Field Notebook: Maryland, New Jersey, Tennessee, Virginia, West Virginia, Indiana, Ohio, New York, Ontario 1907
Page 120
Image from the Biodiversity Heritage Library. Contributed by Yale Peabody Museum of Natural History. | www.biodiversitylibrary.org
Transcription
-14 Wednesday August 13 Tuesday, Canton, O. Paed the Sandusky Passes and shipped by Express. Left on the B. & O. R. R. for Carth at 11 A.M. to see brother this. Met him well at home with one of his regular bone attacks. Still had a good talk with him. Remained at his home until the next day at 11:30. Returned on the 11.45 B. & O. t. Cleveland, Left the latter place at 2 P.M. and arrived at Niagara Falls at about 9 P.M. Eastern Time. Stopping at Imperial Hotel. August 15 Thursday. Lewiston. Started out along the Central Lines in the hand down the gorge to Lewiston. The Lockford dolomites consist of series of thin and heavy bedded dolomites in which measure the fossil curules (mawigures?) the joint curules and once a len piler with calcite. Otherwise along the bedding planes one sees crinoidal material. The pink heeme [illegible] demand turns the Rochester shale. Towards the base the bearing bed shows a distinct cross bedding - the bottomy shell's water- while higher up the thick beds look more like water limestone but are not