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