The Mirror of Literature, Amusement, and Instruction - Volume 13, No. 369, May 9, 1829 by Various
page 30 of 50 (60%)
page 30 of 50 (60%)
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the caverns formed in the minacious schistose between the granite
and the limestone, as something very extraordinary. They contained rock-salt in large quantities, forming thick incrustations on every part of the surface, beautifully crystallized, and penetrating into the most compact parts of the rock. In many of these caverns were very brilliant stalactites and stalagmites of extraordinary size adhering to the nodules of granite which form their bases or floors, and which are from forty to fifty feet above the level of the sea. In several parts of the limestone formation, mineral springs were found; one in particular was noticed within half a mile of the entrance into Swan River. It bubbled out at the base of the solid rock in a stream, whose transverse area was measured by Captain Stirling, and found to be from six to seven feet, running at the rate of three feet in a second of time. It was thermal, saline, pleasant to the taste, and some, who partook of it, attributed to it an aperient quality. Such is the outline of a country on which the government have determined to establish a colony, and over which they have justly, and we think judiciously, appointed Captain Stirling to act as lieutenant-governor. The plan on which it is to be founded is, in our opinion, unobjectionable. It promises the most advantageous terms to qualified settlers, and deserves only to be known to ensure as many of the most respectable agriculturists as may in the first instance be desirable. In point of climate, this colony and New South Wales may perhaps be equally salubrious, though we are disposed to think that the western aspect and the sea-breezes may preponderate in favor of the new |
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