(327.) It was only, however, when chemical analysis had acquired
a certain degree of precision and universal applicability that
the importance of mineralogy as a science began to be recognized,
and the connection between the external characters of a stone and
its ingredient constituents brought into distinct notice. Among
these characters, however, none were found to possess that eminent
distinctness which the crystalline form offers; a character, in the
highest degree geometrical, and affording, as might be naturally
supposed, the strongest evidence of its necessary connection with the
intimate constitution of the substance. The full importance of this
character was, however, not felt until its connection with the texture
or cleavage of a mineral was pointed out, and even then it required
numerous and striking instances of the critical discernment of Haüy
and other eminent mineralogists in predicting from the measurements
of the angles of crystals which had been confounded together that
differences would be found to exist in their chemical composition, all
which proved fully justified in their result before the essential value
of this character was acknowledged. This was no doubt in great measure
owing to the high importance set by the German mineralogists on those
external characters of touch, sight, weight, colour, and other sensible
qualities, which are little susceptible, with the exception of weight,
of exact determination, and which are subject to material variations
in different specimens of the same mineral. By degrees, however, the
necessity of ascribing great weight to a character so definite was
admitted, especially when it was considered that the same step which
pointed out the intimate connection of external form with internal
structure furnished the mineralogist with the means of reducing all
the forms of which a mineral is susceptible under one general type, or
primitive form, and afforded grounds for an elegant theoretical account
of the assumption of definite figures _ab initio_.
(328.) A simple and elegant invention of Dr. Wollaston, the reflecting
goniometer, gave a fresh impulse to that view of mineralogy which makes
the crystalline form the essential or leading character, by putting
it in the power of every one, by the examination of even the smallest
portion of a broken crystal, to ascertain and verify that essential
character on which the identity of a mineral in the system of Haüy
was made to depend. The application of so ready and exact a method
speedily led to important results, and to a still nicer discrimination
of mineral species than could before be attained; and the confirmation
given to these results by chemical analysis stamped them with a
scientific and decided character which they have retained ever since.
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