early vertical veins of white quartz, the surface of
which was in a crystallized state. The floor of the cavern was covered
with heaps of water-worn fragments of quartzose rock, containing copper
pyrites, in some of which the cavities were covered by a deposit of
greenish calcedony. The sides of the cavern had a stalagmitical
appearance but the recess was so dark that we could not ascertain either
its formation or extent; it did not however appear to be more than twelve
or fourteen yards deep. On first entering it we were nearly overpowered
by a strong sulphureous smell which was soon accounted for by the flight
of an incredible number of small bats which were roosting in the bottom
of the cave and had been disturbed by our approach. We attempted to grope
our way to the bottom, but, not having a light, were soon obliged to give
up its further examination.
The island is connected to the cape by a narrow ridge of rocks which the
spring-tides may probably cover. The main corresponds with the island in
character and general conformation, being extremely barren and rocky, and
of the same description of sandstone, the strata of which appear nearly
horizontal; the greatest deviation from that position not being more than
an inclination of 5 degrees to the south-east.
Upon our return we landed at Caper Point near the bottom of the bay;
where, on taking some bearings, a considerable local magnetic attraction
was detected, for the needle of the theodolite was nearly eight degrees
in error. Whilst I was thus employed Mr. Cunningham, who was my companion
upon this excursion, ranged about among the shrubs in the vicinity and
was fortunate in finding the fruit of a tree that was first seen by us at
Cambridge Gulf, and had for some time puzzled us from its immense size
and peculiar appearance. It proved to be a tree of the natural order
Capparides, and was thought to be a capparis; the gouty habit of the
stem, which was soft and spongy, gave it an appearance of disease: but as
all the specimens, from the youngest plant to the full-grown tree,
possessed the same deformed appearance, it was evidently the peculiarity
of its habit. The stem of the largest of these trees measured twenty-nine
feet in girth whilst its height did not exceed twenty-five feet. "It was
at this time in the earliest stages of foliation, the extremities of the
naked branches appearing green; and one bud that was opened exhibited the
character of Folium quinatum."
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