Eastport quadrangle notebook # 5, 1908
Page 129
Image from the Biodiversity Heritage Library. Contributed by Smithsonian Institution Archives. | www.biodiversitylibrary.org
Transcription
Quadrille Ruled Form. John C. Moore Corporation, Rochester, N. Y. Binder and holes in leaves, each Patented 1906 Aug. 8, 1905 On the east side of Burnt Base 5-57-5 just south of Birmingham Nat. there occurs a cliff of rocks striking N. 22° W. dip 32° N.E. which may be the equivalent of the Wilson Stream zone at Drungville &. The rock is well bedded thick banded very fine grained, dense light siliceo-calcareous kind of a light gray & gray blue color showing in places a little undulated gray shale. Fossil are abundant in several seams one of the seams about 2 foot from the top of the fossil lime bed is an intermittent 0-3 well coral reef of Polyartes as at Drungville. The entire forms of these beds (which are 200 yards east of A) include 5-57-5- Chonetes cornutus (small) Leptostrophia ornatella (small in situ), Strophomena Dalmanella g edseliana D. (of Rhipidomella) sp. Stenoscisma of acrus Rhynchonella stricklandi Wilsonia wilsoni (common band) fura Spirifer elevatus Hyatella or Whitfieldella sp Cammysia cingulata (large) Pteronidella retroflexa Modiolopsis sp murelisoma ? Spirra ductata Natalis, Leuthim & corla. B 13 R. f. Com " " Rare Common Occasional