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Giles, Ernest, 1835-1897

"Australia Twice Traversed, Illustrated,"

On the west side I found another running spring, with some much
larger rock-basins than at our camp. Of course the water ceased
running where the rock ended. Round on the north side I found a still
stronger spring, in a larger channel. I rode completely round the mass
of this wonderful feature; its extraordinary appearance will never be
out of my remembrance. It is no doubt of volcanic origin, belched out
of the bowels, and on to the surface, of the earth, by the sulphurous
upheavings of subterraneous and subaqueous fires, and cooled and
solidified into monstrous masses by the gelid currents of the deepmost
waves of the most ancient of former oceans. As I before remarked, it
is composed of mixed and rounded stones, formed into rounded shapes,
but some upon the eastern side are turreted, and some almost pillars,
except that their thickness is rather out of proportion to their
height. The highest point of the whole, as given before, is 1500 feet
above the ground, while it is 2800 feet above the sea-level. Could I
be buried at Mount Olga, I should certainly borrow Sir Christopher
Wren's epitaph, Circumspice si monumentum requiris. To the eastward
from here, as mentioned in my first expedition, and not very far off,
lay another strange and singular-looking mound, similar perhaps to
this.


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