Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Friday September 2-1910 Belle Isle.
Last night arranged with a fisherman to
take me to Belle Isle this morning in his sail boat.
This morning the wind is again, as it has been so
often this summer, in the wrong direction and
therefore drove go via the railway to Helligew
and from here by steamer.
At Topsail station was told that the little
steamer intended to go regularly from Helligew to Belle
Isle but that it was found that the water is too
shallow here. Therefore the steamer now goes 2 to 3
times a day from Port Royal Cove which is nine miles
north of Topsail and the only way to go there is
to get a canoe or a walk. Or so today.
Visited Manuels Brook to study the contact
between the Lower and Middle Cambrian. This is
Daleth's gneiss "Calcareous sandstone with pindist
limestone in irregular masses, 2 foot" The contact with the
red shale of gneiss it appears to be perfectly conformable
so far as I can see but the contact is all crossed
by the brook. The calcareous sandstone may be termed
a nodular arenaceous limestone, present as a
rule with the lining goes tending to be pindist.