Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
At 9.30 we saw quite a large village,
Bliss Bay: in the last hour we saw two
vessels, one a steamer the other schooner. The
large four story colliery building near the town
is in synclinal only the strata dipping from the
north and south towards it.
At 12.30 P.M. we arrive at the colliery area
we are to take our coal for the return trip, Kelly's Cove
Cape Breton. The ship anchors within thirty feet of
the shore. Soon after our arrival the throwing out
of the talast begins to make oars for the coal. At
three P.M. Mr. White and I go ashore to examine
the coal mine.
When the Hike anchors there is a mountain
of granite at least 1000 feet high. At a much lower
level against the granite rests a very small altered
dolomite followed by a sandstone shale with coals.
These strata have a gentle dip away from the
granite nucleus but towards it they become more
and more tilted until near the granite they are
vertical. A peculiarity of the dolomite is that
it has been partially weathered out where it joins
the granite leaving a deep and narrow gorge.
We collected a piece of the granite, dolomite