Lyell's Principles of Geology*

Abstract

IN our last notice, after a sketch of the methods of investigation employed by Sir Charles Lyell, and an outline of the principles deduced therefrom, we gave a few examples of the kind of proofs brought forward by him to show that the degrading and transporting forces which we see in operation are producing similar phenomena to those we observe in the sedimentary rocks, and that, given sufficient time only, effects on as great a scale must be the inevitable result.

Authors

Rights and permissions

Reprints and Permissions

About this article

Cite this article

HUGHES, T. Lyell's Principles of Geology* . Nature 6, 165–168 (1872). https://doi.org/10.1038/006165a0

Download citation

Comments

By submitting a comment you agree to abide by our Terms and Community Guidelines. If you find something abusive or that does not comply with our terms or guidelines please flag it as inappropriate.

Search

Nature Briefing

Sign up for the Nature Briefing newsletter — what matters in science, free to your inbox daily.

Get the most important science stories of the day, free in your inbox. Sign up for Nature Briefing