LOCATION FELTONIA           ID
Established Series
Rev. TWP/CBR/FCF
08/2008

FELTONIA SERIES


The Feltonia series consists of very deep, well drained soils that formed in mixed alluvium with loess influence. Feltonia soils formed in fan remnants and stream terraces. Slopes are 0 to 4 percent. The mean annual precipitation is about 406[cr1] mm and the mean annual air temperature is about 5.0 degrees C.

TAXONOMIC CLASS: Coarse-loamy, mixed, superactive, frigid Calcic Pachic Haploxerolls

TYPICAL PEDON: Feltonia loam on a fan remnant with 1 percent slope at an elevation of 1838 meters. (Colors are for dry soil unless otherwise noted.)

Ap--0 to 15 cm; grayish brown (2.5Y 5/2) loam, very dark grayish brown (10YR 3/2) moist; weak very fine granular structure; slightly hard, very friable, slightly sticky and slightly plastic; common very fine and few fine roots; common very fine pores; slightly alkaline (pH 7.7); abrupt smooth boundary.

A--15 to 30 cm; grayish brown (10YR 5/2) loam, very dark grayish brown (10YR 3/2) moist; weak very coarse prismatic structure parting to weak very fine granular; slightly hard, very friable, slightly sticky and slightly plastic; common very fine roots; common very fine tubular pores; few krotovinas filled with slightly effervescent material; slightly alkaline (pH 7.8); clear smooth boundary. (Combined thickness of the A horizons is 20 to 58 cm)

Bt1--30 to 51 cm; dark grayish brown (10YR 4/2) loam, very dark grayish brown (10YR 3/2) moist; weak coarse prismatic structure parting to weak coarse subangular blocky then to weak very fine granular; slightly hard, very friable, slightly sticky and slightly plastic; common very fine roots; few fine and many very fine tubular pores; few thin clay films on vertical faces of peds and on surfaces along pores; very few skeletans; slightly alkaline (pH 7.7); clear smooth boundary.

Bt2--51 to 69 cm; brown (10YR 5/3) loam, dark brown (10YR 3/3) moist; weak coarse prismatic structure parting to weak medium subangular blocky ; hard, friable, slightly sticky and slightly plastic; common very fine roots; common very fine tubular pores; few thin clay films on vertical faces of peds; noneffervescent; slightly alkaline (pH 7.8); clear smooth boundary. (Combined thickness of the Bt horizons is 0 to 55 cm)

Bk1--69 to 91 cm; light gray (10YR 7/2) loam, light olive brown (2.5Y 5/3) moist; massive; hard, friable, slightly sticky and slightly plastic; few very fine roots; common very fine tubular pores; common fine calcium carbonate threads; strongly effervescent (19 percent calcium carbonate); moderately alkaline (pH 8.0); abrupt smooth boundary.

Bk2--91 to 124 cm; light gray (10YR 7/2) very gravelly loam, light olive brown (2.5Y 5/3) moist; massive; hard, friable, slightly sticky and slightly plastic; few fine roots; common very fine tubular pores; common fine calcium carbonate threads; 40 percent gravel; strongly effervescent (35 percent calcium carbonate); moderately alkaline (pH 8.0); abrupt smooth boundary. (Combined thickness of the Bk horizons is 25 to 96 cm)

2Bk3--124 to 152 cm; very gravelly loamy sand; single grain; loose; calcium carbonate coats on bottoms of rock fragments; 45 percent gravel; slightly effervescent (12 percent calcium carbonate); moderately alkaline (pH 8.1).

TYPE LOCATION: Teton County, Idaho; about 3.4 kilometers southwest of Tetonia; 788 meters east and 292 meters north from southwest corner of section 5, T.5N., R.45E.; Tetonia USGS topographic quadrangle; lat. 43 degrees, 47 minutes, 1.9 seconds N. and long. 111 degrees, 10 minutes, 17.1 seconds W., NAD 83.

RANGE IN CHARACTERISTICS:
Mollic epipedon thickness: 50 to 75 cmControl section total clay range: 8 to 27 percent; noncarbonated clay averages 8 to 18 percent
Carbonate clay: 5 to 18 percent in the calcic horizon
Control section rock fragments: 0 to 45 percent (weighted average is less than 35 percent)
Depth to calcic horizon: 50 to 97 cm
Calcium carbonate equivalent: 0 to 35 percent in the particle size control section
Depth to sandy-skeletal material (2Bk3 horizon): 100 to 152 cm
Mean annual soil temperature: 6 to 8 degrees C.
Mean summer soil temperature: 15 to 18.9 degrees C. (frigid soil temperature regime)

Ap or A horizons
Hue: 10YR or 7.5YR moist, 2.5Y or 10YR dry
Value: 2 or 3 moist, 4 or 5 dry
Chroma: 2 or 3 moist
Rock fragments: 0 to 5 percent gravel

Bt horizons
Hue: 7.5YR or 10YR moist
Value: 2 or 3 moist, 4 to 6 dry
Chroma: 2 or 3 moist, 2 or 3 dry
Rock fragments: 0 to 5 percent gravel
Reaction: slightly or moderately alkaline

Bk horizons
Hue: 2.5Y or 10YR moist
Value: 3 to 6 moist
Chroma: 3 or 4 moist, 2 or 3 dry
Fine-earth texture: L or SL with 0 to 45 percent gravel and more than 15 percent coarser than very fine sand
Effervescence: strong to violent
Calcium carbonate equivalent: 15 to 35 percent

2Bk horizon
Hue: 10YR or 7.5YR
Value: 3 to 6 moist
Chroma: 3 or 4 moist
Fine-earth texture: LS or S with 45 to 85 percent gravel
Effervescence: slight to violent
Calcium carbonate equivalent: 5 to 35 percent
Reaction: moderately or strongly alkaline

COMPETING SERIES: These are the Jipper, Stipe, and Richvale series. Jipper soils are deep to lithic contact. Stipe soils are moderately deep to lithic contact. Richvale soils have sandy-skeletal materials at depths greater than 152 cm.

GEOGRAPHIC SETTING:
Landscape: alluvial and outwash plains
Landform: fan remnants and stream terraces
Elevation: 1814 to 1890 meters
Slope: 0 to 4 percent
Parent material: mixed alluvium with loess influence
Mean annual air temperature: 3.3 to 6.7 degrees C
Mean annual precipitation: 305 to 457 mm
Frost free period: 40 to 70 days

GEOGRAPHICALLY ASSOCIATED SOILS: These are the St. Anthony, Felt, Arimo and Redfish series. St. Anthony, Felt and Arimo are on the same landform. St. Anthony soils are in swales and have a loamy-skeletal particle size class. Felt soils are on convex areas and steep slopes and are Calcixerolls. Arimo soils are on lower positions and have a coarse-loamy over sandy or sandy-skeletal particle size class. Redfish soils are on floodplains of streams and have an aquic moisture regime.

DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY:
Drainage class: well drained
Runoff: low
Saturated hydraulic conductivity: moderately high in the upper part and very high in the lower part

USE AND VEGETATION:
Major uses: dryland wheat or barley, irrigated wheat, barley, alfalfa, and pasture. Dominant native vegetation: bluebunch wheatgrass, Nevada bluegrass, junegrass, needleandthread grass, mountain big sagebrush, three-tip sagebrush, and some rabbitbrush.

DISTRIBUTION AND EXTENT:
Distribution: Southeastern Idaho, MLRA 13
Extent: the series is not extensive

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

SERIES ESTABLISHED: Teton County, Idaho, 1975; Teton Area, Idaho-Wyoming Soil Survey.

REMARKS: Diagnostic horizons and soil characteristics recognized in this pedon are:
Mollic epipedon: from a depth of 0 to 69 cm
Calcic horizon: from a depth of 69 to 124 cm
Particle size control section: from a depth of 25 to 100 cm
Soil temperature regime: frigid
Soil moisture regime: xeric

ADDITIONAL DATA:
Typical pedon was not sampled.
Additional reference samples are PEDON ID:
S06ID-081-004


National Cooperative Soil Survey
U.S.A.