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I ascended it at the opposite end, but although the view was extensive, I could not make out the little hill of granite from which I had taken my former bearings, and the only elevation I could recognise as connected with them, was one about ten miles distant, bearing S. 168 W. I could observe very distant ranges to the E.N.E. and immediately below me in that direction, there was a large clear plain, skirted by acacia pendula, stretching from S.S.E. to N.N.W. The crown and ridges of the hill on which I stood, were barren, stony, and covered with beef-wood, the rock-formation being a coarse granite.
At last they ran to two mubboo or beef-wood trees, and clung tightly to them. After them rushed the whirlwind, sweeping all before it, and when it reached the mubboo trees, to which the boys were clinging, it tore them from their roots and bore them upward swiftly, giving the boys no time to leave go, so they were borne upward clinging to the mubboo trees.
They seemed to be covered with cypresses and beef-wood, but dwarf-box and the acacia pendula prevailed along the plains; while flooded-gum alone occupied the lands in the immediate neighbourhood of the stream, which was evidently fast diminishing, both in volume and rapidity; its bed, however, still continuing to be a mixture of sand and clay.
On ascending the most westerly of the hills, we found it composed of micaceous schist, the upper coat of which was extremely soft, and broke with a slaty fracture, or crumbled into a sparkling dust beneath our feet. The summit of the hill was barren, and beef-wood alone grew on it.
To the westward, the decline of country was more observable than ever; and the hills on both sides of the river, were lower and more distant from it. Those upon which we found ourselves were composed of iron-stone, were precipitous towards the river in many places, of sandy soil, and were crowned with beef-wood as well as box.
I ascended it at the opposite end, but although the view was extensive, I could not make out the little hill of granite from which I had taken my former bearings, and the only elevation I could recognise as connected with them, was one about ten miles distant, bearing S. 168 W. I could observe very distant ranges to the E.N.E. and immediately below me in that direction, there was a large clear plain, skirted by acacia pendula, stretching from S.S.E. to N.N.W. The crown and ridges of the hill on which I stood, were barren, stony, and covered with beef-wood, the rock-formation being a coarse granite.
They seemed to be covered with cypresses and beef-wood, but dwarf-box and the acacia pendula prevailed along the plains; while flooded-gum alone occupied the lands in the immediate neighbourhood of the stream, which was evidently fast diminishing, both in volume and rapidity; its bed, however, still continuing to be a mixture of sand and clay.
To the westward, the decline of country was more observable than ever; and the hills on both sides of the river, were lower and more distant from it. Those upon which we found ourselves were composed of iron-stone, were precipitous towards the river in many places, of sandy soil, and were crowned with beef-wood as well as box.
On ascending the most westerly of the hills, we found it composed of micaceous schist, the upper coat of which was extremely soft, and broke with a slaty fracture, or crumbled into a sparkling dust beneath our feet. The summit of the hill was barren, and beef-wood alone grew on it.
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