LOCATION LAYVIEW            NV
Established Series
Rev. JBF-CEJ-TM
01/2009

LAYVIEW SERIES


The Layview series consists of shallow, well drained soils formed in residuum and colluvium from andesite, rhyolite, chert and tuff. Layview soils are on mountain crests, summits, shoulders and side slopes. Slopes are 4 to 75 percent. The mean annual precipitation is about 360 mm and the mean annual temperature is about 6 degrees C.

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

TYPICAL PEDON: Layview very gravely sandy loam, rangeland. (Colors are for dry soil unless otherwise noted.) The soil surface is covered with 10 percent stones, 15 percent cobbles and 50 percent gravel.

A--0 to 8 cm; brown (10YR 5/3) very gravelly sandy loam, dark brown (10YR 3/3) moist; moderate medium platy structure; slightly hard, very friable, slightly sticky and slightly plastic; few very fine roots; many very fine vesicular pores; 35 percent pebbles; neutral (pH 7.2); abrupt smooth boundary (8 to 20 cm thick)

Bt1--8 to 18 cm; brown (10YR 5/3) very gravelly clay loam, dark brown (10YR 3/3) moist; weak medium subangular blocky structure parting to moderate fine granular; slightly hard, very friable, sticky and plastic; common very fine and fine roots; common very fine tubular pores; few thin clay film lining pores; 35 percent pebbles; neutral (pH 7.2); clear wavy boundary. (8 to 25 cm thick)

Bt2--18 to 30 cm; yellowish brown (10YR 5/4) very gravelly clay loam, dark yellowish brown (10YR 4/4) moist; moderate medium angular blocky structure; hard, friable, sticky and plastic; few fine and common medium roots; few very fine tubular pores; few moderately thick clay films lining pores; 40 percent pebbles, 10 percent cobbles; neutral (pH 7.2); abrupt irregular boundary. (0 to 20 cm thick)

2R--30 cm, fractured tuff.

TYPE LOCATION: Lander County, Nevada, about 41 miles southwest of Austin, approximately 1,700 feet west and 1,100 feet south of northeast corner of section 1, R. 33 E., T. 16 N. latitude 39 degrees 16 minutes 57 seconds N and longitude 118 degrees 13 minutes 36 seconds W; NAD 83.

RANGE IN CHARACTERISTICS:

Soil moisture - These soils are usually dry during summer and fall, moist mid-October through mid-July.

Soil temperature - 6 to 8 degrees C.

Mean summer soil temperature - 10 to 15 degrees C.

Depth to bedrock - 25 to 36 cm.

Reaction - Neutral or mildly alkaline.

Mollic epipedon thickness - 18 to 30 cm.

Particle-size control section - Clay content: 18 to 30 percent.
Rock fragments: 35 to 60 percent, mainly pebbles.

A horizon - Value: 4 or 5 dry, 2 or 3 moist.
Chroma: 2 or 3.

Bt horizon - Value: 4 or 5 dry, 3 or 4 moist.
Chroma: 2 through 4.
Texture: Very gravelly loam or very gravelly clay loam.
Clay content: 22 to 35 percent.
Rock fragments: 35 to 60 percent, mainly pebbles.
Structure: Weak or moderate subangular or angular blocky.
Consistence: Soft to hard, very friable or friable, slightly sticky or sticky and slightly plastic or plastic.

COMPETING SERIES: These are the Bushpark, Copenhaver, Donkehill, Hogmalat, Maygal, Mosroc, Nielson, Nieman, Notstew and Thiefridge series.

Bushpark soils have a udic soil moisture regime. Copenhaver, Donkehill, Neiman and Nielsen soils have a mean annual soil temperature less than 6 degrees C. Hogmalat soils are strongly to medium acid throughout. Maygal and Thiefridge soils have bedrock at 36 to 50 cm. Mosroc soils formed in weathered material derived dominantly from granite and the mollic epipedon includes the entire argillic horizon. Notstew soils have more than 35 percent clay in the argillic horizon.

GEOGRAPHIC SETTING: Layview soils are on convex mountain crests, summits, shoulders and side slopes. These soils formed in residuum and colluvium from rhyolite, andesite, chert and tuffaceous rocks. Slopes are 4 to 75 percent. Elevations are 2,134 to 3,048 meters. The climate is cool, semi-arid with a mean annual precipitation ranging from 300 to 400 mm; mean annual temperature is 5 to 6 degrees C.,and the frost-free season is 50 to 80 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Hapgood, Packer, and Mosquet series. Hapgood and Packer are deep soils, Mosquet is clayey-skeletal and ruptic.

DRAINAGE AND PERMEABILITY: Well drained; runoff is medium or very rapid; moderately slow permeabiltiy; moderately high saturated hydraulic conductivity.

USE AND VEGETATION: Rangeland and wildlife habitat. The present vegetation is Thurber needlegrass, Sandberg bluegrass, Idaho fescue, and low sagebrush.

DISTRIBUTION AND EXTENT: Central Nevada. Layview soils are of small extent. MLRA 27, 28B, 24.

MLRA OFFICE RESPONSIBLE: Reno, Nevada

SERIES ESTABLISHED: Lander County, Nevada, South Part, 1985.

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

Mollic epipedon - The zone from the soil surface to about 18 cm (A and Bt1 horizons).

Argillic horizon - The zone from about 8 to 30 cm (Bt1 and Bt2 horizons).

Lithic contact - The boundary at about 30 cm (R layer).

Particle-size control section - The zone from the soil surface to about 30 cm (A, Bt1 and Bt2 horizons).


National Cooperative Soil Survey
U.S.A.