LOCATION REDFERN            MT 
Established Series
Rev. DES-BDD-JAL
05/1999

REDFERN SERIES


The Redfern series consists of shallow, well drained soils that formed in colluvium or residuum derived from hard fine grained sandstone or fine grained igneous rock. These soils are on escarpments, ridges, divides and sideslopes of hills and mountains. Slopes are 15 to 70 percent. Mean annual precipitation is about 17 inches, and mean annual air temperature is about 38 degrees F.

TAXONOMIC CLASS: Loamy-skeletal, mixed, superactive Lithic Haplocryalfs

TYPICAL PEDON: Redfern very cobbly loam, bouldery, forested (colors are for dry soil unless otherwise noted).

Oi--1/2 to 0 inches; partially decomposed needles, twigs, and leaves. (0 to 3 inches thick)

A--0 to 3 inches; light brownish gray (2.5Y 6/2) very cobbly loam, dark grayish brown (2.5Y 4/2) moist; weak fine and medium subangular blocky structure; soft, very friable, slightly sticky and slightly plastic; many very fine and fine and few medium roots; many very fine and fine interstitial and tubular pores; 20 percent cobbles, 30 percent pebbles; neutral (pH 6.9); clear smooth boundary. (0 to 5 inches thick)

E--3 to 7 inches; light gray (10YR 7/2) extremely gravelly loam, brown (10YR 5/3) moist; weak fine and medium subangular blocky structure; slightly hard, very friable, slightly sticky and slightly plastic; many very fine and fine and few medium roots; many very fine and fine interstitial and tubular pores; 20 percent cobbles, 40 percent pebbles; neutral (pH 6.8); clear smooth boundary. (3 to 8 inches thick)

Bt--7 to 18 inches; yellowish brown (10YR 5/4) extremely gravelly clay loam, dark yellowish brown (10YR 4/4) moist; moderate medium subangular blocky structure; slightly hard, friable, moderately sticky and slightly plastic; common very fine and fine and few medium roots; common very fine and fine interstitial and tubular pores; many distinct dark grayish brown (10YR 4/2) clay films on faces of peds and bridging sand grains; 20 percent cobbles, 45 percent pebbles; moderately acid (pH 5.8). (6 to 13 inches thick)

R--18 inches; very dark gray (5Y 3/1), hard fine grained igneous bedrock.

TYPE LOCATION: Jefferson County, Montana; 1,200 feet south and 1,800 feet east of the NW corner of sec. 8, T. 5 N., R. 3 W.

RANGE IN CHARACTERISTICS:

Soil temperature - 38 to 42 degrees F.
Moisture control section - between 4 and 12 inches or from 4 inches to the lithic contact if bedrock is less than 12 inches.
Depth to argillic horizon - 3 to 13 inches.
Depth to bedrock - 10 to 20 inches.
Surface stones or boulders - 0 to 20 percent.
A transitional weak Bt or BC horizon is allowed.

A horizon - Hue: 10YR or 2.5Y
Value: 4, 5 or 6 dry; 2, 3, 4 or 5 moist
Chroma: 2 or 3
Clay content: 15 to 27 percent
Rock fragments: 20 to 60 percent--0 to 20 percent stones and cobbles, 20 to 40 percent pebbles
Reaction: pH 5.6 to 7.3

E horizon - Hue: 10YR or 2.5Y
Value: 6 or 7 dry; 4, 5 or 6 moist
Chroma: 2, 3 or 4
Texture: loam or sandy loam
Clay content: 15 to 25 percent
Rock fragments: 35 to 65 percent--0 to 5 percent stones, 10 to 25 percent cobbles, and 20 to 40 percent pebbles
Reaction: pH 5.6 to 7.3

Bt horizon - Hue: 7.5YR, 10YR, or 2.5Y
Value: 5, 6 or 7 dry; 4 or 5 moist
Chroma: 2, 3, or 4
Texture: loam, clay loam, or sandy clay loam
Clay content: 23 to 35 percent
Rock fragments: 35 to 70 percent--0 to 15 percent stones, 15 to 30 percent cobbles, and 20 to 45 percent pebbles
Reaction: pH 5.6 to 7.3

COMPETING SERIES:

Hapjack (WY) - does not have an E horizon; has 15 to 24 percent clay in the particle-size control section.

Herakle (CO) - has a calcic horizon; has a Btk horizon; has limestone rock fragments; bedrock is limestone.

Snowdon (CO) - has a udic moisture regime.

Whiteman (UT) - does not have an E horizon; formed in residuum from limestone.

GEOGRAPHIC SETTING:

Landform - escarpments, ridges, divides and sideslopes of mountains.
Elevation - 5,400 to 7,800 feet.
Slope - 15 to 70 percent.
Parent material - colluvium or residuum derived from hard fine grained sandstone or fine grained igneous rock
Climate - long, cold winters; cool, moist springs; short, cool summers.
Mean annual precipitation - 15 to 24 inches.
Mean annual air temperature - 36 to 40 degrees F.
Frost-free period - 30 to 70 days.

DRAINAGE AND PERMEABILITY: Well drained; moderate permeability.

USE AND VEGETATION: Redfern soils are primarily used for timber production, wildlife habitat, and watershed. The potential native vegetation is mainly Douglas fir, lodgepole pine, and subalpine fir with a sparse understory of common juniper, Oregongrape, heartleaf arnica, Kinnikinnick, russet buffaloberry, and grouse whortleberry.

DISTRIBUTION AND EXTENT: Redfern soils are of moderate extent in southwestern Montana.

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

SERIES ESTABLISHED: Jefferson County, Montana, 1998.

REMARKS: Soil interpretation record: MT3083, MT3084. Diagnostic horizons and features recognized in this pedon are: a layer of partially decomposed needles, twigs, and leaves from 1/2 inches to the mineral soil surface (Oi horizon); an ochric epipedon from the mineral surface to 7 inches (A, E horizons); an argillic horizon from 7 to 18 inches (Bt horizon); a particle- size control section from 7 to 18 inches (Bt horizon); hard fine grained igneous bedrock at 18 inches (R horizon). Redfern soils have a cryic temperature regime and an ustic moisture regime.


National Cooperative Soil Survey
U.S.A.