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BUILDING STONES

Classification.— Building stones are classified in a general way un­der the heading of igneous, sedimentary, and metamorphic rocks.

Igneous -Rocks.—These are formed by fusion below the earth's surface.

Sedimentary Rocks. —All sedimentary rocks, which include sand­stones and limestones, come under this heading. They are formed in deposits by the agency of water or winds, and are known as strati­fied rocks.

Metamorphic Rocks.—These may be either of the above when changed information by heat and pressure. Marbles and slates come under this heading.

Granites.—Granites are igneous rocks made up of granular parti­cles, the latter being crystalline, and usually composed of quartz, fel­spar, and mica.

Granite has never flowed out over the earth's surface as lava, but became consolidated at a great depth under extreme pressure.

Quartz.—The durability of granite depends largely upon the amount of quartz and its combination with other minerals, quartz being practically indestructible. Quartz, sand, and the chemical named silica may be said to be interchangeable terms.

Felspar is the most easily distinguished mineral and its colour varies considerably. The pink felspar is known as orthoelase, and is a potash felspar; this constituent is very characteristic in granite. Sometimes the white soda or lime felspar known as plagioclase is found. Felspars are commonly found with about equal quantities of quartz.

Mica is of two kinds: muscovite, which is potash mica (light); and biotite, which is a dark brown, iron and other substances being present. The light micas are more stable.

The proportions of mica should be small compared with quartz and felspar. Hornblende and augite sometimes occur and take the place of mica; the stone is then known as a syenite.

Iron pyrites produce oxidation and hydration either in the form of local spots, or as a uniform tinge of brown, and should always be looked upon as a fault.

The characteristics of a good granite are: fineness of grain, the disposition of the various minerals forming the mass, and the high percentage of quartz present.

Sandstones. —Sandstones are formed by the disruption of pre­existing rocks due to the action of winds or moving water, the par­ticles being deposited in beds, or strata. The chief constituents are the original quartz crystals (or grains) and the cement that binds them together. The quality of a sandstone depends upon the cementing ma­terial. The presence of an inferior cementing material is the chief cause of disintegration upon the exposed surfaces. The cementing ma­terials are numerous, and may be silica, clay, iron oxides, caleite, or dolomite. Usually there is a combination of these substances, but one kind predominates. Sometimes the grains, or quartz crystals, are соnsolidated by heat and pressure as in quartzite. Sandstones vary from fine grain to coarse grit stone, whilst the colour depends chiefly upon the cementing material. Red, brown, and yellow are due to oxide of iron. White owes its colour to the combination of clear quartz with white argillaceous or clay-containing matter free from iron stains.

If the stone contains a high percentage of mica distributed along the planes of bedding it is known as a micaceous sandstone. Great care should be exercised in placing sandstones in the building so that the laminae are horizontal.

Limestones.— Тhe chief characteristic of limestones is the presence of a large proportion of carbonate of lime. They were formed chiefly by the accumulation of shells or calcareous skeletons of marine or fresh water organisms, which were deposited as sediment in the waters of seas or lakes. The common or chalk limestones are more suit­ed for the production of lime. The oolitic limestones are of marine origin; they are composed chiefly of carbonate of lime, with other substances, such as carbonate of magnesia, silica, alumina, and iron. The oolite resembles the roe of a fish, and results from the accumu­lation of carbonate of lime around the small nuclei of fragmentary shells or grains of mud or sand. They are of spherical or oval shape, and can easily be seen with the naked eye. They vary in hardness and texture; some are fairly fine, others coarse and porous.

All limestones are soft when first quarried, but harden on expo­sure to the atmosphere.

The stone should be uniform in colour throughout in the case of both sandstones and limestones.

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