In the north, on the edge of the tableland, they are most numerous. On the east coast, at the head of the Burdekin River, there are unmistakeable signs of an upward effort of the imprisoned waters to free themselves. One main tributary, a creek called Fletcher's Creek, takes its rise in a labyrinth of basaltic rocks, that for years defied the efforts of the whites to penetrate. This stream rising from its cradle in the dead lava, winds in and out of the encompassing stretches of rocks, until it emerges on the outer country, where it feeds and maintains two large lakes, ere it is lost in the sandy bed of one of the anabranches of the Burdekin. It is one of the strongest and most consistent outbreaks in the north, and its volume and continuance show the strength of the source from which it emerges. The head of the Burdekin itself is amongst lava beds, wherein there are many similar springs; most of these take the form of permanent lagoons. To the westward we find ourselves on a more arid surface, the formation of the ranges not being so favourable to the development of springs; and where they do occur, they are evidently the product of rainfall. On the watershed we are on a corner, as it were, of the inland plain, and our ascent has put us above the spring level. Lower down, if we follow the well-known Flinders River, we find in the hot springs at Mount Brown another upshoot from below that has evidently come from the neighbourhood of the internal fires themselves. From this point right away west, skirting the edge of the tableland, great rushes of water are comparatively common. Some find their way between basaltic columns, and after feeding the flow of some large river for many miles, die suddenly, leaving the lower part of the watercourse a barren, sandy channel. The heads of the Leichhardt and Gregory Rivers are particularly prolific in springs; the latter river, as I have already noticed, being one of the steadiest flowing rivers in Australia. Westward still, the heads of all the rivers, no matter what their lower course is like, abound in springs at the break of the descent from the tableland, and, as nearly as can be computed, all these occur at nearly about an identical altitude. To travel west, through to the western shore of Australia, only gives us the same phenomena: everywhere the belt of springs is to be found about half-way between the edge of the tableland and the coast level, just where the abrupt descent terminates and a gentler slope is entered on. It would be wearisome to enumerate them all, the fact of their existence is so well-known in these days.