IDENTIFIERS
Current Taxon Name (Soil Name):
Milton
OSD
Series Extent
User Site ID:
1970OH057022
User Pedon ID:
1970-OH057-022
Lab Information:
Certified Lab Pedon Description -
no
Lab Source ID -
OHSTATE
Lab Pedon # -
GN-022
NCSS Pedon Lab Data NASIS Record ID -
71415
Print Date:
11/23/2024
LOCATION
Location Description:
Glen Helen, 1/2 mi. E of village of Yellow Springs. 100 yds. Nw of Outdoor Education Center Office and 75 yds. NE of Staff Quarters.
State:
Ohio
County:
OH057—Greene
PEDON
Describers Name:
garner
Current Taxonomic Class:
Fine, mixed, mesic Typic Hapludalfs
Pedon Record Orgin:
NASIS
Correlated Information:
Soil Name -
Milton
Classificaton Date -
5/4/2012
Dynamic Soil Properties:
Pedoderm Loose Cover Indicator -
no
Hydric:
no
SITE
Parent Material:
Wisconsinan till; Limestone
Landform:
ground moraine
Drainage Class:
well
Surface Fragments:
Benchmark Soil?:
no
VEGETATION
SITE OBSERVATION
Observation Date:
10/14/1970 (actual site observation date)
Surface Cover Properties:
Site Obs. Cover Kind 1 -
tree cover
Site Obs. Cover Kind 2 -
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
3
—
—
301.8
—
—
—
—
—
—
—
—
—
—
—
—
—
—
—
A—0 to 8 centimeters (0.0 to 3.1 inches); dark grayish brown (10YR 4/2) Error; strong fine granular structure; friable; fragments; slightly acid, pH 6.5; clear smooth boundary. Lab sample # OSU0020302. The upper 6 inches appears to have been cultivated at one time, but it has been retired to woodland for a long enough period that an A1 horizon has reformed.
E—8 to 15 centimeters (3.1 to 5.9 inches); brown (10YR 4/3) Error; moderate fine subangular blocky structure; friable; fragments; slightly acid, pH 6.5; abrupt irregular boundary. Lab sample # OSU0020303. Pendants of the E horizon extend to 12 inches or deeper in what appear to be root channels.
BEt—15 to 25 centimeters (5.9 to 9.8 inches); brown (7.5YR 4/4) Error; moderate medium subangular blocky structure; friable; faint dark yellowish brown (10YR 4/4), moist, clay films; fragments; slightly acid, pH 6.5; gradual smooth boundary. Lab sample # OSU0020304. patchy - phpvsfiid 979906; patchy - phpvsfiid 979906
2Bt1—25 to 48 centimeters (9.8 to 18.9 inches); brown (7.5YR 5/4) and strong brown (7.5YR 5/6) Error; moderate medium subangular blocky, and moderate structure; firm; distinct brown (7.5YR 4/4), moist, clay films; 5 percent by volume nonflat indurated unspecified fragments; slightly acid, pH 6.5; gradual wavy boundary. Lab sample # OSU0020305. Coarse fragments are glacial erratics.; continuous - phpvsfiid 979907; continuous - phpvsfiid 979907
2Bt2—48 to 76 centimeters (18.9 to 29.9 inches); brown (7.5YR 4/4) Error; strong medium subangular blocky, and moderate structure; very firm; distinct dark yellowish brown (10YR 4/4), moist, clay films; 8 percent by volume nonflat indurated unspecified fragments; slightly acid, pH 6.5; abrupt wavy boundary. Lab sample # OSU0020306. Coarse fragments are igneous glacial erratics. Abrupt, wavy boundary follows the contour of the underlying bedrock. Thin pendants of the 2Bt2 horizon extend for 2 to 3 inches into the larger joints in the underlying limestone. The vertical faces of these; continuous - phpvsfiid 979908; continuous - phpvsfiid 979908
3C—76 to 77 centimeters (29.9 to 30.3 inches); pale brown (10YR 6/3) and yellowish brown (10YR 5/4) Error; friable; fragments; slight effervescence; moderately alkaline, pH 8.0; abrupt wavy boundary. This is a thin zone of weathered bedrock that ranges from 0.25 to 1 inch over the horizontal surface of the bedrock and it is slightly thicker where it extends into the joints of the bedrock. It is dominantly 10YR 6/3 but is stained with 10YR 5/4 or 10YR
3R—77 to 84 centimeters (30.3 to 33.1 inches); light gray (10YR 7/1); fragments; slight effervescence. Cedarville dolomite bedrock. Hard. The uppper 2 to 3 inches of the bedrock could be chipped out with a spade, but below this it was very hard. Not sampled.