THE AREA AND CLIMATE OF AUSTRALIA

Australia is a continent not only in name but in fact. Its area,

including Tasmania, is almost 3,000,000 square miles, which is about

the area of the United States exclusive of Alaska, and only about one

fourth less than the area of the continent of Europe. Fully two fifths

of this area lie within the torrid zone, and of the rest, even in

Victoria, the part farthest from the equator, the climate is so warm

that it corresponds with that of Spain, southern France, and Italy.

But over so vast a territory great differences of climate must occur,

and consequently of products also. A general description of the

climate and products of Australia is therefore impossible. Yet there

are several characteristics which appertain to the whole continent.

The chief of these are (1) the great DRYNESS of the ATMOSPHERE--not

merely its lack of rain, but its absolute freedom from moisture; (2)

the remarkable INEQUALITY, or want of regularity, in the RAINFALL.

Occasionally the rainfall is excessive, but a more frequent and

serious cause of trouble is excessive drought. The continent on every

side has a low coast region, where the rainfall is heavier and the

temperature generally hotter than in the corresponding table-land

interior to it. But the vast table-land of the interior has

comparatively little rain, and indeed in some parts of it, especially

in the centre and west, the rainfall is so slight that the country is

practically a desert.

But even when all the desert areas of Australia are excluded from

calculation there still remains in the interior plateau, toward the

east and south, an immense area of country of great fertility and

productiveness. The Murray River alone drains an area of 500,000

square miles, one sixth of the whole continent, a great part of which

is of exceeding richness. In these fertile parts irrigation by

artesian wells has been tried, and always with great success. And it

is thought that almost the whole continent can be regained for

agriculture, or at least for sheep-pasturing, by similar means; for

even in the arid and so-called desert parts of the interior, there is

very little soil that is not really fertile, for all of it is covered

with thick brushwood. Moisture alone is needed to make it bear crops

abundantly. And this dryness of the atmosphere which prevails

throughout the whole continent is not without its compensations. It

renders the climate exceedingly healthful.

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