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 than that of the bottoms and valleys, and is a red, brown and black 274 loam. It produces an excellent quality of natural grass, and under careful cultivation, produces good crops of grain, fruits and vegetables. East of the Cascade Mountains the soil is a dark loam of great depth, composed of alluvial deposits and decomposed lava, overlying a clay subsoil. The constituents of this soil adapt the land peculiarly to the production of wheat.

All the mineral salts which are necessary to the perfect development of this cereal are abundant, reproducing themselves constantly as the gradual processes of decomposition in this soil of volcanic origin proceeds. The clods are easily broken by the plow, and the ground quickly crumbles on exposure to the atmosphere.

In Northwestern Oregon, adjacent to the Columbia River, although the dry season continues for months, this light porous land retains and absorbs enough moisture from the atmosphere, after the particles have been partly disintegrated, to insure perfect development and full harvests.

In Southeastern Oregon, especially in the vast areas of fertile lands in Malheur and Snake River Valleys, the soils are much like those of the Northeastern Oregon region, but there is less moisture. Except in a very small portion of this region, irrigation is necessary to successful