IDENTIFIERS
Current Taxon Name (Soil Name):
Edloe
OSD
Series Extent
User Site ID:
S1957CO015002
User Pedon ID:
S1957CO015002
Vegetation Plot ID:
S1957CO015002
Lab Information:
Certified Lab Pedon Description -
no
Lab Source ID -
SSL
Lab Pedon # -
40A3867
NCSS Pedon Lab Data NASIS Record ID -
39513
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 #:
2
Sampled As Information:
Soil Name -
Edloe
Classificaton Date -
9/18/1957
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:
9/18/1957 (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
ARUV
PICEA
Abies
Arctostaphylos uva-ursi
Picea
fir
kinnikinnick
spruce
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—
—
—
—
—
—
—
—
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
42
—
—
3004
—
0
—
—
—
—
—
—
—
—
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—
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Ao—0 to 3 centimeters (0.0 to 1.2 inches); fragments. Lab sample # 40A29617. This is a thin organic mat made up mostly of undecomposed pine needles, leaves, and grass remains, but having its lower portion moderately well decomposed. It rests abruptly on the horizon below.
A1—3 to 8 centimeters (1.2 to 3.1 inches); very dark grayish brown (10YR 3/2), grayish brown (10YR 5/2), dry; gravelly sandy loam; moderate fine granular structure; soft, very friable; 25 percent by volume 2-39-75 millimeter unspecified fragments; noneffervescent; abrupt smooth boundary. Lab sample # 40A29618
A2—8 to 23 centimeters (3.1 to 9.1 inches); grayish brown (10YR 5/2), light gray (10YR 7/2), dry; gravelly loamy sand; 3 percent yellowish brown (10YR 5/4) distinct mottles; weak fine platy parts to moderate fine granular structure; soft, very friable; 40 percent by volume 2-39-75 millimeter unspecified fragments; noneffervescent; gradual wavy boundary. Lab sample # 40A29619
B1—23 to 36 centimeters (9.1 to 14.2 inches); brown (10YR 5/3), very pale brown (10YR 7/3), dry; gravelly sandy loam; weak medium subangular blocky parts to moderate fine granular structure; soft, very friable; 10 percent clay films on faces of peds; 40 percent by volume 2-39-75 millimeter unspecified fragments; noneffervescent; gradual wavy boundary. Lab sample # 40A29620. This horizon contains some aggregates similar in character to those of the horizon below but these are imbedded in light-colored material similar to that of the overlying horizon; there are a few thin continuous clay skins on some of the soil aggregates, and in some portions of the horizon seams of clay-like material are visible.; continuous - phpvsfiid 197031; continuous - phpvsfiid 197031
B2t—36 to 49 centimeters (14.2 to 19.3 inches); brown (10YR 4/3), pale brown (10YR 6/3), dry; stony sandy clay loam; moderate medium subangular blocky structure; hard, friable; clay films on faces of peds; 30 percent by volume 250-425-600 millimeter unspecified fragments and 35 percent by volume 2-39-75 millimeter unspecified fragments; noneffervescent; diffuse irregular boundary. Lab sample # 40A29621. Some gray coating material occurs on the surface of the soil aggregates in this horizon.; continuous - phpvsfiid 197032; continuous - phpvsfiid 197032
Cr—49 to 89 centimeters (19.3 to 35.0 inches); fragments. Lab sample # 40A29622. This horizon is mainly weathered granite and biotite schist. The material is partially indurated but usually can be broken between the thumb and finger. Its consistence increases with depth.