IDENTIFIERS
Current Taxon Name (Soil Name):
Berthahill
OSD
Series Extent
User Site ID:
S1995ID035008
User Pedon ID:
95ID035008
Lab Information:
Certified Lab Pedon Description -
no
Lab Source ID -
SSL
Lab Pedon # -
96P0025
NCSS Pedon Lab Data NASIS Record ID -
68106
Print Date:
11/12/2024
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:
46.7713890
Std. Longitude:
-115.7888870
Datum:
WGS84
Township:
40N
Range:
5E
Section:
35
PLSS Details:
NE/4
Location Description:
just below Bertha Hill lookout
State:
Idaho
County:
ID035—Clearwater
MLRA:
43—Northern Rocky Mountains
Non-MLRA Soil Survey Area:
ID612—Clearwater Area, Idaho
PEDON
Describers Name:
B.R.
Current Taxonomic Class:
Medial over loamy-skeletal, amorphic Typic Haplocryands
Current Taxon Kind:
series
Pedon Type:
classifies to current taxon name, full description
Pedon Purpose:
full pedon description
Pedon Record Orgin:
Converted from PDP 3.x
Pedon #:
8
Correlated Information:
Soil Name -
Berthahill
Classificaton Date -
1/27/2010
Sampled As Information:
Soil Name -
Berthahill
Taxonomic Class -
Medial over loamy-skeletal, mixed Vitric Haplocrya
Taxon Kind -
series
Classificaton Date -
7/8/1995
Moisture Class -
udic
Dynamic Soil Properties:
Pedoderm Loose Cover Indicator -
no
Hydric:
no
SITE
Landscape:
mountains
Landform:
mountainside
Surface Fragments:
Benchmark Soil?:
no
VEGETATION
SITE OBSERVATION
Observation Date:
7/8/1995 (actual site observation date)
Plant Association Name:
handoff
Surface Cover Properties:
Site Obs. Cover Kind 1 -
tree cover
Site Obs. Cover Kind 2 -
intermixed conifers and hardwoods
Pedoderm Loose Cover Indicator -
no
Drained? -
no
Bedded Soil? -
no
Forest Plantation? -
no
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
28
—
—
1524
—
0
127
—
—
—
—
—
—
—
—
—
—
—
—
—
Oi—0 to 1 centimeters (0.0 to 0.4 inches); fragments; abrupt smooth boundary. Undecomposed and decomposed leaves, needles, twigs and stems.
Oe—1 to 3 centimeters (0.4 to 1.2 inches); fragments; abrupt smooth boundary. Undecomposed and decomposed leaves, needles, twigs and stems
A1—3 to 8 centimeters (1.2 to 3.1 inches); very dark brown (10YR 2/2) crushed, dark grayish brown (10YR 4/2) crushed, dry; silt loam; weak very fine and fine subangular blocky parts to weak very fine and fine granular structure; very friable, nonsticky, nonplastic; 3.0 fine and medium roots throughout and 21.0 coarse roots throughout; 3.0 very fine high-continuity interstitial pores; 10 percent fine iron-manganese concretions; 3 percent by volume subangular 2-39-75 millimeter quartzite fragments; clear wavy boundary. Lab sample # 96P00180
A2—8 to 18 centimeters (3.1 to 7.1 inches); very dark grayish brown (10YR 3/2) crushed, brown (10YR 4/3) crushed, dry; silt loam; weak fine and medium subangular blocky parts to weak fine and medium granular structure; very friable, nonsticky, nonplastic; 3.0 fine and medium roots throughout and 21.0 coarse roots throughout; 3.0 very fine high-continuity interstitial pores; 3 percent fine spherical iron-manganese concretions; 5 percent by volume subangular 2-39-75 millimeter quartzite fragments; abrupt wavy boundary. Lab sample # 96P00181
Bw1—18 to 41 centimeters (7.1 to 16.1 inches); dark yellowish brown (10YR 3/4) crushed, light yellowish brown (10YR 6/4) crushed, dry; silt loam; weak fine and medium subangular blocky structure; soft, very friable, nonsticky, nonplastic; 3.0 fine and medium roots throughout and 0.5 coarse roots throughout; 0.5 very fine low-continuity tubular and 3.0 very fine moderate-continuity interstitial pores; 2 percent fine spherical iron-manganese concretions; 2 percent by volume subrounded 250-425-600 millimeter quartzite fragments and 5 percent by volume subangular 2-39-75 millimeter quartzite fragments and 5 percent by volume subangular 75-162-250 millimeter quartzite fragments; abrupt wavy boundary. Lab sample # 96P00182
Bw2—41 to 54 centimeters (16.1 to 21.3 inches); dark yellowish brown (10YR 3/4) crushed, light yellowish brown (10YR 6/4) crushed, dry; gravelly loam; weak fine and medium subangular blocky structure; slightly hard, friable, nonsticky, nonplastic; 21.0 fine and medium roots throughout and 0.5 coarse roots throughout; 0.5 very fine low-continuity tubular and 21.0 very fine moderate-continuity interstitial pores; 1 percent fine spherical iron-manganese concretions; 5 percent by volume subangular 75-162-250 millimeter quartzite fragments and 10 percent by volume subangular 250-425-600 millimeter quartzite fragments and 10 percent by volume subangular 2-39-75 millimeter quartzite fragments; clear wavy boundary. Lab sample # 96P00183
2B/E—54 to 82 centimeters (21.3 to 32.3 inches); 85 percent brown (7.5YR 5/4) interior and 15 percent light brown (7.5YR 6/4) interior, 85 percent very pale brown (10YR 7/4) interior and 15 percent pink (7.5YR 7/4) interior, dry; gravelly loam; moderate fine and medium subangular blocky structure; slightly hard, friable, nonsticky, nonplastic; 21.0 fine and medium roots between peds and 0.5 coarse roots between peds; 21.0 very fine and fine moderate-continuity interstitial and tubular pores; 2 percent faint brown (7.5YR 4/4) clay films on faces of peds; 5 percent fine platy mica flakes, unspecified; 10 percent by volume subangular 250-425-600 millimeter gneiss-basic fragments and 20 percent by volume subangular 75-162-250 millimeter quartzite fragments and 25 percent by volume subangular 2-39-75 millimeter quartzite fragments; clear smooth boundary. Lab sample # 96P00184. Questionable B/E maybe just a 2Bt1; patchy - phpvsfiid 194779; patchy - phpvsfiid 194779
2Bt1—82 to 107 centimeters (32.3 to 42.1 inches); strong brown (7.5YR 4/6) interior, light brown (7.5YR 6/4) interior, dry; very gravelly loam; moderate medium and coarse subangular blocky structure; slightly hard, firm, slightly sticky, slightly plastic; 0.5 very fine roots throughout and 21.0 fine and medium roots between peds; 21.0 very fine and fine moderate-continuity interstitial and tubular pores; 1 percent faint brown (7.5YR 4/4) clay films on faces of peds; 5 percent fine platy mica flakes, unspecified; 10 percent by volume subangular 250-425-600 millimeter quartzite fragments and 15 percent by volume subangular 75-162-250 millimeter quartzite fragments and 35 percent by volume subangular 2-39-75 millimeter quartzite fragments; clear wavy boundary. Lab sample # 96P00185. Soil moist T/O when described. Structure is hard to get since quartzite when weathers breaks up into fine qtz. gr. Clay bands are so common these alone due to their thickness could qualify for an argillic.; discontinuous - phpvsfiid 182647; discontinuous - phpvsfiid 182647
2Bt2—107 to 133 centimeters (42.1 to 52.4 inches); strong brown (7.5YR 5/6) interior, pink (7.5YR 7/4) interior, dry; extremely gravelly coarse sandy loam; weak fine and medium subangular blocky structure; slightly hard, firm, nonsticky, nonplastic; 21.0 very fine and fine roots between peds and 0.5 coarse roots between peds; 21.0 very fine and fine low-continuity interstitial pores; 2 percent faint brownish yellow (10YR 6/6) skeletans over cutans on tops of soil columns; 2 percent fine platy mica flakes, unspecified; 15 percent by volume subangular 75-162-250 millimeter quartzite fragments and 35 percent by volume subangular 2-39-75 millimeter quartzite fragments; clear wavy boundary. Lab sample # 96P00186. Soil moist T/O when described. Structure is hard to get since quartzite when weathers breaks up into fine qtz. gr. Where A = clay bands 4 to 8"" apart and 1-2"" thick of Sil w/10% mica to Scl w/5% mica. Clay bands are so common these alone due to their thickness could qualify for an argillic.; discontinuous - phpvsfiid 182653; discontinuous - phpvsfiid 182653
2Bt3—133 to 173 centimeters (52.4 to 68.1 inches); 50 percent reddish brown (5YR 5/4) interior and 50 percent yellowish red (5YR 4/6) interior, 50 percent light brown (7.5YR 6/4) interior and 50 percent yellowish red (5YR 5/6) interior, dry; extremely gravelly coarse sandy loam, extremely gravelly sandy clay loam; weak very fine and fine subangular blocky structure; slightly hard, firm, nonsticky, nonplastic; 21.0 very fine and fine roots between peds and 0.5 coarse roots between peds; 0.5 very fine low-continuity tubular and 21.0 very fine low-continuity interstitial pores; 2 percent faint yellowish red (5YR 4/6) skeletans over cutans on tops of soil columns; 1 percent fine platy mica flakes, unspecified; 10 percent by volume subangular 250-425-600 millimeter quartzite fragments and 25 percent by volume subangular 75-162-250 millimeter quartzite fragments and 30 percent by volume subangular 2-39-75 millimeter quartzite fragments; clear smooth boundary. Lab sample # 96P00187. Soil moist T/O when described. Structure is hard to get since quartzite when weathers breaks up into fine qtz. gr. 50% is clay bands and 5-10% mica in bands. Clay bands 1-3"" apart and 1-3"" thick of Scl 5YR 4/6 w/10% mica. Clay bands are so common these alone due to their thickness could qualify for an argillic.; discontinuous - phpvsfiid 182654; discontinuous - phpvsfiid 182654
C—173 to 199 centimeters (68.1 to 78.3 inches); yellowish brown (10YR 5/6) interior, very pale brown (10YR 7/4) interior, dry; extremely gravelly coarse sandy loam; weak massive; slightly hard, firm, nonsticky, nonplastic; 0.5 very fine roots between peds; 0.5 very fine low-continuity interstitial pores; 2 percent faint brown (7.5YR 5/4) skeletans over cutans on tops of soil columns; 2 percent fine platy mica flakes, unspecified; 25 percent by volume subangular 75-162-250 millimeter quartzite fragments and 45 percent by volume subangular 2-39-75 millimeter quartzite fragments. Lab sample # 96P00188. Clay bands 4-7" apart and 1-2" thick of Sl w?5% mica; discontinuous - phpvsfiid 182655; discontinuous - phpvsfiid 182655