LECTURE XX.

_Of Argillaceous Earth._

Argillaceous earth is found in _clay_, _schistus_, or _slate_, and in

_mica_; but the purest is that which is precipitated from a solution of

alum by alkalies; for alum consists of the union of vitriolic acid and

argillaceous earth.

This species of earth is ductile with water; it then hardens and

contracts by heat, so as to be of the greatest use in forming _bricks_,

or stones of any required form or size. By means of the property of clay

to contract in the fire, Mr. Wedgwood has constructed an excellent

thermometer to measure the degrees of extreme heat.

The ductility of clay seems to depend upon some acid, probably the

vitriolic, adhering to it; for it loses that property when it is burned

into a brick, but recovers it when it has been again dissolved in an

acid.

_Of Terra Ponderosa._

_Terra ponderosa_, or _marmor metallicum_, is generally found in two

states, viz. united to vitriolic acid, when it is called _calk_, or to

fixed air, when it is called _terra ponderosa aerata_.

To obtain it pure from its union with the vitriolic acid, it must be

melted with about twice its weight of fixed alkali; which unites with

the acid, and forming a saline substance, may be washed out of it. In

this state it contains water, and therefore, when exposed to heat, will

yield fixed air; whereas the terra ponderosa aerata will not yield fixed

air by heat only, but when steam is made to pass over it when red hot.

This proves that water is essential to the composition of fixed air.

This stone is distinguishable by its great specific gravity, being four

times as heavy as water; but though in this it resembles an _ore_, it

has not been found to be metallizable.

_Of Magnesia._

This species of earth is found in _steatites_, or _soap rock_, _Spanish

chalk_, _asbestus_, and _Muscovy talck_; but the purest is got by

dissolving _Epsom salts_ (which consists of this earth united to the

vitriolic acid) and precipitating it by a mild alkali. In this state it

becomes united to fixed air, which may be expelled by heat. It is then

_calcined_, or _caustic_, but differs from quick-lime by not being

soluble in water.

_Asbestus_, which contains much of this kind of earth, is remarkable for

not being destructible by heat, though it is sometimes found in flexible

fibres, so as to be capable of being woven into cloth.

_Muscovy talck_ is remarkable for the thin and transparent flakes into

which it is divisible, and thereby capable of various uses.

There are some other distinct species of earth, particularly one brought

from Botany Bay, and another called _Stontiate_, from the place where it

was found in Scotland; but they have not as yet been much examined.

All stones formed by nature are compounded, and to distinguish them from

one another, and ascertain the parts of which they consist, is the

subject of _lithology_, a very extensive branch of knowledge.

All the simple earths are nearly, if not absolutely, _infusible_; but

when they are mixed they may all be fused.

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