Book, Paragraph

 1   I,  4 |     thrown downwards because the condensation which propels them inclines
 2   I,  4 |    sometimes the contraction and condensation of the air. Further, all
 3   I,  5 |        persist long, because the condensation of the air is transient.~"
 4   I,  5 |         air. When the process of condensation goes further in such a case
 5   I,  9 | obviously causes dissipation and condensation and so gives rise to generation
 6   I,  12|        and this happens when the condensation takes place quickly,-though
 7  II,  3 |         water that are formed by condensation, and must redescend to the
 8  II,  6 |         that they cause a sudden condensation.~Hurricanes are commonest
 9 III,  3 |          shows that a process of condensation is proceeding which must,
10 III,  3 |         the same way because the condensation they imply is so insignificant
11 III,  4 |        explained later. Again, a condensation of this kind cannot persist
12  IV,  6 |          Liquefaction is, first, condensation into water; second, the
13  IV,  6 |      solidified body. The first, condensation, is due to the cooling of