The Testimony Of The Rocks
Hugh Miller
16 chapters
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16 chapters
TESTIMONY OF THE ROCKS;
TESTIMONY OF THE ROCKS;
OR, GEOLOGY IN ITS BEARINGS ON THE TWO THEOLOGIES, NATURAL AND REVEALED. BY HUGH MILLER, AUTHOR OF "THE OLD RED SANDSTONE," "FOOTPRINTS OF THE CREATOR," ETC., ETC. WITH MEMORIALS OF THE DEATH AND CHARACTER OF THE AUTHOR. "Thou shalt be in league with the stones of the field."— Job.   BOSTON: GOULD AND LINCOLN, 59 WASHINGTON STREET. NEW YORK: SHELDON, BLAKEMAN & CO. CINCINNATI: GEORGE S. BLANCHARD. 1857. Entered according to Act of Congress, in the year 1857, by GOULD AND LINCOLN, In the
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TO THE READER.
TO THE READER.
Of the twelve following Lectures, four (the First, Second, Fifth, and Sixth) were delivered before the members of the Edinburgh Philosophical Institution (1852 and 1855). One (the Third) was read at Exeter Hall before the Young Men's Christian Association (1854), and the substance of two of the others (the Eleventh and Twelfth) at Glasgow, before the Geological Section of the British Association (1855). Of the five others,—written mainly to complete and impart a character of unity to the volume
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MEMORIALS
MEMORIALS
OF THE DEATH AND CHARACTER OF HUGH MILLER, WITH AN ACCOUNT OF HIS FUNERAL OBSEQUIES. Near the end of last autumn the American publishers of Hugh Miller's works received from him, through his Edinburgh publishers, the offer of a new work from his pen. The offer was accepted and a contract was at once closed. Soon the advance sheets began to come; and as successive portions were received and perused, it became more and more evident that the work was destined not only to extend his fame, but to est
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A PRAYER
A PRAYER
BY JOHN KNOX, MADE AT THE FIRST ASSEMBLIE OF THE CONGREGATION, WHEN THE CONFESSION OF OUR FAITHE AND WHOLE ORDERS OF THE CHURCH WAS THERE RED AND APPROVED. [3] O Lord God Almightie, and Father moste mcrcifull, there is none lyke thee in heaven nor in earthe, which workest all thinges for the glorie of thy name and the comfort of thyne elect. Thou dydst once make man ruler over all thy creatures, and placed hym in the garden of all pleasures; but how soone, alas, dyd he in his felicitie forget th
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LECTURE FIRST.
LECTURE FIRST.
THE PALÆONTOLOGICAL HISTORY OF PLANTS. Palæontology , or the science of ancient organisms, deals, as its subject, with all the plants and animals of all the geologic periods. It bears nearly the same sort of relation to the physical history of the past, that biography does to the civil and political history of the past. For just as a complete biographic system would include every name known to the historian, a complete palæontologic system would include every fossil known to the geologist. It en
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LECTURE SECOND.
LECTURE SECOND.
THE PALÆONTOLOGICAL HISTORY OF ANIMALS. Amid the unceasing change and endless variety of nature there occur certain great radical ideas, that, while they form, if I may so express myself, the groundwork of the change,—the basis of the variety,—admit in themselves of no change or variety whatever. They constitute the aye-enduring tissue on which the ever-changing patterns of creation are inscribed: the patterns are ever varying; the tissue which exhibits them for ever remains the same. In the ani
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LECTURE THIRD.
LECTURE THIRD.
THE TWO RECORDS, MOSAIC AND GEOLOGICAL. It is now exactly fifty years since a clergyman of the Scottish Church, engaged in lecturing at St. Andrews, took occasion in enumerating the various earths of the chemist, to allude to the science, then in its infancy, that specially deals with the rocks and soils which these earths compose. "There is a prejudice," he remarked, "against the speculations of the geologist, which I am anxious to remove. It has been said that they nurture infidel propensities
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LECTURE FOURTH.
LECTURE FOURTH.
THE MOSAIC VISION OF CREATION. The history of creation is introduced into the "Paradise Lost" as a piece of narrative, and forms one of the two great episodes of the poem. Milton represents the common father of the race as "led on" by a desire to know "What within Eden or without was done Before his memory;" and straightway Raphael, "the affable archangel," in compliance with the wish, enters into a description of the six days' work of the Divine Creator,—a description in which, as Addison well
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LECTURE FIFTH.
LECTURE FIFTH.
GEOLOGY IN ITS BEARINGS ON THE TWO THEOLOGIES. PART I. The science of the geologist seems destined to exert a marked influence on that of the natural theologian. For not only does it greatly add to the materials on which the natural theologian founds his deductions, by adding to the organisms, plant and animal, of the present creation the extinct organisms of the creations of the past, with all their extraordinary display of adaptation and design; but it affords him, besides, materials peculiar
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LECTURE SIXTH.
LECTURE SIXTH.
GEOLOGY IN ITS BEARINGS ON THE TWO THEOLOGIES. PART II. Up till the introduction of man upon our planet, the humbler creatures, his predecessors, formed but mere figures in its various landscapes, and failed to alter or affect by their works the face of nature. They were conspicuous, not from what they did , but from what they were . At a very early period reefs of coral, the work of minute zoophytes, whitened the shallows of the ocean, or encircled with pale, ever broadening frames, solitary is
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LECTURE SEVENTH.
LECTURE SEVENTH.
THE NOACHIAN DELUGE. PART I. There are events so striking in themselves or from their accompaniments, that they powerfully impress the memories of children but little removed from infancy, and are retained by them in a sort of troubled recollection ever after, however extended their term of life. Samuel Johnson was only two and a half years old when, in accordance with the belief of the time, he was touched by Queen Anne for the "Evil;" but more than seventy years after, he could call up in memo
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LECTURE EIGHTH.
LECTURE EIGHTH.
THE NOACHIAN DELUGE. PART II. A century has not yet gone by since all the organic remains on which the science of Palæontology is now founded were regarded as the wrecks of a universal deluge, and held good in evidence that the waters had prevailed in every known country, and risen over the highest hills. Intelligent observers were not wanting at even an earlier time who maintained that a temporary flood could not have occasioned phenomena so extraordinary. Such was the view taken by several Ita
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LECTURE NINTH.
LECTURE NINTH.
THE DISCOVERABLE AND THE REVEALED. It seems natural, nay, inevitable, that false revelations, which have descended from remote, unscientific ages, should be committed to a false science. Natural phenomena, when of an extraordinary character, powerfully impress the untutored mind. In operating, through the curiosity or the fears of men, upon that instinct of humanity—never wholly inactive in even the rudest state—which cannot witness any remarkable effect without seeking to connect it with its pr
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LECTURE TENTH.
LECTURE TENTH.
THE GEOLOGY OF THE ANTI-GEOLOGISTS. It has been well remarked, that that writer would be equally in danger of error who would assign very abstruse motives for the conduct of great bodies of men, or very obvious causes for the great phenomena of nature. The motives of the masses,—on a level always with the average comprehension,—are never abstruse; the causes of the phenomena, on the other hand, are never obvious. And when these last are hastily sought after, not from any devotion to scientific t
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LECTURE ELEVENTH.
LECTURE ELEVENTH.
ON THE LESS KNOWN FOSSIL FLORAS OF SCOTLAND. [45] PART I. Scotland has its four fossil floras,—its flora of the Old Red Sandstone, its Carboniferous flora, its Oolitic flora, and that flora of apparently Tertiary age of which his Grace the Duke of Argyll found so interesting a fragment overflown by the thick basalt beds and trap tuffs of Mull. Of these, the only one adequately known to the geologist is the gorgeous flora of the Coal Measures,—probably the richest, in at least individual plants,
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LECTURE TWELFTH.
LECTURE TWELFTH.
ON THE LESS KNOWN FOSSIL FLORAS OF SCOTLAND. PART II. In the noble flora of the Coal Measures much still remains to be done in Scotland. Our Lower Carboniferous rocks are of immense development; the Limestones of Burdiehouse, with their numerous terrestrial plants, occur many hundred feet beneath our Mountain Limestones; and our list of vegetable species peculiar to these lower deposits is still very incomplete. Even in those higher Carboniferous rocks with which the many coal workings of the co
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