Useful Knowledge: Volume 1. Minerals: Or, a familiar account of the various productions of natureBingley, William
History
Useful Knowledge: Volume 1. Minerals: Or, a familiar account of the various productions of nature
Bingley, William
Commercial products; Geology, Economic; Natural history
This is a widely─extended rock; it sometimes forms whole mountains, and
even chains of mountains; but these usually have a gentle acclivity. The
summit of the celebrated mountain called Skiddaw in Cumberland is of
clay slate.
258. _PRIMITIVE LIMESTONE is a simple mountain rock of crystalline or
granular structure; and generally of white, yellowish, greenish, or
reddish colour._
To this species of rock belong many of the rich and beautiful kinds of
marble already described (143, &c.). Carrara, or statuary marble (146),
is a familiar instance of it. Whole mountains in Stiria, Carinthia,
Carniola, and the Pyrenees, and three mountains in Switzerland, 10,000
feet in height, are of primitive limestone. The mountain of Filabres in
Spain, is said to consist of one block of white granular marble, 2,000
feet high, and three miles in circuit; without intermixture of other
earths or stones, and almost without a fissure.
Various mineral ores, in beds and veins, as lead, zinc (241), and iron,
are occasionally found in this kind of rock.
259. _PRIMITIVE TRAP is a mountain rock composed of a black mineral
called hornblende, mixed, in some varieties, with felspar (110), and, in
others, with mica (123)._
The word _trap_ is of German origin, signifying a _stair_; and rocks of
this formation are called trap rocks, because their strata, when
exposed, usually jut out, one beneath the other, somewhat like a stair.
Under this term is comprehended a series of rocks, distinguished chiefly
by the hornblende, which they all contain.
Rocks belonging to this formation are numerous. They occur in Scotland;
and abundantly in Derbyshire and some other parts of England. In many
countries they constitute considerable hills. They abound in ores.
260. _SERPENTINE is a primitive rock, usually consisting of quartz (76),
magnesia (198), alumine (197), with a portion of oxide (21) of iron._
This rock and its various uses, have been already described (132). It
generally occurs in shapeless masses and beds; and seldom in distinct
strata. It is found in Cornwall, the island of Anglesea, and several
parts of Scotland; but it rarely forms mountains.
Ores of lead, silver, and copper, are sometimes found in serpentine.
261. _PORPHYRY is a primitive rock, consisting of quartz (76) or felspar
(110), or both, embedded in a solid and compact cement or ground._
_The ground or basis of porphyry varies in the different kinds. In some
it is claystone, in others pitchstone, hornstone, or compact felspar._
When not covered by other formations, porphyry sometimes forms single
rocks; but it never constitutes elevated mountains. It occurs in beds of
considerable magnitude, but never appears in distinct and well─defined
strata.
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