The same winter maximum of rainfall is characteristic of the whole Pacific coast. The Region of the Lower Columbia, with an average rainfall of 46 inches, receives 47 per cent. of it in winter and 24 per cent. in spring. Southward on the coast, Drum Barracks (near Los Angeles) and San Diego receive more than half their rain in winter, but as the whole amount is only 9 inches agriculture is not benefited. The eastern bases of the Sierra Nevada and Cascade Range exhibit the winter maximum of rainfall, and this feature can be traced eastward in Idaho and Nevada, but in these districts it is accompanied by no amelioration of winter temperature. (See [Table X.])

Table X.—Seasonal precipitation and temperatures on the Pacific coast, etc.

Station.Mean annual rainfall.Percentage of rainfall.Mean temperature.
Inches.Spring.Summer.Autumn.Winter.Spring.Winter.
San Francisco Region 15.90 25 1 14 60 57 50
Region of Lower Columbia 46.45 24 6 23 47 51 40
Drum Barracks, Cal 8.74 26 3 4 67 60 56
San Diego, Cal 9.31 20 4 20 56 60 54
Camp Independence, Cal 6.60 17 5 9 69 57 39
Fort Bidwell, Cal 20.23 24 8 15 53 48 32
Camp Warner, Oreg 14.41 30 8 17 45 42 29
Camp Harney, Oreg 8.76 26 13 18 43 47 27
Fort Colville, Wash 14.06 26 22 18 34 45 24
Fort Walla Walla, Wash 19.36 24 11 26 39 52 34
Camp McDermitt, Nev 8.53 35 9 13 43 46 29
Camp Halleck, Nev 10.98 33 11 21 35 45 28
Fort Lapwai, Idaho 14.89 28 16 23 33 53 33
Fort Boisé, Idaho 15.48 33 8 16 43 52 30

Third District.—In Arizona and New Mexico there is a general maximum of rainfall in summer, and a restricted maximum in winter. The principal minimum is in spring. In [Table XI] the stations are arranged according to longitudes, a disposition well suited to exhibit their relations. In eastern New Mexico the distribution of rainfall has the same character as in adjacent Texas, but with a more decided maximum. Half of the total rainfall is in summer and half of the remainder in autumn. Westward the maximum diminishes slightly, but it appears in every station of the two territories. In western Arizona the winter maximum of the Pacific coast asserts itself, and it can be traced eastward as far as Fort Wingate, New Mexico. Except at Camp Mohave, on the western border of Arizona, it is inferior in amount to the summer maximum.

Table XI.—Seasonal precipitation in Arizona and New Mexico.

Station.Longitude.Mean annual rainfall.Percentage of annual rainfall.
° ´Inches.Spring.Summer.Autumn.Winter.
Western Texas 19 36 31 14
Fort Union, N. Mex 104 57 19.15 11 62 20 7
Cantonment Burgwin, N. Mex 105 30 8.65 18 34 28 20
Fort Stanton, N. Mex 105 38 20.94 14 51 23 12
Santa Fé, N. Mex 106 02 14.91 14 46 23 17
Albuquerque, N. Mex 106 38 8.11 10 54 25 11
Fort Fillmore, N. Mex 106 42 8.42 5 50 36 9
Fort Selden, N. Mex 106 55 8.49 7 57 22 14
Fort Craig, N. Mex 107 00 11.06 6 53 31 10
Fort McRae, N. Mex 107 03 11.59 21 53 20 6
Fort Wingate, N. Mex 107 45 17.32 11 38 20 31
Fort Bayard, N. Mex 108 30 14.32 11 50 16 23
Fort Defiance, Ariz 109 10 14.21 14 42 26 18
Camp Bowie, Ariz 109 30 15.26 9 48 13 30
Camp Grant, Ariz 110 40 15.08 14 41 22 23
Camp McDowell, Ariz 111 36 11.45 10 42 15 33
Camp Verde, Ariz 111 54 10.85 12 43 22 23
Camp Whipple, Ariz 112 20 19.28 20 42 11 27
Camp Mohave, Ariz 114 36 4.65 18 27 20 35
San Francisco Region 25 1 14 60

In all this region the daily range of temperature is great, and frosts occur so early in autumn that no use can be made of the autumnal rainfall. The yearly precipitation is very small, and the summer quota rarely exceeds seven or eight inches. Nevertheless the Pueblo Indians have succeeded, in a few localities, and by a unique method, in raising maize without irrigation. The yield is too meagre to tempt the white man to follow their example, and for his use the region is agricultural only where it can be watered artificially.

CHAPTER IV.
WATER SUPPLY.

By G. K. Gilbert.

The following discussion is based upon a special study of the drainage-basin of Great Salt Lake.