Book, Paragraph

 1   I,  4 |          sun warms the earth the evaporation which takes place is necessarily
 2   I,  4 |         every state of the fumid evaporation: but we must use this terminology
 3   I,  4 |       and cooling of the moister evaporation: for this latter as it condenses
 4   I,  4 |          to the way in which the evaporation lies, and its disposition
 5   I,  7 |  necessarily drier and the moist evaporation is so dissolved and dissipated
 6   I,  10|         quenches the heat of the evaporation. But in Pontus the south
 7   I,  10|     bring warmth enough to cause evaporation, whereas the coldness of
 8   I,  10|    recoil, so that there is more evaporation and not less. This is a
 9   I,  10|        while in a south wind the evaporation is allowed to accumulate.~
10  II,  3 |        we recognize two kinds of evaporation, one moist, the other dry,
11  II,  3 |          a great quantity of dry evaporation from the places it passes
12  II,  4 |        We recognize two kinds of evaporation, one moist, the other dry.
13  II,  4 |         up by its heat the moist evaporation: when it recedes the cold
14  II,  4 |     since there are two kinds of evaporation, as we have said, one like
15  II,  4 |  explained before, while the dry evaporation is the source and substance
16  II,  4 |    phenomena themselves, for the evaporation that is to produce them
17  II,  4 |       warmed): whereas the smoky evaporation is hot and dry. Hence each
18  II,  4 |        theory. It is because the evaporation takes place uninterruptedly
19  II,  4 |          yet on occasion the dry evaporation will prevail in one part
20  II,  4 |         this latter is that each evaporation goes over to that of the
21  II,  4 |  district: for instance, the dry evaporation circulates in its own place
22  II,  4 |         place: or else the moist evaporation remains and the dry moves
23  II,  4 |          above and gives off the evaporation which we saw to be the material
24  II,  4 |          forms and cools the dry evaporation when the clouds are driven
25  II,  4 | approaches it provokes the moist evaporation, and when it recedes to
26  II,  4 |        the south, and since most evaporation must take place where there
27  II,  4 |       most smoke, and since this evaporation is wind, it is natural that
28  II,  4 |          oblique: for though the evaporation rises straight up from the
29  II,  4 |    defined as "a quantity of dry evaporation from the earth moving round
30  II,  4 |   oblique movement of the rising evaporation is caused from above: for
31  II,  5 |          stimulates it. When the evaporation is small in amount and faint
32  II,  5 |     lesser heat contained in the evaporation. It also dries up the earth,
33  II,  5 |         earth, the source of the evaporation, before the latter has appeared
34  II,  5 |       checks them by wasting the evaporation, and prevents their rising
35  II,  5 |         Either cold quenches the evaporation, for instance a sharp frost:
36  II,  5 |        generally either that the evaporation has not had time to develop
37  II,  5 |        dries up the earth before evaporation has taken place, but when
38  II,  5 |          little its heat and the evaporation are present in the right
39  II,  5 |      What is frozen gives off no evaporation, nor does that which contains
40  II,  5 |       moisture that it gives off evaporation under the influence of heat.~
41  II,  6 |      earth it necessarily causes evaporation to rise in greater quantities
42  II,  8 |        must both give rise to an evaporation: earthquakes are a necessary
43  II,  8 |       the inrush of the external evaporation into the earth.~Hence, since
44  II,  8 |          earth.~Hence, since the evaporation generally follows in a continuous
45  II,  8 |         about noon) it shuts the evaporation into the earth. Night, too,
46  II,  8 |     absence of the sun makes the evaporation return into the earth like
47  II,  8 |        of the dry over the moist evaporation. Again, excessive rain causes
48  II,  8 |          rain causes more of the evaporation to form in the earth. Then
49  II,  8 |   obscured and darkened when the evaporation which dissolves and rarefies
50  II,  8 |       The cold comes because the evaporation which is naturally and essentially
51  II,  8 |        as wind.) Well, when this evaporation disappears into the earth
52  II,  8 |         agency which created the evaporation and gave it an impulse to
53  II,  8 |       there is too little of the evaporation left to have any perceptible
54  II,  8 |         secretes far more of the evaporation than its depths. Wherever
55 III,  1 |       and wind is a dry and warm evaporation. Now frost and cold prevail
56 III,  6 |      that, but in every case the evaporation congealed before water was
57  IV,  7 |         whitening follows on the evaporation of any water that may have
58  IV,  7 |       that are thickened (not by evaporation due to fire) are made up
59  IV,  9 |          boil away or thicken by evaporation because it does not give
60  IV,  10|         for it is both liable to evaporation and it also thickens; for