IDENTIFIERS
Current Taxon Name (Soil Name):
Arvada
OSD
Series Extent
User Site ID:
S1954WY025001
User Pedon ID:
S1954WY025001
Vegetation Plot ID:
S1954WY025001
Lab Information:
Certified Lab Pedon Description -
no
Lab Source ID -
SSL
Lab Pedon # -
40A3431
NCSS Pedon Lab Data NASIS Record ID -
38546
Print Date:
2/3/2025
LOCATION
Location In Web Soil Survey
AOI is roughly a square mile and pedon is marked in the center.
Location in SoilWeb
Location in Google Maps
Std. Latitude:
42.8052788
Std. Longitude:
-106.5916672
Datum:
WGS84
Township:
33N
Range:
81W
Section:
29
PLSS Details:
300 feet south and 150 feet east of northwest corner
State:
Wyoming
County:
WY025—Natrona
Non-MLRA Soil Survey Area:
WY625—Natrona County Area, Wyoming
PEDON
Describers Name:
A. J. Cline
Pedon Purpose:
full pedon description
Pedon Record Orgin:
Converted from PDP 3.x
Pedon #:
1
Sampled As Information:
Soil Name -
Arvada
Classificaton Date -
8/17/1954
Dynamic Soil Properties:
Pedoderm Loose Cover Indicator -
no
Hydric:
no
SITE
Landform:
terrace
Slope Shape Down:
convex
Drainage Class:
well
Surface Fragments:
Benchmark Soil?:
no
VEGETATION
SITE OBSERVATION
Observation Date:
8/17/1954 (actual site observation date)
Surface Cover Properties:
Site Obs. Cover Kind 1 -
grass/herbaceous 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
2LICHN
2MOSS
BOGR2
—
—
Bouteloua gracilis
Lichen
Moss
blue grama
—
—
—
—
—
—
—
—
—
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
5
—
—
—
—
270
—
—
—
—
—
—
—
—
—
—
—
—
—
—
A2—0 to 8 centimeters (0.0 to 3.1 inches); grayish brown (10YR 5/2), white (10YR 8/1), dry; fine sandy loam; weak coarse platy parts to moderate fine granular structure; soft, very friable; fragments; noneffervescent; clear smooth boundary. Lab sample # 40A26579
B2t—8 to 23 centimeters (3.1 to 9.1 inches); dark grayish brown (10YR 4/2), grayish brown (10YR 5/2), dry; silty clay; moderate medium columnar parts to strong medium angular blocky structure; very hard, very firm; 30 percent clay films; fragments; noneffervescent; abrupt smooth boundary. Lab sample # 40A26580. structural aggregates have well rounded caps.
B3sa—23 to 38 centimeters (9.1 to 15.0 inches); light olive brown (2.5Y 5/3), light yellowish brown (2.5Y 6/3), dry; silty clay loam; moderate coarse prismatic parts to moderate coarse angular blocky structure; very hard, firm; 1 percent carbonate concretions; fragments; strong effervescence; gradual irregular boundary. Lab sample # 40A26581. the horizon contains a few small calcium carbonate concretions.
C1sa—38 to 58 centimeters (15.0 to 22.8 inches); light olive brown (2.5Y 5/3), light brownish gray (2.5Y 6/2), dry; clay loam; weak coarse angular blocky structure; very hard, firm; carbonate masses and 1 percent carbonate concretions; fragments; strong effervescence; gradual smooth boundary. Lab sample # 40A26582. the horizon contains much calcium carbonate and other salts; calcium carbonate chiefly as lime flour but with a few concretions.
C2sa—58 to 76 centimeters (22.8 to 29.9 inches); olive gray (5Y 5/2), light olive gray (5Y 6/2), dry; sandy clay loam; massive, and weak coarse subangular blocky; very hard, firm; carbonate concretions and carbonate masses and gypsum crystals, unspecified; fragments; strong effervescence; gradual smooth boundary. Lab sample # 40A26583. horizon contains much accumulated calcium carbonate and other salts; calcium carbonate chiefly as lime flour; there are a few concretions believed to be calcium sulfate in the lower part.
C3sa—76 to 104 centimeters (29.9 to 40.9 inches); pale olive (5Y 6/3), pale olive (5Y 6/3), dry; sandy clay loam; massive; very hard, firm; fragments; strong effervescence. Lab sample # 40A26584. horizon contains some visible calcium carbonate and other salts but much less than the horizons above; this horizon consists principally of reworked clayey alluvium washed down the sides of old terrace levels.