If we strike a line to the N.W. from Sydney to Wellington Valley, we shall find that little change takes place in the geological features of the country.

On the subject of emigration, it is not my intention to dwell at any length.

Australia is properly speaking an island, but it is so much larger than every other island on the face of the globe, that it is classed as a continent in order to convey to the mind a just idea of its magnitude.

In a colony constituted like that of New South Wales, the proportion of crime must of course be great.

The increasing importance of Sydney must in some measure be attributed to the flourishing condition of the colony itself, to the industry of its farmers, to the successful enterprise of its merchants, and to particular local causes.

Mount Harris is of basaltic formation, but I could not observe any columnar regularity in it, although large blocks are exposed above the ground. The rock is extremely hard and sonorous.

Yet, upon the whole, the space I traversed is unlikely to become the haunt of civilized man, or will only become so in isolated spots, as a chain of connection to a more fertile country; if such a country exist to the westward.