Page:Geology and Mineralogy considered with reference to Natural Theology, 1837, volume 1.djvu/430

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426
PROOFS OF DESIGN.

to preserve the purity of the sea, renders them unfit for the support of terrestrial animals or vegetables,) and transmitting them in genial showers to scatter fertility over the earth, and maintain the never-failing reservoirs of those springs and rivers by which they are again returned to mix with their parent ocean; in all these circumstances we find such evidence of nicely balanced adaptation of means to ends, of wise foresight, and benevolent intention, and infinite power, that he must be blind indeed, who refuses to recognize in them proofs of the most exalted attributes of the Creator."[1]





CHAPTER XXIII.


Proofs of Design in the Structure and Composition of unorganized Mineral Bodies.


Much of the physical history of the compound forms of unorganized mineral bodies, has been anticipated in the considerations given in our early chapters to the unstratified and crystalline rocks. It remains only to say a few words respecting the simple minerals that form the ingredients of these rocks, and the elementary bodies of which they are composed.[2]

"In crossing a heath," (says Paley,) "suppose I pitched my foot against a stone, and were asked how the stone came

  1. Buckland, Inaug. Lecture, p. 13.
  2. The term simple mineral is applied not only to uncombined mineral substances, which are rare in Nature, such as pure native gold or silver, but also to all kinds of compound mineral bodies that present a regular crystalline structure, accompanied by definite proportions of their chemical ingredients. The difference between a simple mineral and a simple substance may be illustrated by the case of calcareous spar, or crystallized carbonate of lime. The ultimate elements, viz. Calcium, Oxygen, and Carbon, are simple substances; the crystalline compound resulting from the union of these elements, in certain definite proportions, forms a simple mineral, called Carbonate of lime. The total number of simple minerals hitherto ascertained according to Berzelius is nearly six hundred, that of simple substances, or elementary principles, is fifty-four.