[Narrative of a Survey of the Intertropical and Western Coasts of Australia] [Volume 2 of 2] by Phillip Parker King]@TWC D-Link bookNarrative of a Survey of the Intertropical and Western Coasts of Australia] [Volume 2 of 2] CHAPTER 5 507/583
The heights from thence towards the north decline gradually, as the mountainous ranges approach the shore, which they join at Cape Weymouth, about latitude 12 degrees; and from that point northward, to Cape York, the land in general is comparatively low, nor do any detached points of considerable elevation appear there.
But about midway between Cape Grenville and Cape York, on the mainland south-west of Cairncross Island, a flat summit called Pudding-Pan Hill is conspicuous; and its shape, which differs from that of the hills on the east coast in general, remarkably resembles that of the mountains of the north and west coasts, to which names expressing their form have been applied.* (*Footnote.
Jane's Table-Land, south-east of Princess Charlotte's Bay (about latitude 14 degrees 30 minutes) and Mount Adolphus, in one of the islands (about latitude 10 degrees 40 minutes) off Cape York, have also flat summits.
King manuscripts.) The line of the coast above described retires at a point which corresponds with the decline of its level; and immediately on the north of Cape Melville is thrown back to the west; so that the high land about that Cape stands out like a shoulder, more than forty miles beyond the coastline between Princess Charlotte's Bay and the north-eastern point of Australia. The land near Cape York is not more than four or five hundred feet high, and the islands off that point are nearly of the same elevation. The bottom of several of the bays, on the eastern coast, not having been explored, it is still probable that rivers, or considerable mountain streams, may exist there. Along this eastern line of shore, granite has been found throughout a space of nearly five hundred miles; at Cape Cleveland; Cape Grafton; Endeavour River; Lizard Island; and at Clack's Island, on the north-west of the rocky mass which forms Cape Melville.
And rocks of the trap formation have been obtained in three detached points among the islands off the shore; in the Percy Isles, about latitude 21 degrees 40 minutes; Sunday Island, north of Cape Grenville, about latitude 12 degrees; and in Good's Island, on the north-west of Cape York, latitude 10 degrees 34 minutes. The Gulf of Carpentaria having been fully examined by Captain Flinders, was not visited by Captain King; but the following account has been deduced from the voyage and charts of the former, combined with the specimens collected by Mr.Brown, who has also favoured me with an extract from the notes taken by himself on that part of the coast. The land, on the east and south of the Gulf of Carpentaria, is so low, that for a space of nearly six hundred miles--from Endeavour Strait to a range of hills on the mainland, west of Wellesley Islands, at the bottom of the gulf--no part of the coast is higher than a ship's masthead.* Some of the land in Wellesley islands is higher than the main; but the largest island is, probably, not more than one hundred and fifty feet in height;** and low-wooded hills occur on the mainland, from thence to Sir Edward Pellew's group.
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