Geological reading, especially when of a strictly uniformitarian character and in warm weather, sometimes becomes monotonous.


Some Salient Points in the Science of the Earth, Chapter II (p. 9)


Geological reading, especially when of a strictly uniformitarian character and in warm weather, sometimes becomes monotonous.

Geological reading, especially when of a strictly uniformitarian character and in warm weather, sometimes becomes monotonous.

Geological reading, especially when of a strictly uniformitarian character and in warm weather, sometimes becomes monotonous.

Geological reading, especially when of a strictly uniformitarian character and in warm weather, sometimes becomes monotonous.