Geological facts; or, the crust of the earth, what it is, and what are its usesBarrett, W. G. (William Garland)
Religion
Geological facts; or, the crust of the earth, what it is, and what are its uses
Barrett, W. G. (William Garland)
Geology
Lord Bacon remarks, “Some men think that the gratification of curiosity
is the end of knowledge, some the love of fame, some the pleasure of
dispute, and some the necessity of supporting themselves by knowledge;
but the real use of all knowledge is this, that we should dedicate that
reason which was given us by God to the use and advantage of man.” The
historian of the old red sandstone, Hugh Miller, to whose researches not
only we, but such men as Murchison, Lyell, Ansted, Agassiz and others,
are so exclusively indebted, is a philosopher in this last category. He
does not hesitate to tell us, how, as a Cromarty quarryman “twenty years
ago,” he commenced a “life of labour and restraint,” a “slim,
loose-jointed boy, fond of the pretty intangibilities of romance, and of
dreaming when broad awake;”[35] and how, as a quarryman, he ever kept
his eyes open, to observe the results of every blow of the hammer,
stroke of the pick, or blast of the powder; and finding himself in the
midst of new and undreamt-of relics of an old creation, preserved in
“tables of stone,” he adds _his_ testimony to that of the great father
of inductive philosophy, “that it cannot be too extensively known, that
nature is vast and knowledge limited, and that no individual, however
humble in place or acquirement, need despair of adding to the general
fund.”[36]
We here enter upon a marvellous field of discovery. Hitherto the forms
of life we have met with have all been invertebrate. The trilobite,
something between a crab and a beetle, once revelling, in untold
myriads, probably on the land as well as in the water, and of which two
hundred and fifty species have been brought to light, is the highest
type of life with which our researches have made us familiar. We are now
to begin the study of fossil fish, and to their discovery, strange
forms, and characters, this chapter will be specially devoted. It was
once a generally received opinion among even the most learned
geologists, that the “old red sandstone,” or the “Devonian system,” was
particularly barren of fossils, but the labours (literally such, “mente,
manu, malleoque”[37]) of Hugh Miller have proved the contrary. “The
fossils,” he says, “are remarkably numerous, and in a state of high
preservation. I have a hundred solid proofs by which to establish the
proof of my assertion, within less than a yard of me. Half my closet
walls are covered with the peculiar fossils of the lower old red
sandstone; and certainty a stranger assemblage of forms have rarely been
grouped together; creatures whose very type is lost, fantastic and
uncouth, and which puzzle the naturalist to assign them even their
class; boat-like animals, furnished with oars and a rudder; fish plated
over like the tortoise, above and below, with a strong armour of bone,
and furnished with but one solitary rudder-like fin; other fish less
equivocal in their form, but with the membranes of their fins thickly
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