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It lies just two hours or five miles north-west of the Ungerengeri crossing. The ground is rocky, composed principally of quartzose detritus swept down by the constant streams.

This little point settled, off started Kachuchu in his usual merry manner, whilst I took a look at the hills, to see their geological formation, and found them much as before, based on streaky clay sandstones, with the slight addition of pure blue shales, and above sections of quartzose sandstone lying in flags, as well as other metamorphic and igneous rocks scattered about.

If we take a handful of quartzose sand, mixed with mica, and throw it into a clear running stream, we see the materials immediately sorted by the water, the grains of quartz falling almost directly to the bottom, while the plates of mica take a much longer time to reach the bottom, and are carried farther down the stream.

About a sixth part of the whole mass is composed of carbonate of lime, and there is usually an intermixture of fine quartzose and micaceous sand. Although this loam of the Rhine is unsolidified, it usually terminates where it has been undermined by running water in a vertical cliff, from the face of which shells of terrestrial, fresh-water and amphibious mollusks project in relief.

My hosts were forming a pepper and gambir plantation, and in the immediate neighbourhood were extensive tin-washings, employing over a thousand Chinese. The tin is obtained in the form of black grains from beds of quartzose sand, and is melted into ingots in rude clay furnaces.

A series of worm-holes traced erratic hieroglyphics across a scaling corner; all the varied texts were illuminated by quartzose particles glittering in the sun, and here and there fine green grains of glauconite. He knew no names like these, and naught of meteorological potency. He had studied no other rock. His casual notice had been arrested nowhere by similar signs.

I soon came to undulating ground or low hills of quartzose gravel without any grass, consisting of unabraded small angular fragments of quartz. I observed a few trees of the ironbark eucalyptus and pines or callitris on the highest grounds.

It is not the object of the present work to give a description of these operations, repeated as they are, year after year, and century after century; but I may suggest an explanation of the manner in which some micaceous sandstones have originated, namely, those in which we see innumerable thin layers of mica dividing layers of fine quartzose sand.

Whatever rises above the surface of the water is composed of broken pieces, cemented by carbonate of lime, in which grains of quartzose sand are set. Whether rocks formed by polypi still living are found at great depth below this fragmentary rock of coral or whether these polypi are raised on the Jura formation are questions which I am unable to answer.

It is the "boiling" type of spring, and the water, which is stone-cold, bubbles up through white quartzose sand at the foot of a low granite ledge. It flows throughout the year at the rate of about eight gallons a minute.