Book, Paragraph

 1   I,  9 |          condensing into water is cloud. Mist is what is left over
 2   I,  9 |          what is left over when a cloud condenses into water, and
 3   I,  9 |          might be called a barren cloud. So we get a circular process
 4   I,  11|        and snow is the same: when cloud freezes there is snow, when
 5   I,  11|          were overpowering it the cloud would not freeze. For there
 6   I,  12|       origin of hail is this. The cloud is thrust up into the upper
 7   I,  12|        not take place because the cloud is thrust up into the cold
 8   I,  12|   surrounding heat and causes the cloud to go over into water suddenly. (
 9   I,  12|        that this happens when the cloud has risen into the cold
10   I,  12|          that it happens when the cloud has descended into the warm
11   I,  12|          the more the further the cloud has descended). But when
12   I,  13|           condenses again becomes cloud and water, implying that
13  II,  8 |         little, light, long-drawn cloud is seen, like a long very
14  II,  8 |       this very straight and thin cloud is left, a sort of wave-mark
15  II,  9 |       said before, condenses into cloud, and the density of the
16  II,  9 |           the densest part of the cloud.) Now the heat that escapes
17  II,  9 |          of its extinction in the cloud.~But this involves the view
18  II,  9 |          that the moisture in the cloud is beaten about in the same
19  II,  9 |          fire shining through the cloud and thunder its extinction,
20 III,  1 |           quantity present in the cloud is at once secreted from
21 III,  1 |   Sometimes the exhalation in the cloud, when it is being secreted,
22 III,  1 |    hurricane which shakes off the cloud without cessation and becomes
23 III,  1 |    becomes a continuous wind) the cloud follows the exhalation unbroken,
24 III,  1 |    failing to break away from the cloud because of its density,
25 III,  1 |      hurricane to escape from its cloud: it is due to the resistance
26 III,  1 |       earth and drags with it the cloud which it cannot shake off.
27 III,  1 |       whatever it meets.~When the cloud burns as it is drawn downwards,
28 III,  1 |        and is squeezed out in the cloud itself we get a thunderbolt.
29 III,  3 |       vapour are condensed into a cloud and the condensed matter
30 III,  3 |        through the points GZD the cloud from which the line of sight
31 III,  3 | indivisible to sense. The band of cloud next to it is black, its
32 III,  4 |         bright enough to make the cloud a mirror and cause the sight
33 III,  4 |          whenever the sun and the cloud are related in the way described
34 III,  4 |         noticing. When there is a cloud near the sun and we look
35 III,  4 |          when we look at the same cloud in water it shows a trace
36 III,  4 |        rainbow is purest when the cloud is blackest; and then the
37 III,  4 |         with the blackness of the cloud around: for it is white
38 III,  4 |          is white compared to the cloud and the green. Again, when
39 III,  4 |          is dissolving, the white cloud is brought into contact
40 III,  4 |    because it appears on the dark cloud and at night. So, just as
41 III,  6 |        some liquid surface to the cloud. Here the clouds themselves
42 III,  6 |     latter case the colour of the cloud seems to reside in the water,
43 III,  6 |           the case of rods on the cloud itself. Rods appear when
44 III,  6 |       when the composition of the cloud is uneven, dense in part
45 III,  6 |         for the sun dissolves the cloud if it is near, but if it
46 III,  6 |      opposite to the sun.) If the cloud is above the sun and close
47 III,  6 |         sun does not dissolve the cloud, and yet sight reaches it