In gneisses, sandstones and limestones, joints also occur; and while frequently convenient for the division of the beds into masses of useful size, they may be a detriment, as when they occur so close together as to fall within the limits of a block suitable or economically usable for commercial purposes. In commerce the various kinds of building stone are usually designated by the name of the locality or region in which the quarry is situated. In the case of the more important varieties this geographic name usually conveys to the architect or builder sufficient information concerning colour, texture and other properties of the material.
The practice of quarrying consists in uncovering a sufficient surface of the rock by removing superficial soil, sand, clay, or overborder of overlaying waste rock by some suitable process or by sinking a shaft or slope, and then with proper tools or explosive, detaching blocks of form and size adapted to the purpose in view. Frequently the exposed outer portion of the rock has been either cut up and eroded away in fissures or has been affected by the action of various atmospheric agencies, until it has become discoloured or softened by decay. This weathered material must be removed before stone can be obtained for economic use in the production of dimension stone.
The separation of blocks of building or dimension stone is ordinarily carried on by some specific variation of one of the two general present-day methods of quarrying known respectively as the "blasting" and "channeling" process. Blasting is used for the harder rocks that do not tend to shatter and channeling for most other kinds of rock. The blasting process consists of drilling holes along the outlines of the block to be removed, and then, by exploding blasting-powder in the holes, exerting sufficient force to overcome the cohesion of the rock and rend it asunder. In many quarries it is found most convenient to separate a large mass and afterwards divide it into blocks of the required size, by drilling holes for further charges of blasting powder, or by driving wedges into these to split the rock. When the rock is
stratified, or has an easily determined rift, the holes are drilled at right angles to the plane of separation.
When there is no stratification or rift, or these natural planes of separation are too far apart, or when the position of the joints is not advantageous, a row of horizontal holes must be drilled into the face or breast of the quarry, along which separation is effected either by blasting or the use of wedges. At certain American quarries, in a granite which has no rift or direction of ready cleavage, compressed air has been brought into service to effect the separation of extensive layers. A hole is drilled as deep as the desired thickness of the layer to be separated, and a small charge of dynamite is exploded at the bottom of it. This develops a cavity in which a small charge of powder is next exploded, producing a crack or crevice parallel to the surface of the rock. A pipe for conveying compressed air is now sealed into the opening, and gradually increasing pressure is introduced. This results in the gradual extension of the crevice developed by the explosion of the powder. In the absence of compressed air, water under pressure may be used and also small powder charges exploded at intervals of a few days.