Field book of common rocks and minerals : $b for identifying the rocks and minerals of the United States and interpreting their origins and meaningsLoomis, Frederic Brewster
Science
Field book of common rocks and minerals : $b for identifying the rocks and minerals of the United States and interpreting their origins and meanings
Loomis, Frederic Brewster
Minerals -- United States; Rocks -- United States
Sand is used for a wide variety of commercial purposes, and under these
conditions gets various trade names; for instance “glass sand” is a
pure, colorless to white, quartz sand, which is used as one of the
components in making glass. It must be free from impurities, as these
color the glass, and much of the sand used for this purpose is quartz,
crushed to a fine sand-like condition. “Moulding sand” is a rather
fine-grained quartz sand, with a small but very definite admixture of
clay, and this is used to make the moulds for castings in foundries.
“Polishing sand” is one composed of angular fragments of quartz, usually
from stream beds or glacial deposits, or even crushed quartz, and is
used for cutting and polishing marble, for sandpaper, and for polishing
wood and softer stones. There are many other special uses, like
building, ballast, filters, furnaces, etc., in which quartz sand is
used, being screened if necessary to get the right sizes.
Sandstone
When sand of any sort is cemented so as to make a solid rock, it is
termed sandstone, which varies widely according to the size, color and
composition of the grains, and also with the sort and amount of the
cement. When the size of the grains is larger than that of a pea,
sandstone grades into conglomerate; when smaller than ¹/₅₀₀th of an
inch, especially if mixed with clay, it grades into shale. There are all
grades of firmness, due to the amount and kind of cement, ranging from
those which have little or no cement, but are compact as a result of the
pressure of the overlying rocks, to those in which the cement has filled
all the pore spaces. In general there is a considerable amount of space
between the grains of sand; so that a sandstone will absorb large
amounts of water, up to 25% of its bulk. In moist climates where it
freezes, this makes many sandstones unsuitable for use as building
stones, as they are likely to spale, or chip off, as is seen in the
“brown stone” so much used in New York City.
Sandstones are usually bedded rocks and are relatively easy to quarry,
and most of them are not so firmly cemented, but that they can be
readily worked or cut into shape by the stone cutter; and so, certain
sandstones are very popular for building stone or for trimming on
buildings, where they are not too much exposed to the weather.
Sandstone gets a variety of names according to the cement.
Siliceous sandstone is cemented with silica and usually very hard.
Calcareous sandstone is cemented with lime and usually rather soft.
Ferruginous sandstone is cemented with one of the iron oxides.
Argillaceous sandstone is held together with clay impurities, and is
usually both soft and of undesirable color.
According to their composition there is also a number of varieties.
Arkose is a sandstone composed of quartz and feldspar grains, usually
derived from the disintegration of granite and not transported far.
Public-domain text, read in full here on John Shaqi.
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