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SECTION 8232 Hill South of Morales I 370 m E., 1210 m N. of SW Corner, Sec. 1, T. 20 N., R. 35 E., Garfield County, Montana. Elevation = 8231 m 236° A2 - 0° dip from initiation of Morales I section. Distance + 30 paces to Morales I. Elevation of base of unit (m) Unit Thickness (m) Tullock Formation: Siltstone, Mudstone: in alternating yellow and orange interbeds, mudstone with limonitic concre- tionary ledges, typical of Lower Tullock. 4.2 4.05 Shale: fissile, carbonaceous .15 Sandstone: fine-grained, clayey, laminated, subangular, brown-grey, with carbon on laminae, with limonitic yellow weathered patches in lower half. Becoming more and more silty above 3.6 m. 2.6 1.45 Inferred channel filling unit of carbonaceous shales, mudstones, and rare sandstone. Siltstone: fissile, dark brown grey, 2.42 becoming a shale upward. Shale: fissile, dark grey, with shells above 2.05. 1.7 1.51 Mudstone: fissile, dark brown grey. Siltstone: fissile, dark brownish to yellowish grey, with plant fragments. 1.15 Shale: fissile, dark brown grey, becoming a fissile mudstone upward. Weathers rusty yellow above 0.6 and with a 0.01 in clay- ironstone concretion layer at basal contact. Sandstone: fine to medium grained, massive, dirty brown, rusty at top. 0.25 0.08 shell bed. -0.02 Shale: fissile, brownish black, carbonaceous, with plant fragments. Basal 3 cm with lignite splits, but not a lignite. -0.27 2.87 Hell Creek Formation: Mudstone: massive, olive drab, with rare plant fragments, as Unit 1 of 8231. -0.3 .03 Base of Section
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SECTION 8210 Section runs from base of Mantua lentil through lignitic base of Fort Union Formation and uppermost Lance Formation. Polecat Bench N. Side 180 m NW of Mantua Quarry, center e. line, NW, NE, SW ¼ sec 31, T7N, R98W, Park County, Wyoming. Old locality 7839. Garland 7½' Quad. Pollen and Iridium sampling at even 10 cm intervals. Sampling with steel tools. Dug 2 trenches about 1 foot apart through weathered zone. No wedding rings. Final digging done with a ceramic spatula. Section starts about 1.8 m below the base of a lignite marking the bottom of the Fort Union Formation and ends in a sandstone bed of the Mantua lentil of the Fort Union Formation. UNIT Elevation at Base Thickness (m) Fort Union Formation: 2.6 Top of section as measured in Mantua lentil. Mantua Lentil: sandstone: very fine grained, subangular, dirty, cross-bedded, ledge-forming, color 5Y 7/2, lower contact irregular. Base of Mantua lentil. 2.52 .08 2.5 Shale: thin, lignitic just below contact Mudstone: Parallel bedded, 5Y 6/1, with stringers of lignite. Interbedded segment of thin wavy lignite stringers and 1 to 4 cm beds of mudstone. 2.01 .49 1.92 Lignite .09 1.86 Clay interbed 5Y 6/1 .06 1.79 Lignite: Marks base of Fort Union Formation .07 Lance Formation: Underclay, 5Y 6/1, with roots, comminuted plant matter and contorted carbonaceous laminae. 1.7 - 1.79 above base. Underclay 5Y 6/1, with limonite stains on joints, and root impressions. 1.62 .17 Mudstone: with gypsum on joints. Stringers of coal 1-2 mm thick above 1.56. 1.42 .2
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SECTION 8211 Road to Dumbell Hill at top of escarpment just where road comes off Polecat Bench. 1130 m east of SW Corner, 340 m north of SE Corner of sec 31 T 57N, R98W, Park County, Wyoming. Deaver Reservoir 7½' Quad. UNIT Fort Union Formation: Thickness 5.2 Top of Section Mantua lentil: sandstone; as in Sec. 8210 at 2.52 m, representing the lateral extension of the Mantua lentil. Unit is calcareously cemented and ledge forming with a 0.4 m interbed of carbonaceous shale lying 1 m above its basal contact. 3.04 2.16 Shale: carbonaceous, 5YR 4/1 with limonite staining and plant fragments, becomes papery above 2.68. 2.95 siltstone, cross-laminated, with vertical roots, otherwise as below. 2.87 shale: becomes platey with plant fragments 2.83 shale: gypsiferous, 5GY 6/1 2.46 2.74 shale: chippy, silty, with poor leaf fragments. 1.06 2.42 Siltstone: about 2.5 cm thick .04 2.23 Clay: massive, 10YR 6/2, with vertical and horizontal roots. .19 2.15 Lignite: blocky, black, top 1 cm brown and gypsiferous. Basal contact of Fort Union Formation. .08 Lance Formation: 2.11 Clay: massive, carbonaceous, 10YR 5/2 .04 2.10 Lignite stringer .01 Clay: carbonaceous, 5Y 3/2, slickensided, limonite stained, with root impressions. Interpreted as an underclay of lignite at 2.10. 1.8 1.99 - 1.95 Band of unctuous dark grey (5Y 2/2) clay. .11 Mudstone: fissile, 5Y 6/2 with root casts, carbonaceous material, and limonite joint stains. Plant fragments and roots more common upward. 1.25 1.45 mudstone: chippy .74
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SECTION 8210 Section runs from base of Mantua lentil through lignitic base of Fort Union Formation and uppermost Lance Formation. Polecat Bench N. Side 180 m NW of Mantua Quarry, center e. line, NW, NE, SW ¼ sec 31, T7N, R98W, Park County, Wyoming. Old locality 7839. Garland 7½' Quad. Pollen and Iridium sampling at even 10 cm intervals. Sampling with steel tools. Dug 2 trenches about 1 foot apart through weathered zone. No wedding rings. Final digging done with a ceramic spatula. Section starts about 1.8 m below the base of a lignite marking the bottom of the Fort Union Formation and ends in a sandstone bed of the Mantua lentil of the Fort Union Formation. UNIT Elevation at Base Fort Union Formation: 2.6 Top of section as measured in Mantua lentil. Mantua Lentil: sandstone: very fine grained, subangular, dirty, cross-bedded, ledge-forming, color 5Y 7/2, lower contact irregular. Base of Mantua lentil. 2.52 .08 2.5 Shale: thin, lignitic just below contact Mudstone: Parallel bedded, 5Y 6/1, with stringers of lignite. Interbedded segment of thin wavy lignite stringers and 1 to 4 cm beds of mudstone. 2.01 .49 1.92 Lignite .09 1.86 Clay interbed 5Y 6/1 .06 1.79 Lignite: Marks base of Fort Union Formation .07 Lance Formation: Underclay, 5Y 6/1, with roots, comminuted plant matter and contorted carbonaceous laminae. 1.7 - 1.79 above base. Underclay 5Y 6/1, with limonite stains on joints, and root impressions. 1.62 .17 Mudstone: with gypsum on joints. Stringers of coal 1-2 mm thick above 1.56. 1.42 .2
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SECTION 8211 Road to Dumbell Hill at top of escarpment just where road comes off Polecat Bench. 1130 m east of SW Corner, 340 m north of SE Corner of sec 31 T 57N, R98W, Park County, Wyoming. Deaver Reservoir 7½' Quad. UNIT Fort Union Formation: Thickness 5.2 Top of Section Mantua lentil: sandstone; as in Sec. 8210 at 2.52 m, representing the lateral extension of the Mantua lentil. Unit is calcareously cemented and ledge forming with a 0.4 m interbed of carbonaceous shale lying 1 m above its basal contact. 3.04 2.16 Shale: carbonaceous, 5YR 4/1 with limonite staining and plant fragments, becomes papery above 2.68. 2.95 siltstone, cross-laminated, with vertical roots, otherwise as below. 2.87 shale: becomes platey with plant fragments 2.83 shale: gypsiferous, 5GY 6/1 2.46 1.06 2.74 shale: chippy, silty, with poor leaf fragments. 2.42 Siltstone: about 2.5 cm thick .04 2.23 Clay: massive, 10YR 6/2, with vertical and horizontal roots. .19 2.15 Lignite: blocky, black, top 1 cm brown and gypsiferous. Basal contact of Fort Union Formation. .08 Lance Formation: 2.11 Clay: massive, carbonaceous, 10YR 5/2 .04 2.10 Lignite stringer .01 Clay: carbonaceous, 5Y 3/2, slickensided, limonite stained, with root impressions. Interpreted as an underclay of lignite at 2.10. 1.8 1.99 - 1.95 Band of unctuous dark grey (5Y 2/2) clay. .11 Mudstone: fissile, 5Y 6/2 with root casts, carbonaceous material, and limonite joint stains. Plant fragments and roots more common upward. 1.25 1.45 mudstone: chippy .74