LOCATION MEGONOT            MT
Established Series
NRS-SGV-CJH
04/2002

MEGONOT SERIES


The Megonot series consists of moderately deep, well drained soils that formed in residuum from semi-consolidated shale, siltstone or mudstone, or in alluvium over semi-consolidated shale, siltstone or mudstone. These soils are on dissected alluvial fans, ridges, strath terraces, sedimentary plains, lake plains, hills, and escarpments. Slopes are 0 to 60 percent. Mean annual precipitation is about 12 inches, and mean annual air temperature is about 43 degrees F.

TAXONOMIC CLASS: Fine, smectitic, frigid Torrertic Haplustepts

TYPICAL PEDON: Megonot silty clay loam, in non-irrigated cropland. (Colors are for dry soil unless otherwise noted)

Ap--0 to 5 inches; grayish brown (2.5Y 5/2) silty clay loam, dark grayish brown (2.5Y 4/2) moist; moderate medium granular structure; hard, friable, sticky and plastic; many fine roots; many fine vesicular pores; slightly effervescent; neutral (pH 7.2); clear smooth boundary. (3 to 10 inches thick)

Bw--5 to 12 inches; grayish brown (2.5Y 5/2) silty clay loam, dark grayish brown (2.5Y 4/2) moist; weak medium prismatic structure parting to moderate medium and fine subangular blocky; hard, friable, sticky and plastic; common fine and very fine roots; common fine and very fine discontinuous tubular pores; disseminated lime; slightly effervescent; slightly alkaline (pH 7.6); clear smooth boundary. (7 to 20 inches thick)

Bk--12 to 21 inches; grayish brown (2.5Y 5/2) silty clay, dark grayish brown (2.5Y 4/2) moist; moderate medium prismatic structure parting to moderate medium and fine subangular blocky; very hard, firm, sticky and very plastic; common fine and very fine roots; common very fine discontinuous tubular pores; 10 percent soft weathered shale fragments; few medium masses of segregated lime; strongly effervescent; moderately alkaline (pH 8.2); clear wavy boundary. (6 to 20 inches thick)

By--21 to 29 inches; grayish brown (2.5Y 5/2) silty clay, dark grayish brown (2.5Y 4/2) moist; massive or thin platy structure as a result of in situ weathering of shale; hard, firm, sticky and plastic; common fine and very fine roots in cracks and between plates; common fine threads and seams of gypsum; 25 percent soft shale fragments, 10 percent hard shale fragments; disseminated lime; slightly effervescent; moderately alkaline (pH 8.0); gradual wavy boundary. (0 to 12 inches thick)

2Cr--29 to 60 inches; mixed dark gray (5Y 4/1) and olive gray (5Y 4/2) semi-consolidated shale; hard and firm; neutral (pH 6.8).

TYPE LOCATION: Teton County, Montana; 1,200 feet east and 1,500 feet north of the SW corner of sec. 29, T. 23 N., R. 2 W.

RANGE IN CHARACTERISTICS:

Soil temperature - 41 to 47 degrees F.

Moisture control section - between 4 and 12 inches; dry in all parts between four-tenths and five-tenths of the cumulative days per year when the soil temperature at 20 inches is 41 degrees F or above.

Rock fragments - 0 to 15 percent hard shale fragments.

Depth to bedrock - 20 to 40 inches.

Depth to secondary lime - 10 to 27 inches.

A Bky horizon is allowed.

Depth to paralithic contact - 20 to 40 inches.

Ap horizon - Hue: 10YR or 2.5Y

Value: 5 or 6 dry, 4 or 5 moist

Chroma: 2 or 3

Texture: silty clay loam, clay loam, or silty clay

Clay content: 27 to 45 percent

Coarse fragments: 0 to 15 percent pebbles

Reaction: pH 6.6 to 7.8

Bw horizons - Hue: 10YR or 2.5Y

Value: 5 or 6 dry, 4 or 5 moist

Chroma: 2 or 3

Texture: silty clay loam, clay loam, clay or silty clay

Clay content: 35 to 50 percent

Coarse fragments: 0 to 15 percent hard pebbles, 0 to 15 percent soft pebbles

Calcium carbonate equivalent: 1 to 12 percent

Reaction: pH 7.4 to 8.4

Bk horizon - Hue: 10YR, 2.5Y or 5Y

Value: 5 or 6 dry; 4 or 5 moist

Chroma: 2 or 3

Texture: silty clay loam, clay loam, clay or silty clay

Clay content: 35 to 50 percent

Coarse fragments: 0 to 15 percent hard pebbles, 0 to 15 percent soft pebbles

Calcium carbonate equivalent: 5 to 15 percent

Reaction: pH 7.4 to 8.4

By horizon - Hue: 10YR, 2.5Y or 5Y

Value: 4, 5, or 6 dry; 3, 4 or 5 moist

Chroma: 2 or 3

Texture: silty clay loam, clay loam, clay or silty clay

Clay content: 35 to 45 percent

Coarse fragments: 10 to 50 percent soft shale; 5 to 30 percent hard shale fragments

Gypsum: 1 to 5 percent

Reaction: pH 6.6 to 8.4

2Cr horizon - semi-consolidated shale or mudstone

Reaction: pH 5.6 to 7.8

COMPETING SERIES:

Alzada (MT) - does not have a paralithic contact at depths of 20 to 40 inches.

Brunelda (MT) - has a gypsic horizon; does not have a paralithic contact above a depth of 60 inches.

Kobase (MT) - does not have a paralithic contact at depths of 20 to 40 inches.

Nunemaker (MT) - does not have a paralithic contact above a depth of 40 inches.

Teigen (MT) - does not have a paralithic contact above a depth of 40 inches.

Zatoville (MT) - has a gypsic horizon; has horizons of other salt accumulations.

GEOGRAPHIC SETTING:

Landform - dissected alluvial fans; strath terraces; sedimentary plains; lake plains; hills; escarpments; ridges.

Elevation - 2,200 to 5,200 feet.

Slope- 0 to 60 percent.

Parent material - residuum from semi-consolidated shale, siltstone or mudstone, or in alluvium over the semi-consolidated shale, siltstone or mudstone.

Climate - long, cold winters; moist springs; hot, dry summers.

Mean annual precipitation - 10 to 16 inches.

Mean annual air temperature - 39 to 45 degrees F.

Frost-free season - 95 to 135 days.

GEOGRAPHICALLY ASSOCIATED SOILS:

DRAINAGE AND PERMEABILITY: Well drained; slow permeability.

USE AND VEGETATION: Megonot soils are used as rangeland and non-irrigated cropland. Potential native vegetation is mainly bluebunch wheatgrass, green needlegrass, western wheatgrass, needleandthread, winterfat, and skunkbush sumac.

DISTRIBUTION AND EXTENT: Megonot soils are of moderate extent in north central Montana and in Colorado.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: St. Paul, Minnesota

SERIES ESTABLISHED: Choteau-Conrad Area, Montana, 1990.

REMARKS: Soil interpretations record: MT0684.

Diagnostic horizons and features recognized in this pedon are: ochric epipedon - from the soil surface to 5 inches (Ap horizon); cambic horizon - from 5 to 12 inches (Bw horizon); horizon of secondary carbonate accumulation - from 12 to 21 inches (Bk horizon); horizon of gypsum accumulation - from 21 to 29 inches (By horizon); paralithic contact of semi-consolidated shale - at a depth of 29 inches (Cr horizon); particle-size control section - from 10 to 29 inches (Bw, Bk, By horizons). Megonot soils have a frigid temperature regime and an ustic moisture regime that borders on aridic.


National Cooperative Soil Survey
U.S.A.