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{Introduction}{Physical Setting}{Methods}{Results}{Conclusions}{Future Study}{Aerial Photo}{Digital Elevation Map}
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A1: 0-17 cm; very
dark brown (10YR 2/2), moist; sandy loam; medium sub-rounded, 0.7
sphericity, poorly sorted, mostly quartz with feldspar and other
crystalline lithologies; very friable; medium granular structure;
slightly sticky; non-plastic; common medium roots; no HCl reaction;
abrupt smooth boundary.
A2: 17-32 cm; dark
brown (10YR 3/3) moist; sandy loam; medium sub-rounded, 0.7 sphericity,
poorly sorted, mostly quartz with feldspar and other crystalline
lithologies; very friable; medium granular structure; slightly sticky;
non-plastic; few medium roots; no HCl reaction; abrupt smooth boundary.
Bw: 32-35 cm; brown
(7.5 YR 4/4) moist; sandy loam; medium sub-angular to subrounded, 0.7
sphericity, poorly sorted, mostly quartz with feldspar and other
crystalline lithologies; medium, sub-rounded sand; weak sub-angular
blocky structure; non-sticky; non-plastic; no roots; no clasts; no HCl
reaction; abrupt smooth boundary.
C1: 35-51 cm; dark
brown (7.5 YR 3/4) moist; sub-rounded sand, 0.9 sphericity, well sorted,
mostly quartz with feldspar and
other crystalline lithologies; clasts:
2-5mm, 15%, subangular to subrounded, 0.9/0.7 sphericity, no
orientation, basalt,
granite, metamorphic lithology;
no HCl reaction; abrupt smooth boundary.
C2: 51-85.5 cm; dark
yellowish brown (10 YR 3/4) moist; medium sub-rounded sand, 0.7
sphericity, moderately to well sorted, mostly
quartz with feldspar and other crystalline lithologies;
clasts: 5-20mm diameter, 10%, 0.7/0.9 sphericity; no orientation, basalt,
granite, metamorphic lithology;
no HCl reaction; abrupt smooth boundary. |
C3:
85.5-91 cm; dark yellowish brown (10YR 4/4) moist; medium to
coarse sub-rounded sand, 0.7 sphericity, poorly sorted, mostly
quartz with feldspar and other crystalline lithologies; clasts:
20-40mm, 50%, 0.9/0.7 sphericity, horizontal orientation, basalt,
granite, metamorphic lithology;
no HCl reaction; abrupt smooth boundary.
C4: 91-122 cm; brown (7.5YR 4/4) moist; medium, sub-rounded sand,
0.7 sphericity, very well sorted, mostly quartz with feldspar and other
crystalline lithologies; clasts: 2-5mm, <1%, 0.7/0.9 sphericity, no
orientation, basalt, granite, metamorphic lithology; no HCl reaction;
abrupt smooth boundary. C5: 122-134 cm; brown (7.5 YR 4/3) moist; coarse, sub-rounded sand, 0.7 sphericity, very well sorted, mostly quartz with feldspar and other crystalline lithologies; clasts: 2-5mm, ≤1%, 0.7/0.7 sphericity, no orientation, basalt granite, metamorphic lithology; no HCl reaction; wavy, clear boundary.
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| Conclusion
Soil Pit #6 is located on the slope shoulder of the terrace located 8-10 meters from the Hartnett drive. The pit is located 2 meters from a tree line composed of Aspen and Prickly Ash. Vegetation surrounding pit 6 is comprised of mainly grassy forbs. Soils in this location are mapped as the Finchford Series in new soil map data (Meyer Personal Communication 2001), and as Hubbard Loamy Sand 6-12 percent slopes (HuC2), in the Dunn County Soil survey (ref). Our soil description generally is consistent with The Finchford Series, but there are some discrepancies. The Finchford Series has a plow zone within its first horizon ours did not. Because of these discrepancies, we think the Soil Profile of Pit #6 is most consistent with the Hubbard Loamy Sand (HuC2) Series as described in the Dunn County Soil Survey (ref). Similarities between soil characteristics we observed in the Pit #6 soil profile and the Hubbard Series description include: both have lost original surface material due to erosion, surface area is very dark brown, large A horizons (roughly32 cm in depth), the C horizon is roughly the same depth, and both descriptions have the same parent material (outwash plains and stream terraces). |