In currying leather for shoes the leather is first soaked in water until it is thoroughly wet; then the flesh side is shaved to a proper surface with a knife of peculiar construction, rectangular in form with two handles and a double edge. The leather is then thrown into the water again, scoured upon a stone till the white substance called “bloom” is forced out, then rubbed with a greasy substance and hung up to dry. When thoroughly dry it is grained with a toothed instrument on the flesh side and bruised on the grain or hair side for the purpose of softening the leather. A further process of paring and graining makes it ready for waxing or coloring, in which oil and lampblack are used on the flesh side. It is then sized, dried and tallowed. In the process the leather is made smooth, lustrous, supple and waterproof.
What is a “Glass Snake”?
“Glass snake” is the name which has been given to a lizard resembling a serpent in form and reaching a length of three feet.
The joints of the tail are not connected by caudal muscles, hence it is extremely brittle, and one or more of the joints break off when the animal is even slightly irritated.
The Story in Diamond-Cutting[71]
Diamonds were known and worn as jewels (in the rough) in India 5,000 years ago and used as cutters and gravers 3,000 years ago. India was the source of supply until diamonds were discovered in Brazil about the year 1700, when Brazil became the largest producer and remained so until diamonds were found in South Africa about 1869. The African mines now produce four-fifths of the diamond supply. Previous to the discoveries in Africa, diamonds were known to originally come only from high places in the mountains, because the diamond deposits were found in India and Brazil, on high plateaus, on the sides of mountains, in the beds of mountain streams, and in the plains below; where mountain torrents had rolled them.
In Africa, for the first time, the true original home of the diamond was found at high levels in the mountains, in enormous fissures, open chasms, chimneys or pipes, extending to great and unknown depths. Into these immense chimneys, nature forced from subterranean sources, slow rivers of a peculiar blue clay, a diamondiferous earth termed “serpentine breccia” or “volcanic tuf” and now known by the latter-day name of “Kimberlite.” As this soft mixture oozed into the “chimneys” or “pipes” from the bottom, it was gradually forced upwards, filling the whole chasm from wall to wall and to the top, where its progress ended by hardening in a small mound ten to twelve feet higher than the surrounding surface.