[8] For a much more minute and extended account of the different modes proposed to reconcile geology and revelation, and indeed of their entire connection, I would refer to several papers in the American Biblical Repository, especially to the number for October, 1835, p. 261. The progress of science has, indeed, rendered it desirable to change a few sentences in those articles; but all their essential principles I still maintain.

[9] See Stuart and Hodge on Rom. v. 12; also Chalmers’s Lectures on Romans, Lecture 26; and Harris’s Man Primeval, p. 178.

[10] Johnston’s Physical Atlas, pp. 66, 76, (Philadelphia edition, 1850.)

[11] Rev. Joseph Tracy, Bibliotheca Sacra, Oct. 1850, p. 614.

[12] See the Frontispiece.

[13] The subject of this inference is treated with great ability and candor in the Biblotheca Sacra for November, 1849, by my friend and colleague, Rev. Joseph Haven, Jr., professor of intellectual and moral philosophy in Amherst College.

[14] In this description I have attempted to give exactly the experience of myself and John Tappan, Esq., with our wives, who ascended Snowdon in June, 1850. A few days after, we ascended Cader Idris, another mountain of Wales, near Dolgelly, where the views were perhaps equally wild and sublime, with the addition of a vast number of trap columns, and a pseudo-crater, with its jagged and frowning sides.

[15] When I visited this spot, in September, 1850, I was so fortunate as to get sight of a party that had just commenced the descent from the summit of Mont Blanc. To the naked eye they were invisible, but the whole train could be distinctly seen through a telescope. This was the third party that had ascended that mountain in the summer of 1850. I doubt not that the dangers have been exaggerated, and that the excursion will become common.

There are other points of great interest around Chamouny, which I have not noticed, some of which I visited, but not all. I have mentioned only the most common.

[16] In September, 1850, I visited this well, and found the water running still, at the rate of six hundred and sixty gallons per minute at the surface, and half that amount at the top of a tube one hundred and twelve feet high, from whence it could be carried to any part of Paris; and, in fact, does supply some of the streets. I tasted the water, and found it pleasant, though warm, (84 deg. Fahrenheit.)