Journals Of Two Expeditions Into The Interior Of New South Wales, 1817-18 - By John Oxley











































































 -  I consider that the river may have from eight to
ten feet more water in it than usual: its present - Page 32
Journals Of Two Expeditions Into The Interior Of New South Wales, 1817-18 - By John Oxley - Page 32 of 354 - First - Home

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I Consider That The River May Have From Eight To Ten Feet More Water In It Than Usual:

Its present average depth is about eighteen feet.

The soil of these extensive plains, designated Field's Plains, is for the most part extremely rich, as indeed might be expected, from the deposition of the quantities of vegetable matter that must take place in periods of flood. The plains are in some places even lower than the ground forming the immediate bank of the river, very soft, and difficult for loaded horses to pass over. If we had been so unfortunate as to have had a rainy season, it would have been utterly impossible to have come thus far by land. The ranges of hills are unconnected, and are rocky and barren; the swamps for the most part surrounding them. Mount Cunningham is a lofty rocky hill, about a mile and a half long, composed of granite rock, but entirely surrounded by low swampy ground.

Here we were so unfortunate as to find the barometer broken, the horse which carried the instruments having thrown his load in passing the swamps: every precaution had been taken in the packing to prevent such an accident, which was the more to be regretted, as it interrupted a chain of observations by which I hoped to ascertain the height of the country with tolerable accuracy. The last observations that were made, reduced to this place, gave us an elevation of not more than five hundred feet above the sea, or about a hundred feet lower than the country at the depot.

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