Book, Paragraph

 1   I,  10|          and is commoner in cold places. It is dew when the vapour
 2   I,  10|     rises from hollow and watery places, so that the heat that is
 3   I,  10|       can often observe in other places too. Wells, for instance,
 4   I,  12|       warmer, and snow in colder places. Again, there is a difficulty
 5   I,  13|    minute quantities but in many places. They receive a great deal
 6   I,  13|      about the existence of such places containing a quantity of
 7   I,  13|     valleys to the sea. So these places get full of water, and this,
 8   I,  13|         it together but in three places. And in Liguria a river
 9   I,  14|      life and moisture. Now when places become drier the springs
10   I,  14|         of prosperity. For these places dry up and come to be in
11   I,  14|         good condition while the places that were formerly well-tempered
12   I,  14|         to have happened in more places now than formerly. But this
13   I,  14|       true. It is true that many places are now dry, that formerly
14   I,  14|         find that there are many places where the sea has invaded
15   I,  14|       make the moisture of those places almost everlasting. But
16   I,  14| everlasting. But as time goes on places of the latter type dry up
17   I,  14|         as we say, that the same places are not for ever moist through
18  II,  2 |       reason being that the same places cannot always supply the
19  II,  2 |      these form lakes in various places (our sea is an instance
20  II,  3 |          from the fact that many places are found to be drier now
21  II,  3 |         dry evaporation from the places it passes over.) The north
22  II,  3 |       flavours are found in many places. These flavours must in
23  II,  4 |        district because adjacent places (unless there is something
24  II,  4 |         generally rises in those places where the rain fell, and
25  II,  6 |   definite winds and these their places.~There are more winds from
26  II,  7 |      found to be sinking in many places. Again, why do earthquakes
27  II,  7 |  earthquakes frequently occur in places which are not excessively
28  II,  8 |      confined character of these places that makes them so liable
29  II,  8 |       actual observation in many places. It has been known to happen
30  II,  8 |          a sound is heard in the places from which the eruptions
31  II,  8 |    except occasionally, in a few places, where they act vertically,