With levity he treats the apprehension of a coming convulsion, and laughs at the fears of the natives; but as soon as his wish is gratified, he is terror-stricken, and is involuntarily prompted to seek safety in flight.” Now, a partially consolidated planet, tempested by frequent earthquakes of such terrible potency, that those of the historic ages would be but mere ripples of the earth’s surface in comparison, could be no proper home for a creature so constituted. The fish or reptile,—animals of a limited range of instinct, exceedingly tenacious of life in most of their varieties, oviparous, prolific, and whose young immediately on their escape from the egg can provide for themselves, might enjoy existence in such circumstances, to the full extent of their narrow capacities; and when sudden death fell upon them,—though their remains, scattered over wide areas, continue to exhibit that distortion of posture incident to violent dissolution, which seems to speak of terror and suffering,—we may safely conclude there was but little real suffering on the case: they were happy up to a certain point, and unconscious forever after. Fishes and reptiles were the proper inhabitants of our planet during the ages of the earth-tempests; and when, under the operation of the chemical laws, these had become less frequent and terrible, the higher mammals were introduced. That prolonged ages of these tempests did exist, and that they gradually settled down, until the state of things became at length comparatively fixed and stable, few geologists will be disposed to deny. The evidence which supports _this_ special theory of the development of our planet in its capabilities as a scene of organized and sentient being, seems palpable at every step. Look first at these Grauwacke rocks; and, after marking how in one place the strata have been upturned on their edges for miles together, and how in another the Plutonic rock has risen molten from below, pass on to the Old Red Sandstone, and examine its significant platforms of violent death,—its faults, displacements, and dislocations; see, next, in the Coal Measures, those evidences of sinking and ever-sinking strata, for thousands of feet together; mark in the Oolite those vast overlying masses of trap, stretching athwart the landscape, far as the eye can reach; observe carefully how the signs of convulsion and catastrophe gradually lessen as we descend to the times of the Tertiary, though even in these ages of the mammiferous quadruped the earth must have had its oft-recurring ague fits of frightful intensity; and then, on closing the survey, consider how exceedingly partial and unfrequent these earth-tempests have become in the recent periods. Yes; we find every where marks of at once progression and identity,—of progress made, and yet identity maintained; but it is in the habitation that we find them,—not in the inhabitants. There is a tract of country in