Dry-farmers in that section will of
necessity be obliged to adopt cultural methods that will prevent the
excessive evaporation naturally induced by the unhindered wind, and
the possible blowing of well-tilled fallow land.
Summary
The dry-farm territory is characterized by a low rainfall, averaging
between 10 and 20 inches, the distribution of which falls into two
distinct types: a heavy winter and spring with a light summer
precipitation, and a heavy spring and summer with a light winter
precipitation. Snow falls over most of the territory, but does not
lie long outside of the mountain states. The whole dry-farm
territory may be classed as temperate to cold; relatively high and
persistent winds blow only over the Great Plains, though local
conditions cause strong regular winds in many other places; the air
is dry and the sunshine is very abundant. In brief, little water
falls upon the dry-farm territory, and the climatic factors are of a
nature to cause rapid evaporation.
In view of this knowledge, it is not surprising that thousands of
farmers, employing, often carelessly agricultural methods developed
in humid sections, have found only hardships and poverty on the
present dry-farm empire of the United States.
Pages:
26
27
28
29
30
31
32
33
34
35
36
37
38
39
40
41
42
43
44
45
46
47
48
49
50