[[pencil drawing of strata of coal seam]]

Vaccinium sp., arborvitae,  a fern? and some others unknown to me, laurel? & 
shagberry. &c.
The coal is nowhere more than 18 inches thick in the clear - it contains a good deal of sulphur & iron & splits very easily into thin sheets. The roof stone is unstable. All the strata dip to the westward from 5� to 20� There are not many
folds but a few waves  The conglomerate appears to have been a leach formation while the level was changing as many of the upper lie unconformably on each other
Above all are marine tertiary which I have not