IDENTIFIERS
Current Taxon Name (Soil Name):
Edloe
OSD
Series Extent
User Site ID:
S1957CO015003
User Pedon ID:
S1957CO015003
Vegetation Plot ID:
S1957CO015003
Lab Information:
Certified Lab Pedon Description -
no
Lab Source ID -
SSL
Lab Pedon # -
40A3868
NCSS Pedon Lab Data NASIS Record ID -
39514
Print Date:
11/22/2024
LOCATION
Location Description:
Trout Creek Watershed, Chaffee County, Colorado.
State:
Colorado
County:
CO015—Chaffee
Non-MLRA Soil Survey Area:
CO658—Chaffee-Lake Area, Colorado, Parts of Chaffee and Lake Counties
PEDON
Describers Name:
A. J. Cline
Pedon Purpose:
full pedon description
Pedon Record Orgin:
Converted from PDP 3.x
Pedon #:
3
Sampled As Information:
Soil Name -
Edloe
Classificaton Date -
9/8/1957
Dynamic Soil Properties:
Pedoderm Loose Cover Indicator -
no
Hydric:
no
SITE
Landform:
mountainside
Drainage Class:
well
Surface Fragments:
Benchmark Soil?:
no
VEGETATION
SITE OBSERVATION
Observation Date:
9/8/1957 (actual site observation date)
Surface Cover Properties:
Site Obs. Cover Kind 1 -
tree cover
Site Obs. Cover Kind 2 -
other tree cover
Pedoderm Loose Cover Indicator -
no
Drained? -
no
Bedded Soil? -
no
Forest Plantation? -
no
Vegetation Plot Plants
Plant Symbol
Scientific Name
National Vernacular Name
Plant Type Group
Canopy Cover %
Vegetation Stata Level
ABIES
PICEA
Abies
Picea
fir
spruce
—
—
—
—
—
—
Setting and Climate
Slope
Slope Length USLE
Upslope Length
Elev.
Corr. Elev
Aspect
MAP
REAP
FFD
MAAT
MSAT
MWAT
MAST
MSST
MWST
MFFP
PE Index
Climate Station ID
Climate Station Name
Climate Station Type
%
m
degrees
mm
mm
C
mm
45
—
—
3034
—
0
—
—
—
—
—
—
—
—
—
—
—
—
—
—
Ao—0 to 1 centimeters (0.0 to 0.4 inches); fragments. Lab sample # 40A29623. This horizon is a very thin mat of organic material in both decomposed and undecomposed forms. The undecomposed portions are mainly spruce and fir needles.
A1—1 to 4 centimeters (0.4 to 1.6 inches); very dark gray (10YR 3/1), gray (10YR 5/1), dry; gravelly sandy loam; moderate fine granular structure; soft, very friable; 25 percent by volume 2-39-75 millimeter unspecified fragments; noneffervescent; neutral, pH 6.8, unspecified; abrupt smooth boundary. Lab sample # 40A29624
A21—4 to 9 centimeters (1.6 to 3.5 inches); brown (10YR 4/3), pale brown (10YR 6/3), dry; gravelly sandy loam; 1 percent yellowish brown (10YR 5/6) faint mottles; weak fine platy parts to moderate fine granular structure; soft, very friable; 20 percent by volume 2-39-75 millimeter unspecified fragments; noneffervescent; neutral, pH 6.6, unspecified; clear wavy boundary. Lab sample # 40A29625
A22—9 to 26 centimeters (3.5 to 10.2 inches); dark grayish brown (10YR 4/2), light brownish gray (10YR 6/2), dry; gravelly loamy sand; 1 percent yellowish brown (10YR 5/6) faint mottles; moderate fine granular structure; soft, very friable; 50 percent by volume 2-39-75 millimeter unspecified fragments; noneffervescent; neutral, pH 6.6, unspecified; diffuse wavy boundary. Lab sample # 40A29626
B1—26 to 47 centimeters (10.2 to 18.5 inches); brown (10YR 5/3), pale brown (10YR 6/3), dry; stony sandy loam; moderate fine granular structure; soft, very friable; clay films on horizontal faces of peds; 30 percent by volume 250-425-600 millimeter unspecified fragments and 30 percent by volume 2-39-75 millimeter unspecified fragments; noneffervescent; neutral, pH 6.6, unspecified; gradual wavy boundary. Lab sample # 40A29627. Some of the aggregates in this horizon appear to be similar to that of the horizon below but are imbedded in a light-colored material similar to that of the horizon above; some of the soil aggregates have thin continuous clay skins and in some parts of the horizon thin seams of clay-like material are clearly visible.; continuous - phpvsfiid 197033; continuous - phpvsfiid 197033
B2t—47 to 80 centimeters (18.5 to 31.5 inches); brown (10YR 4/3), pale brown (10YR 6/3), dry; very stony sandy clay loam; weak medium subangular blocky structure; hard, friable; 75 percent clay films on faces of peds; fragments; noneffervescent; neutral, pH 6.6, unspecified. Lab sample # 40A29628. The texture as given is that of the fine textured material which occurs between the rocks and gravel fragments; this horizon is mainly well-weathered granite and biotite schist with about 90 percent of the horizon being rock fragments. It is believed that this horizon represents the B2 horizons of this soil that is forming in the cracks between the rocks and may continued for some depth. It was impossible at this location to penetrate below 31 inches without an excessive amount of labor.