[Footnote 67: Lecture I of three Lectures on Evolution. From American Addresses, London, 1877.]
[Footnote 68: The diagram, which is not reproduced here, gives an ideal section of the crust of the earth, showing the various strata lying one under the other. The strata are divided by geologists into three groups: the Primary, which is the oldest and deepest; the Secondary, above that; and the Tertiary and Quaternary on top. The Cretaceous is the lowest stratum of the Tertiary.]
[Footnote 69: One of the upper strata of the Primary rocks.]
[Footnote 70: The Silurian rocks occur about the middle of the Primary formations. The _eozoön_ was formerly supposed by some geologists to be a form of fossil. The Laurentian rocks are the lowest strata of the Primary formations.]
[Footnote 71: The Jurassic formation occurs about the middle, the Triassic, just below it, in the lower half of the Secondary rocks. The Devonian occurs just above the middle of the Secondary, between the Carboniferous above and the Silurian below.]
[Footnote 72: From _The Popular Science Monthly_, July, 1901.]
[Footnote 75: _The Outlook_, April 29, 1911.]
[Footnote 76: Probably the reason why it has not yet been adopted by Switzerland is because her organized manufacturing Industries are so few that no pressure has been brought upon the state to change the law.]
[Footnote 77: Robertson _vs_. Baldwin, United States, 281.]
[Footnote 78: Noble State Bank _vs_. Haskell; Shallenberger _vs_. Bank of Holstein, January 3, 1911. Lawyers' Cooperative Publishing Company, Rochester, New York.]
[Footnote 79: Foster, Argumentation and Debating, p. 281.]
End of Project Gutenberg's The Making of Arguments, by J. H. Gardiner