LOCATION ROCKCREEKBUTTE     OR
Tentative Series
IRD. RJO/JLW/DAL
06/2007

ROCKCREEKBUTTE SERIES


The Rockcreekbutte series consists of moderately deep, well drained soils on backslopes of mountains. Rockcreekbutte soils formed in colluvium from granite with volcanic ash mixed in surface horizons. Slopes are 0 to 90 percent. Mean annual precipitation is about 45 inches and the mean annual temperature is about 35 degrees F.

TAXONOMIC CLASS: Loamy-skeletal, isotic Haploxerandic Humicryepts

TYPICAL PEDON: Rockcreekbutte extremely stony ashy coarse sandy loam - sparse woodland, on a 55 percent south-facing slope at an elevation of 7,650 feet. (Colors are for moist soil unless otherwise noted.)

Oi--0 to 1 inch; slightly decomposed needles, leaves and twigs.

A--1 to 8 inches; very dark grayish brown (10YR 3/2) extremely stony ashy coarse sandy loam, dark grayish brown (10YR 4/2) dry; weak fine granular structure; soft, very friable, nonsticky and nonplastic; few fine, medium, and coarse roots; many fine irregular pores; 30 percent gravel, 10 percent cobbles, and 40 percent stones; strongly acid (pH 5.5); clear smooth boundary. (7 to 14 inches thick)

Bw--8 to 21 inches; dark yellowish brown (10YR 3/4) extremely stony coarse sandy loam, yellowish brown (10YR 5/4) dry; weak, medium subangular blocky structure; soft, very friable, nonsticky and nonplastic; common fine, medium, and coarse roots; common fine and few medium irregular pores; 20 percent gravel, 10 percent cobbles, and 40 percent stones; moderately acid (pH 6.0); gradual smooth boundary. (12 to 28 inches thick)

C--21 to 36 inches; brown (10YR 4/3) extremely stony coarse sandy loam, yellowish brown (10YR 5/4) dry; single grain; loose, very friable, nonsticky and nonplastic; few fine and coarse, and common medium roots; common fine and medium irregular pores; 20 percent gravel, 10 percent cobbles, and 50 percent stones; moderately acid (pH 6.0); abrupt irregular boundary. (0 to 21 inches thick)

R--36 inches; granodiorite.

TYPE LOCATION: Baker County, Oregon
Section 32 (NW 1/4, SE 1/4, NW 1/4), T. 7 S., R. 37 E.
Latitude: 44 degrees, 54 minutes, 55 seconds North
Longitude: 118 degrees, 12 minutes, 44 seconds West
UTM coordinates: zone 11; 4974036.5 northing 404314.8 easting; NAD27
USGS Quadrangle: Anthony Lakes

RANGE IN CHARACTERISTICS:
Soil Temperature: cryic regime
Mean Annual Soil Temperature: 33 to 40 degrees F
Mean Summer Soil Temperature: 39 to 47 degrees F
Mean Winter Soil Temperature: 26 to 36 degrees F
Soil Moisture: xeric regime; dry 45 to 55 consecutive days in summer

particle-size control section: 10 inches below mineral soil surface to a lithic contact
clay content, average: 3 to 10 percent
rock fragment content, average: 40 to 75 percent
rock fragment shape: subangular to subrounded

andic subgroup properties: upper boundary at the mineral soil surface; 7 to 14 inch thick ash mantle
Al+1/2Fe(aox): 1.0 to 2.0 percent
bulk density: 0.8 to 1.0 g/cc
P retention: 50 to 75 percent
glass content in the 0.02-2.0mm fraction: 20 to 45 percent
water content 1500 kPa (air dried): 5 to 12 percent
8Si + 2Fe (aox): 3 to 5 percent
umbric epipedon: 7 to 13 inches thick
cambic horizon: 12 to 28 inches thick
lithic contact, depth to: 20 to 40 inches

A horizon:
color, moist: 10YR 3/2, 3/3
color, dry: 10YR 4/2, 4/3, 5/3
texture: STV-ASHY-SL, STX-ASHY-COSL
clay content: 5 to 10 percent
rock fragment content: 35 to 80 percent
gravel: 20 to 35 percent
cobbles: 0 to 20 percent
stones: 0 to 40 percent
reaction: very strongly acid to strongly acid; pH: 4.5 to 5.5
base saturation (NH4OAc): 30 to 45 percent

Bw horizon:
color, moist: 10YR 3/4
color, dry: 10YR 4/3, 4/4, 5/3, 5/4
texture: STV-SL, STX-COSL, CBV-SL, STV-L, STX-SL
clay content: 5 to 12 percent
rock fragment content: 40 to 75 percent
gravel: 10 to 35 percent
cobbles: 0 to 20 percent
stones: 10 to 40 percent
reaction: strongly acid to moderately acid; pH: 5.1 to 6.0
base saturation (NH4OAc): 20 to 40 percent

C horizon:
color, moist: 10YR 4/3, 5/4
color, dry: 10YR 5/4, 6/4
texture: STX-COSL, STX-SL
clay content: 3 to 5 percent
rock fragment content: 60 to 80 percent
gravel: 20 to 25 percent
cobbles: 10 to 20 percent
stones: 15 to 50 percent
reaction: moderately acid; pH: 5.6 to 6.0
base saturation (NH4OAc): 20 to 40 percent

COMPETING SERIES:
Clarkscreek (T): formed in till from mixed rocks, mixed with volcanic ash and loess; rock fragments are rounded or subrounded; base saturation (NH4OAc) 50 to 75 percent in more than one-half the thickness between 10 and 30 inches;
Growden: very deep, formed in colluvium from siliceous rocks with a mantle of volcanic ash; no cambic horizon
Puzzlecreek: formed in colluvium from basalt mixed with volcanic ash and loess in surface horizons; rock fragments are angular to subangular in shape; base saturation (NH4OAc) 50 to 75 percent in more than one-half the thickness between 10 and 30 inches;
Rustlerpeak: moderately deep (20 to 40 inches) to a paralithic contact; 20 to 35 percent clay in the particle-size control section

GEOGRAPHIC SETTING:
Landform: backslopes of mountains
Slope gradient: 0 to 90 percent
Parent material: colluvium with an influence of volcanic ash in surface horizons
Lithology: Mazama ash over granitic rocks
Elevation: 5,800 to 8,000 feet
Climate: cold, wet winters and cool, dry summers
Mean annual precipitation: 35 to 55 inches
Mean annual air temperature: 31 to 38 degrees F
Frost-free period: 20 to 60 days

GEOGRAPHICALLY ASSOCIATED SOILS:
Elkhorncrest: on ridges and convex backslopes under subalpine fir and whitebark pine forest; shallow to bedrock;
Granitemountain: on colluvial backslopes and footslopes under mountain shrub with sparse cold forest; very deep
Leespeak: on planer backslopes and shoulders under shrubs and herbs
Prouty: on sideslopes under subalpine fir forest; 20 to 40 inches to a paralithic contact
Pattenbutte: on backslopes and shoulders of mountains under grassland; shallow to bedrock

DRAINAGE AND PERMEABILITY:
Drainage: well drained
Permeability: moderately rapid

USE AND VEGETATION:
Use: watershed, wildlife habitat, livestock grazing and recreation
Native vegetation: widely scattered subalpine fir, whitebark pine and lodgepole pine with gooseberry, montain big sagebrush, mountain snowberry, phlox, fleeceflower, lupine, asters and elk sedge.
Plant Association: ABLA-PIAL-/POPH (subalpine fir-whitebark pine/fleeceflower); may include: ABLA(PIAL)/CAGE (subalpine fir-whitebark pine/elk sedge), ABLA/VASC/POPU3 (subalpine fir/grouse huckleberry/skunk leaved polemonium) or ABLA/CARU (subalpine fir/pinegrass).

DISTRIBUTION AND EXTENT:
Distribution: Blue Mountains of northeastern Oregon; MLRA 43c
Extent: small

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

SERIES PROPOSED: Wallowa-Whitman National Forest, Oregon 2007. The name is from a stream in the Elkhorn Mountains.

REMARKS: Diagnostic horizons and features recognized in this pedon are:
umbric epipedon: 1 to 8 inches; A
cambic horizon: 8 to 21 inches; Bw
andic subgroup properties: 1 to 8 inches; A
particle-size control section: 10 to 36 inches; Bw, C
dystric feature: (base saturation < 50%): 11 to 31 inches; Bw, C


National Cooperative Soil Survey
U.S.A.