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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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