ards the east. High, rocky
and reddish cliffs have been seen indistinctly about latitude 27 degrees;
and a coast of the same aspect has been surveyed, from Red Point, about
latitude 28 degrees, for more than eighty miles to the south-west. The
hills called Moresby's flat-topped Range, of which Mount Fairfax,
latitude 28 degrees 45 minutes, is the highest point, occupy a space of
more than fifty miles from north to south.

Rottnest Island and its vicinity, latitude 32 degrees, contains in
abundance the calcareous concretions already mentioned; which seem there
to consist in a great measure of the remains of recent shells, in
considerable variety. The islands of this part of the shore have been
described by MM. Peron and Freycinet;* and the coast to the south, down
to Cape Leeuwin, the south-western extremity of New Holland, having been
sufficiently examined by the French voyagers, was not surveyed by Captain
King.

(*Footnote. Peron volume 2 page 168 etc.)

Swan River (Riviere des Cygnes) upon this part of the coast, latitude 31
degrees 25 minutes to 32 degrees, was examined by the French expedition,
to the distance of about twenty leagues from its mouth; and found still
to contain salt water. The rock in its neighbourhood consisted altogether
of sandy and calcareous incrustations, in horizontal beds, enclosing, it
is stated, shells, and the roots and even trunks of trees. Between this
river and Cape Peron, a "great bay" was left unexplored.*

(*Footnote. Peron volume 1 page 179. Freycinet page 5. 170.)

The prominent mass of land, which stands out from the main, between Cape
Naturaliste and Cape Leeuwin, and runs nearly on the meridian for more
than fifty miles, seems to have a base of granite, which, at Cape
Naturaliste, is said to be stratified.* The same rock also occurs, among
Captain King's specimens, from Bald-head in King George's Sound; but
nearly on the summit of that hill, which is about five hundred feet high,
were Found the ramified calcareous concretions, erroneously considered as
corals by Vancouver and others;** but which appear, from Captain King's
specimens, to be nothing more than a variety of the recent limestone so
abundant throughout these shores.

(*Footnote. Peron volume 1 page 69.)

(**Footnote. Vancouver 1 49. D'Entrecasteaux 2 175. Freycinet 105.
Flinders 1 63. See the detailed descriptions hereafter; and Captain
King's Narrative volume 1.)

The south coast, and the southern portion of