LOCATION LAKE JANEE         UT
Established Series
Rev. EJ/LW/MEO/AJE/JMW
03/1999

LAKE JANEE SERIES


The Lake Janee series consists of deep, well drained soils that formed in material weathered from intermediate igneous rocks. Lake Janee soils are on ground and lateral moraines, and have slopes of 15 to 40 percent. The average annual precipitation is about 30 inches and the mean annual air temperature is about 42 degrees F.

TAXONOMIC CLASS: Coarse-loamy, mixed, superactive Typic Dystrocryepts

TYPICAL PEDON: Lake Janee cobbly sandy loam, woodland . (Colors are for dry soil unless otherwise noted. )

Al--O to 2 inches; grayish brown (10YR 4/2) cobbly sandy loam, very dark brown (10YR 2/2) moist; weak fine granular structure; slightly hard, very friable, nonsticky and slightly plastic; many fine roots; 25 percent cobbles and stones; slightly acid (pH 6.1); abrupt wavy boundary. (O to 2 inches thick)

A12--2 to 14 inches; brown (10YR 5/3) cobbly fine sandy loam, dark brown (10YR 4/3) moist; weak medium subangular blocky structure; slightly hard, friable, slightly sticky and nonplastic; many fine and medium roots; 20 percent pebbles and cobbles; medium acid (pH 5.8); gradual wavy boundary. (10 to 12 inches thick)

B21--14 to 24 inches; pale brown (10YR 6/3) cobbly sandy loam, brown (10YR 4/3) moist; weak medium subangular blocky structure; slightly hard, very friable, slightly sticky and nonplastic; many fine and medium roots; common fine and medium pores; few thin clay films in pores; 30 percent cobbles and pebbles; medium acid (pH 5.9); gradual wavy boundary. (9 to 10 inches thick)

B22--24 to 36 inches; light yellowish brown (10YR 6/4) cobbly coarse sandy loam, yellowish brown (10YR 5/5) moist; weak medium subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; common fine and medium roots; many medium pores; few thin clay films in pores and on peds; 30 percent cobbles and pebbles; medium acid (pH 5.9); gradual wavy boundary. (9 to 12 inches thick)

B23--36 to 48 inches; light yellowish brown (10YR 6/4) cobbly sandy loam, yellowish brown (10YR 5/5) moist; other characteristics the same as B22; clear wavy boundary. (10 to 18 inches thick)

B24--48 to 66 inches; light yellowish brown (10YR 6/4) cobbly sandy loam, yellowish brown (10YR 5/5) moist; weak fine subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; few fine roots; common fine pores; few thin clay films in pores and on faces of peds; 35 percent cobbles, pebbles and stones; medium acid (pH 5.9); clear irregular boundary. (6 to 9 inches thick)

Cr--66 to 80 inches; about 70 percent weathered parent rock and 30 percent B2 material in pockets.

TYPE LOCATION: Wasatch County, Utah; about 15 miles northwest of Heber at a point 1 mile west of Park City and Cloud Rim Road Junction at the head of Pine Creek; 1,200 feet south and 4,360 feet west of the NE corner of section 31, T.2S., R.4E.

RANGE IN CHARACTERISTICS: Solum thickness is more than 40 inches. Cobbles and stones range from 20 to 35 percent throughout the profile. The mean annual soil temperature is about 40 degrees F. and the mean annual summer soil temperature is about 54 degrees F. Base saturation is less than 60 percent in some part above a depth of 30 inches. The soils are usually moist and are not dry for as much as 90 cumulative days in some subhorizon. A thin layer of needles and tuff occur in places mainly under the tree canopy.

The Al horizon has value of 4 or 5 dry, 2 through 4 moist, and chroma of 2 or 3. The moist value of 2 or 3 extends to depths of 2 inches or less.

The B2 horizon has value of 5 or 6 dry, 4 or 5 moist and chroma of 3 through 5. It is cobbly sandy loam or cobbly coarse sandy loam. Clay films are thin and patchy, occurring mostly in pores and are more evident deep in the profile.

COMPETING SERIES: These soils are the Cuberant, Leal, Marsell and Scout series. Cuberant and Scout soils have more than 35 percent rock fragments in the control section and have base saturation of more than 60 percent. Cuberant soils are 20 to 40 inches deep over bedrock. Leal soils have B2ir horizons, and A2 horizons. Marsell soils have more than 35 percent rock fragments in the control section.

GEOGRAPHIC SETTING: Lake Janee soils occur on moderately steep to very steep ground and lateral moraines derived from coarse grained intermediate igneous parent rocks. Slopes are 15 to 40 percent. Elevation ranges from 8,000 to 10,000 feet above sea level. The climate is humid, with an average annual precipitation of 25 to 35 inches that falls mostly as snow. The mean annual temperature is about 42 degrees F., mean summer temperature is about 54 degrees F. and the frost-free period is 50 to 80 days. Lake Janee Series

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Hailman and Buell soils. Hailman soils have thick mollic epipedons. Buell soils have thick dark colored umbric epipedons and have control sections containing more than 35 percent pebbles and cobbles.

DISTRIBUTION AND EXTENT: Well drained; medium runoff; moderate to moderately rapid permeability.

USE AND VEGETATION: These soils are used for watershed, wildlife habitat, limited timber production and limited summer grazing by livestock. Native plants are subalpine fir and Englemann spruce with scattered aspen. Understory is gooseberry, elderberry, elkweed and sedges.

DISTRIBUTION AND EXTENT: High mountain areas in north-central Utah. This series is inextensive.

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

SERIES ESTABLISHED: Wasatch Soil Survey Area, Wasatch County, Utah, 1967.

OSED scanned by NSSQA. Last revised by state on 12/76.


National Cooperative Soil Survey
U.S.A.