The History of Australian Exploration from 1788 to 1888Favenc, Ernest
History
The History of Australian Exploration from 1788 to 1888
Favenc, Ernest
Australia -- Discovery and exploration
When one comes to know the real value of water in a thirsty land, it
almost seems like a crime on the part of Nature, that a spring should
rise and flow for a comparatively short distance, to be lost in the sea.
When by placing the source some fifteen or twenty miles away the course
would run for hundreds of miles through a dry country. Can human
ingenuity improve on nature?
In this case nature seems to have laid the ground work of a great
comprehensive continental plain; to have put the lever ready for man to
start it, and though the scheme is one of such magnitude that it may at
first glance seem widely impossible, there is no reason, backed as it
would be by natural forces, that it may not be an accomplishment of the
future.
To fully understand the great problem of the water supply of Australia,
it is necessary to comprehend and carry in mind the wonderfully unique
river system of the continent. In an average area of 1,800 miles east and
west, by 900 miles north and south, the whole drainage runs from north to
south; that is to say, all that finds vent in the ocean. This, of
course, is the surface formation carrying off the rainfall, and has no
bearing on the outbreak of subterranean springs. But, as showing the
upheaval of the land to the northward, it points out that naturally the
flow of irrigation on a large scale will be from north to south.
It may be said that from the 18th parallel there is a steady slope
southward, broken only by the subordinate natural features of the
country, which necessarily form the irregularities of the smaller
tributaries. In this great block of more than a million and a quarter of
square miles there are then all the defined channels requisite for the
carriage of water throughout the heart of the continent, but with the
important fact wanting that they are destitute of a constant and steady
supply from the doubtful rainfall. The tilt of the northern edge of the
plateau puts their sources above the level of the great springs, and
causes them to be dependent on these intermittent and often scanty rains.
And we know that these rains have failed in producing any comprehendable
system of drainage over one third of our continent, at, least, at present
with our limited knowledge, the water system appears wasteful and
purposeless throughout that region.
If then the underground sea that exists beneath could be, tapped as far
north as possible, the water would rise to the surface at a much higher
level, than would be possible elsewhere, and much greater use could be
made of it, inasmuch as a larger area would lay below it for
fertilization. Now, the question of the existence of this water supply at
a uniform depth beneath the earth's surface can be proved by noting the
existence of the springs that we know of, that have found their way
without artificial aid to the light of day. Only those can be brought in
evidence that are unmistakeably outside of local influence, and are
unaffected by wet weather, or dry.
Public-domain text, read in full here on John Shaqi.
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