Book, Paragraph

1   I,  3 |     the sun’s motion alone is sufficient to account for the origin
2   I,  3 | combines both conditions in a sufficient degree. That most heat should
3   I,  10|      been raised nor the cold sufficient (owing to the warmth of
4   I,  12|  certain time and the cold is sufficient to freeze it in less, there
5   I,  13|      almost say, would not be sufficient (any more than the region
6  II,  8 |   When the wind is present in sufficient quantity there is an earthquake.
7  IV,  12|      the hot and the cold are sufficient to form all such parts as
8  IV,  12|       far as to consider them sufficient in the case of the non-homogeneous