It was my object in the last chapter, to confine my observations strictly to the agricultural and pastoral capabilities of the province of South Australia, which I thought I could not better do than by describing the nature of its climate and soil, for on these depend the producing powers of every country.  In speaking of the climate, however, I merely adverted to its temperature, leaving its seasons out of question for the time, intending to close my remarks on these heads, by a short review of the state of the agricultural and pastoral interests of the colony at the present date.

It will be borne in mind that the seasons of Australia are the reverse of our own; that when in England the ground is covered with snow, there the sun is hottest, and that when summer heats are ripening our fruits, in Australia it is the coldest season of the year, December, January, February, and March being the summer months; June, July, August, and September the winter ones.  An experience of ten years has shewn that the seasons of South Australia are exceedingly regular, that the rains set in within a few days of the same period each successive year, and that during the winter the ground gets abundantly saturated.  This regularity of season may be attributed to the almost insular position of the promontory of Cape Jarvis, and may be said to be almost local, in elucidation of which, I may refer to what I have stated in the former part of my work, of the state of the weather in the valley of the Murray when the expedition was proceeding up its banks in the month of August, 1844.  For some time before there had been heavy rains in the hills, and it was with some difficulty the drays crossed them.  During our stay at Moorundi, the ranges were covered with heavy clouds, and the mountain streams were so swollen as to stop one of my messengers; but the sky over the valley of the Murray was as clear as crystal, morning mists it is true curled up at early dawn from the bosom of its waters, but they were soon dissipated, and a sharp frosty night was succeeded by a day of surpassing beauty.

The regularity, however, both in its commencement and in the quantity of moisture that falls during the rainy season in the colony, enables the agriculturist to calculate with certainty upon it, and the only anxiety of the farmer is to get his grain into the ground sufficiently early, if possible, to escape the first hot winds.  In a region, portions of which are subject, it must be confessed, to long continued drought, this is no inconsiderable advantage, although South Australia is not singular in this respect, for the rainy seasons in the Port Phillip districts are, I believe, equally regular and more abundant, whilst the climate of Van Diemen’s Land almost approaches to that of England; neither, indeed, fairly speaking, is South Australia more favoured than those of her immediate neighbours in the quality of her soil.  Van Diemen’s Land is the granary of the southern seas, and there