LOCATION COPPERSMITH        CA NV
Established Series
Rev. JBF/TM
06/2006

COPPERSMITH SERIES


The Coppersmith series consists of very deep, well drained soils formed in eolian material, beach deposits, alluvium derived from volcanic rocks, and volcanic ash. Coppersmith soils are on beach terraces. Slopes are 2 to 8 percent. The mean annual precipitation is about 11 inches, and the mean annual temperature is about 48 degrees F.

TAXONOMIC CLASS: Ashy, glassy, mesic Vitritorrandic Argixerolls

TYPICAL PEDON: Coppersmith ashy sandy loam - rangeland. (Colors are for dry soil unless otherwise noted.)

A1--0 to 2 inches; grayish brown (10YR 5/2) ashy sandy loam, very dark grayish brown (10YR 3/2) moist; moderate thin and medium platy structure parting to strong fine subangular blocky; soft, very friable, nonsticky and nonplastic; many very fine roots; many very fine and fine and few medium interstitial pores; noneffervescent; 5 percent igneous gravel and 1 percent cobbles; neutral (pH 6.8); abrupt smooth boundary. (2 to 4 inches thick)

A2--2 to 5 inches; grayish brown (10YR 5/2) ashy sandy loam, very dark grayish brown (10YR 3/2) moist; weak very coarse prismatic structure parting to moderate thick platy; soft, very friable, slightly sticky and slightly plastic; many very fine and few fine and medium roots; many very fine interstitial pores and few very fine and fine tubular pores; noneffervescent; neutral (pH 6.8); abrupt smooth boundary. (2 to 5 inches thick)

Bt1--5 to 11 inches; brown (10YR 5/3) ashy sandy clay loam, dark brown (10YR 3/3) moist; moderate medium and coarse subangular blocky structure; very hard, friable, moderately sticky and moderately plastic; many very fine to medium roots and and coarse roots in mat at top of horizon; many very fine and fine tubular pores; common distinct dark brown (10YR 3/3) clay films between sand grains and few distinct clay films on faces of peds and in pores; noneffervescent; neutral (pH 7.2); clear wavy boundary. (4 to 8 inches thick)

Bt2--11 to 16 inches; pale brown (10YR 6/3) ashy sandy clay loam, dark yellowish brown (10YR 3/4) moist, brown (10YR 4/3), crushed, moist; moderate medium subangular blocky structure; very hard, friable, moderately sticky and moderately plastic; many very fine and fine and few medium roots; many very fine and fine tubular pores; many distinct brown (10YR 4/3) clay films on faces of peds and in pores; noneffervescent; slightly alkaline (pH 7.4); clear wavy boundary. (4 to 7 inches thick)

Bq1--16 to 24 inches; pale brown (10YR 6/3) ashy fine sandy loam, dark yellowish brown (10YR 3/4) moist, dark yellowish brown (10YR 4/4), rubbed, moist; massive; very hard, firm, brittle, slightly sticky and slightly plastic; few very fine and fine roots; few very fine tubular pores; 50 percent 10 to 50 millimeter hard very firm durinodes; few faint clay films between sand grains; noneffervescent; 5 percent tuff gravel; slightly alkaline (pH 7.4); clear wavy boundary. (6 to 14 inches thick)

Bq2--24 to 30 inches; light yellowish brown (10YR 6/4) ashy fine sandy loam, dark yellowish brown (10YR 4/4) moist; massive; hard, firm, brittle, slightly sticky and slightly plastic; few very fine and fine roots; few very fine tubular pores; 25 percent 10 to 50 millimeter, hard, firm durinodes; noneffervescent; 5 percent tuff gravel; slightly alkaline (pH 7.6); clear smooth boundary. (5 to 10 inches thick)

Bq3--30 to 39 inches; pale yellow (2.5Y 7/3) ashy fine sandy loam, olive brown (2.5Y 4/4) moist; massive; slightly hard, friable, nonsticky and nonplastic; few very fine to medium roots; many very fine interstitial pores and few very fine tubular pores; 25 percent 10 to 25 millimeter durinodes; noneffervescent; 3 percent tuff gravel; moderately alkaline (pH 8.0); clear smooth boundary. (2 to 4 inches thick) (8 to 12 inches thick)

2Bqk--39 to 60 inches; pale yellow (2.5Y 7/3) ashy loamy sand, olive brown (2.5Y 4/4) moist; massive; soft, very friable, nonsticky and nonplastic; few very fine to medium roots; many very fine interstitial pores and few very fine tubular pores; 10 percent 5 to 25 millimeter durinodes; violently effervescent; moderately alkaline (pH 8.4).

TYPE LOCATION: Lassen County, California; at the south end of Surprise Valley; about 1 mile south of Nevada HWY 447 and about 0.75 mile west of the California-Nevada state line; about 700 feet east and 2400 feet south of the northwest corner of Section 23, T. 38 N., R. 17 E; 41 degrees, 8 minutes, 37.2 seconds north latitude and 120 degrees, 01 minutes, 03.8 seconds west longitude. NAD 27 Datum. USGS Snake Lake 7.5 minute quadrangle.

RANGE IN CHARACTERISTICS:
Soil moisture - Usually dry; moist in winter and spring; dry June through October. Soil moisture regime is aridic bordering xeric.
Soil temperature - 47 to 52 degrees F.
Mollic epipedon thickness - 8 to 16 inches, includes the upper part of the Bt horizon.
Depth to base of the Bt horizons - 12 to 24 inches.
Control section - Clay content: 20 to 27 percent.
Mineralogy: 40 to 60 percent volcanic glass in the 0.2 to 2.0 millimeter fraction.

A horizon - Value: 2 or 3 moist. Chroma: 2 or 3.

Bt horizon - Hue: 10YR or 7.5YR.
Value: 5 or 6 dry, 3 or 4 moist.
Chroma: 2 through 4.
Structure: Weak through strong, fine through coarse subangular blocky or angular blocky.
Reaction: Neutral or slightly alkaline.
Rock Fragments: Up to 5 percent pebbles.

Bq horizon - Hue: 10YR or 2.5Y.
Value: 5 through 7 dry, 3 through 6 moist.
Chroma: 3 or 4.
Rock fragments: 0 to 30 percent gravel and 0 to 15 percent paragravel. Lithology of the gravel is mostly andesite and basalt.
Consistence: Subhorizons more than 6 inches thick have hard or very hard, firm and brittle consistence.
Reaction: Slightly alkaline or moderately alkaline.
Other features: 20 to 70 percent durinodes. Some pedons have few very thin (< 2 mm thick) discontinuous and unoriented silica laminae. The durinodes are hard or very hard, firm or very firm, and include some durinodes that are extremely hard and extremely firm.

2Bqk horizon - Value: 6 or 7 dry
Chroma: 3 or 4.
Rock fragments: 0 to 30 percent gravel, 0 to 15 percent paragravel. Lithology of the gravel is mostly andesite and basalt.
Effervescence: Strongly effervescent or violently effervescent. None to few fine or medium soft masses of lime

COMPETING SERIES: These are the Ashone, Bidwell, Ponyspring and Simpson series. Ashone soils are 20 to 40 inches deep to paralithic material. Ashone, Bidwell and Simpson soils lack a Bq horizon with durinodes. Ponyspring soils have secondary calcium carbonate within 6 to 14 inches.

GEOGRAPHIC SETTING: Coppersmith soils are on beach terraces. These soils formed in eolian material, beach deposits,alluvium from volcanic rocks, and volcanic ash. Slopes are 2 to 8 percent. Elevations are 4,500 to 5,490 feet. The climate is cool, semiarid with cool, moist winters and warm, dry summers. The mean annual precipitation is 10 to 12 inches; mean annual temperature is 45 to 50 degrees F, and the frost-free period is 100 to 120 days.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Bareranch (T NV), Devada, Nevadash (T NV) and Saraph. Bareranch soils are ashy-skeletal and are deep to pyroclastic tuff. Devada soils are shallow to hard volcanic rock. Nevadash soils lack a mollic epipedon and are on fan piedmonts. Saraph soils are shallow over tuff.

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

USE AND VEGETATION: Rangeland and wildlife habitat. The vegetation is mainly mountain big sagebrush, Thurber's needlegrass, bluebunch wheatgrass and squawapple.

DISTRIBUTION AND EXTENT: : Western Washoe County, Nevada and eastern Lassen County, California Surprise Valley-Home Camp Area. MLRA 23. These soils are not extensive.

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Davis, California

SERIES ESTABLISHED: Surprise Valley-Home Camp Area, California and Nevada, 2000. The name is from the nearby Coppersmith Mountains.

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

Mollic epipedon - The zone from the soil surface to about 11 inches (The A1, A2 and Bt1 horizons).
Argillic horizon- The zone from about 5 to 16 inches (Bt1 and Bt2 horizons).
Duric feature - The zone from about 16 to 39 inches (Bq1, Bq2 and Bq3 horizons).
Particle-size control section - The zone from about 5 to 16 inches (Bt1 and Bt2 horizons).
Mineralogy - Glass content of the 0.2 to 2 millimeter fraction is more than 30 percent.


National Cooperative Soil Survey
U.S.A.