Field Notebook: Oklahoma 1919
Page 56
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Transcription
Hale gme Ferruginous sandstone Blue limestone 115 fat 15 - 5- 10 " This Supannella limestone reminds me much of the "Supanella li." seen in the Cuttles. We then went several miles farther north to Limestone Gap (See. 31 T. 2 N., R. 13, E.) where the M.R. and T. has cut through Limestone Ridge, descending Here Belli gives the following section Limestone 6" fat Orlite 3. Chert ( I should say a dense hard li) [illegible] only 30 - Blue shale 200 " A series of argillaceous - sandy, li. hue separated by gins of dark blue shales.} 97 " Here we find some fossils and free parts of goniatites. The latter attain to 12 inches in diameter. They are nuptile with some twells, like the slab taken from the Chockie quarin, and others like Taormino. This in the Cuttles zone is clearly the one seen north of Berryg [illegible] and in some ways the fossils remind me of the Smiths li. of the Bend series. If this is true then the base