Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Collection 2-6A - 33' up, Coll. 2-6B - 85' up------- 112'
7) Limestone, light gray-3' to 6' beds, few and thin shale interbeds. Coll. 2-7 --
------------------- 32'
8) Limestone, light orange-brown weathering, very fine frag.;
3' to 5' thick separated by 2-7' shaly intervals. The limestone have a "Staffella"
fauna, and locally scattered "fusulinids" --- 90'.
Cyclothems—10 to 12 - get progressively more shaly toward top of unit.
9) Limestone, orange-brown weathering, 1' to 4' beds. Omphalathrocus type gastropods.
PG. 3
7/9/59
near base - fusulinids recrystallized
Collection 2-9A - 42' up (Top of ridge 140')
Collection 2-9B - 145' up
Limestones become progressively more silty and change to light gray weathering.
Collection 2-9C - 160' up
Collection 2-9D - 185' up; total -------- 215'
10) Limestone and dolostone, orange-brown weathering - very silty - 2" to 6"
beds - shale interbeds up to 1'.
Collection 2-10A - at 5',
Saddle at 80'
Collection 2-10B - 105' up
Rose colored dolo 3' separated by 4' of orange weathering silt-clay stem. Cyclic beds become.
{note: illustration:
bed 2: silty limestone (+-)
bed 3: silt-sand, silt-clay
bed 4: dolo pink to orange}
PG. 4
fusulinids are rare - recrystallized when found. Gastropods - brachiopods and ostracods, locally abundant. - 187'.
11) Shale, light gray, and limestone, light gray - shale - 2-5' beds. Limestone - 1/2 to 1' beds.
Collection 2-11A - 5' up.
at 35-50' Ophalotrocus outlines common
limestone is porous and recrystallized). - 89'.
12) Limestone, conglomerate, well sorted - 25'.