Journal Of An Overland Expedition In Australia, By Ludwig Leichhardt




















































































































 -  The
difference between the sandstone country and the basaltic plains and
ridges, is very striking in respect to the quantity - Page 137
Journal Of An Overland Expedition In Australia, By Ludwig Leichhardt - Page 137 of 524 - First - Home

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The Difference Between The Sandstone Country And The Basaltic Plains And Ridges, Is Very Striking In Respect To The Quantity Of Water They Contain:

In the latter, rain is immediately absorbed by the cracked porous soil, which requires an immense quantity of moisture

Before it allows any drainage; whereas the sandstone forms steeper slopes, and does not absorb the rain so quickly, so that the water runs down the slopes, and collects in holes at the foot of the hills parallel to the creeks. Scrubs are frequent round the low rises of sandstone; and, where the country is level, and the soil loamy, the hollows are often filled with water by the thunder-storms. The moist character of this description of country is probably the cause of the vegetation being more dense than it is in the rich black soil of the plains; in which latter, the seeds of the grasses and herbs lie dormant, until the first rain falls, when they instantly germinate and cover the plain with their rapid and luxuriant growth, as if by enchantment; but which, from its nature, is incapable of maintaining the growth of scrubs and trees.

Feb. 3. - The dew was heavy through the night; and, in the morning, loose rainy clouds gathered from the east and north-east, which, however, disappeared about eleven o'clock. Charley went back to the camp, to bring it on, and I continued to reconnoitre to the north-west. After passing a sandstone ridge, I came to a creek, which went to the north-west, and which was supplied with water by the late thunder-showers.

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