LOCATION INEL               ID
Established Series
Rev. DJ/PB/CLM
8/97

INEL SERIES


The Inel series consists of shallow, well drained soils that formed in residuum and colluvium over limestone bedrock. They are on ridgetops and sideslopes of mountains and foothills. Slopes are 10 to 55 percent. Permeability is moderate. Average annual precipitation is about 7 inches and the average annual air temperature is about 43 degrees F.

TAXONOMIC CLASS: Loamy-skeletal, carbonatic, frigid Lithic Haplocalcids

TYPICAL PEDON: Inel stony silt loam - on a 20 percent west facing slope at an elevation of 5,850 feet in rangeland. The vegetation is shadscale and Indian ricegrass. When described on July 28, 1986, the soil was slightly moist throughout. (Color is for dry soil unless otherwise noted.)

A--0 to 3 inches; pale brown (10YR 6/3) stony silt loam, dark brown (10YR 3/3) moist; weak thin platy structure; slightly hard, very friable, nonsticky and slightly plastic; many very fine and fine roots; common very fine tubular pores; 20 percent gravel, 5 percent cobbles and 2 percent stones; strongly effervescent (25 percent calcium carbonate equivalent); moderately alkaline (pH 8.0); clear smooth boundary. (2 to 4 inches thick)

Bw--3 to 9 inches; pale brown (10YR 6/3) gravelly silt loam, brown (10YR 4/3) moist; weak fine subangular blocky structure; slightly hard, very friable, nonsticky and slightly plastic; many very fine, fine and few medium roots; common very fine tubular pores; 10 percent gravel, 5 percent cobbles and 3 percent stones; strongly effervescent (35 percent calcium carbonate equivalent); moderately alkaline (pH 8.0); clear smooth boundary. (4 to 8 inches thick)

Bkq1--9 to 13 inches; very pale brown (10YR 7/3) very gravelly loam, brown (10YR 5/3) moist; weak fine subangular blocky structure; slightly hard, very friable, nonsticky and slightly plastic; common very fine, fine and medium roots; common very fine tubular pores; 15 percent gravel, 15 percent cobbles and 5 percent stones; matrix violently effervescent (40 percent calcium carbonate equivalent); common lime and silica coats 1 to 2 mm thick on undersides of rock fragments; moderately alkaline (pH 8.3); gradual wavy boundary. (4 to 6 inches thick)

Bkq2--13 to 19 inches; very pale brown (10YR 7/3) very cobbly loam, brown (10YR 4/3) moist; weak fine subangular blocky structure; slightly hard, very friable, nonsticky and slightly plastic; common very fine, fine and medium roots; common very fine tubular pores; 15 percent gravel, 20 percent cobbles, and 5 percent stones; violently effervescent (40 percent calcium carbonate equivalent); common lime and silica coats 1 to 2 mm thick on undersides of rock fragments; moderately alkaline (pH 8.2); gradual wavy boundary. (4 to 6 inches thick)

R--19 inches; hard limestone.

TYPE LOCATION: Butte County, Idaho; about two miles southwest of tailing ponds on North Fork Creek; 750 feet east and 700 feet south of the northwest corner of section 14, T. 7 N., R. 26 E.; 43 degrees, 56 minutes, 32 seconds north latitude, 113 degrees, 5 minutes, 25 seconds west longitude.

RANGE IN CHARACTERISTICS:

Average summer soil temperature - 59 to 66 degrees F.
The soil moisture control section is dry for over three-fourths of the time when the soil temperature is above 41 degrees F.
Average annual soil temperature - 41 to 47 degrees F.
Depth to the calcic horizon - 7 to 10 inches
Depth to bedrock - 10 to 20 inches
Particle-size control section Total clay - 10 to 18 percent Total sand - 40 - 60 percent
Carbonate clay - 8 to 15 percent
Carbonate free clay - 2 to 10 percent
Rock fragments - 35 to 50 percent

A horizon Value - 3 through 5 moist Chroma - 2 or 3 dry
Calcium carbonate equivalent - 20 to 40 percent. It is slightly or moderately alkaline.

Bw horizon Value - 6 or 7 dry and 4 or 5 moist Chroma 3 or 4 dry Texture - GR-SIL or GRV-L Rock fragments - 15 to 40 percent Calcium carbonate equivalent - 30 to 40 percent. It is moderately or strongly alkaline.

Bkq horizon Value - 6 through 8 dry and 4 through 7 moist Chroma - 2 or 3 moist Texture - GRV-L, CBV-L, or GRV-SL Rock fragments - 35 to 50 percent
Calcium carbonate equivalent - 40 to 50 percent. It is moderately or strongly alkaline.

COMPETING SERIES: There are no competing series.

GEOGRAPHIC SETTING: Inel soils occur on limestone ridgetops and sideslopes of foothills and mountains. They formed in residuum and colluvium. Slopes are 10 to 55 percent. Elevations range from 4,500 to 6,500 feet. The precipitation ranges from 7 to 8 inches, most of which is in the form of snow. The average annual air temperature is 42 to 45 degrees F. The frost free season is 70 to 90 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Ike, Simeroi, Slide, and McCaleb (T) soils. Ike soils occur on north slopes and higher elevations. Simeroi, Slide, and McCaleb soils are very deep soils on fan terraces. Slide soils are also on foothills.

DRAINAGE AND PERMEABILITY: Well drained; rapid runoff; moderate permeability.

USE AND VEGETATION: Used primarily for rangeland and wildlife habitat. Vegetation is mainly shadscale and Indian ricegrass.

DISTRIBUTION AND EXTENT: Southcentral Idaho. These soils are not extensive.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Portland, Oregon

SERIES ESTABLISHED: Butte County Area, Idaho, 1997.

REMARKS: Diagnostic horizons and features recognized in this pedon are:

Ochric epipedon - the zone from 0 to 3 inches (A horizon)

Calcic horizon - the zone from 9 to 19 inches (Bkq1 and Bkq2 horizons)

Particle-size control section - the zone from 10 to 19 inches (part of the Bkq1 and the Bkq2 horizons)


National Cooperative Soil Survey
U.S.A.