17
This coal, which in the deepest part is about seven or eight feet thick, rises pretty rapidly in every direction from that point, and as it rises it thins out to about two feet. It thus forms a small basin, not half a mile across, and its outcrop is everywhere covered by beds of loose sand. A little beyond its outcrop on the seashore was the following section:—
| Yards. | |
| Trap (in small prismatic pieces) | 7 |
| Sandstone, formed of grains of some trap rock | 18 |
| Sandstone, soft and rather shaly | 6 |
| Shale and bind | 2 |
| Coal | 0½ |
Near this spot they had bored to a farther depth of nearly 100 yards and passed through one twenty-inch coal; but the rest of the mass was almost entirely sandstone. I got from these coal-measures fossil plants, among which were Pecopteris Australis, a Sphenopteris and a Zeugophyllites.
There are other places in Tasmania where coal is worked, but they are chiefly detached and isolated spots separated by greenstone ridges one from the other. I was not able to visit any other of these localities, but I should fear that the beds of coal in Tasmania are comparatively insignificant in an economic point of view, that the true coal-measures of the country have no great thickness, and that the seams of coal contained in them are but partial, thickening and thinning out perhaps along the same horizontal lines, and thus forming limited cakes rather than regular and persistent beds.
C. East Coast of Tasmania.
Rocks of the palæozoic formation, chiefly sandstones, are found at various point of the eastern coast, but greatly broken and obscured by the usual greenstone ranges and local exhibitions of other trap rocks. In Maria Island are limestone quarries which I did not visit, but from which I procured fossils, among which were some of the large Pachydomi, of precisely the same species as those from Wollongong in New South Wales.
At Spring Vale, about ten miles above Great Swan Port, is a
