayish brown (10YR 5/2) clay loam, brown (10YR 4/3) moist; weak medium subangular blocky structure; hard, firm, sticky and plastic; 5 percent gravel, 9 percent cobble; neutral (pH 7.0).

TYPE LOCATION: Montezuma County, Colorado; about 6 miles northeast of Mancos, Colorado, along Forest Service road 566, about 300 feet north of the road; located about 1,100 feet south and 1,700 feet east of the northwest corner of Sec. 7, T. 36 N., R. 12 W.; Rampart Hills USGS quad.; Lat. 37 degrees, 23 minutes, 51 seconds N., and Long. 108 degrees, 13 minutes, 19 seconds W., NAD 27

RANGE IN CHARACTERISTICS:
Soil moisture regime: Ustic
Mean annual soil temperature: 41 to 46 degrees F.
Mean annual summer soil temperature: 50 to 55 degrees F. with an O horizon, and 59 to 63 degrees F. without an O horizon.
Thickness of the mollic epipedon: 10 to 16 inches
Depth to calcium carbonate: if present, 36 to 60 inches

Particle-size control section: 35 to 55 percent clay, 15 to 50 percent silt, 10 to 45 percent sand, and 0 to 30 percent rock fragments, but typically less than 5 percent. They consist of pebbles, cobble and stones mostly derived from sandstone, but have diorite fragments in some pedons.

A horizon:
Hue: 5YR to 10YR
Value: 3 to 5 dry, 2 or 3 moist
Chroma: 1 to 3, dry or moist
Texture: Loam, Clay loam
Rock fragments: 0 to 30 percent, mostly stone and cobble of sandstone and diorite composition
Reaction: slightly acid to slightly alkaline

BA or AB horizon (where present)
Value: 3 to 5 dry, 2 or 3 moist
Chroma: 2 or 3 dry or moist
Texture: silty clay loam, silt loam, or loam

Bt1 horizon:
Hue: 5YR to 10YR
Value: 4 to 6 dry, 2 to 4 moist
Chroma: 2 to 4, dry or moist
Texture: Clay loam, Clay, Silty clay loam
Reaction: slightly acid to slightly alkaline

Bt2 horizon:
Hue: 10YR or 2.5Y
Value: 5 to 7 dry, 4 to 6 moist
Chroma: 3 to 6
Texture: Clay loam, Clay, Silty clay loam
Reaction: slightly acid or neutral

BC horizon: (a Bk or C horizon in some pedons)
Hue: 10YR or 2.5Y
Value: 5 to 7 dry, 4 to 7 moist
Chroma: 2 to 6, dry or moist
Texture: Clay loam, Clay, Silty clay loam
Rock fragments: 0 to 30 percent, sandstone and shale gravel and cobble
Calcium carbonate equivalent: 0 to 5 percent
Reaction: neutral to moderately alkaline

COMPETING SERIES: These are the Absarokee, Acree, Barela, Capillo, Delson, Ekah, Morapos, Moreno, Nortez, Pramiss, Ricot, Tamaneen, Tukuhnik, Work and Zau series.

Absarokee, Acree, Ekah, Morapos, Ricot, Tamaneen, and Work: have horizons of calcium carbonate accumulation above a depth of 40 inches.
Absarokee, Nortez, and Zau soils have lithic contact at depths of 20 to 40 inches.

Barela, and Capillo: have lithic or paralithic contact at depths of 40 to 60 inches.

Delson, Moreno: have hue of 7.5YR and redder in the lower part of the Bt horizon.

Pramiss: have a paralithic contact between 20 to 40 inches.

Tukuhnik: have a lithic contact at 40 to 60 inches.

GEOGRAPHIC SETTING:
Parent material: slope alluvium derived from shale and sandstone; some pedons are influenced by eolian materials in the upper horizons.
Landform: mountain slopes, hillslopes, structural benches, ridges, mesas, cuestas.
Slopes: 0 to 50 percent
Elevation: 6,800 to 9,500 feet
Mean annual air temperature: 38 to 45 degrees F.
Mean annual precipitation: 14 to 25 inches.
Wettest months: July and August receive slightly more precipitation than other months.
Driest months: May and June receive the least precipitation, however the soils are still moist from snowmelt.
Frost-free period: 75 to 115 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Archuleta, Hesperus, Sanchez, and Valto series.

Archuleta, Sanchez, and Valto soils are shallow over a lithic or paralithic contact. All are on hillslopes and mountain slopes.

Hesperus soils have mollic epipedons more than 16 inches thick and have fine-loamy particle size control sections. They are on mountain slopes and in drainageways.

DRAINAGE AND PERMEABILITY: Well drained; medium runoff; slow permeability.

USE AND VEGETATION: These soils are used for timber production, livestock grazing, and wildlife habitat. Native vegetation consists of, Gambel's oak, snowberry, Arizona fescue, mountain muhly, mountain brome, bluegrass, junegrass, and forbs; with or without an overstory of ponderosa pine.

DISTRIBUTION AND EXTENT: Southwestern Colorado and southeastern Utah. LRR E, MLRA 36, 48A. This series is of moderate extent.

MLRA OFFICE RESPONSIBLE: Lakewood, Colorado

SERIES ESTABLISHED: Paonia Area, Colorado, 1976.

REMARKS: Diagnostic horizons and features recognized in this pedon are:
Mollic epipedon: The zone from 0 to 13 inches. (A and AB horizons)
Argillic horizon: The zone from 13 to 45 inches. (Bt1 and Bt2 horizons)
Particle-size control section: The upper 20 inches of the argillic horizon, from 13 to 33 inches (Bt1 and part of the Bt2 horizon)

Keys to Soil Taxonomy: Eighth Edition, 1998

The 2/99 revision moved the type location from the La Plata survey area to the Animas-Dolores survey area.


National Cooperative Soil Survey
U.S.A.