Arizona miner., 1867-01-12

from which their Spanish name has been de- rived.
 The prevalent rock formations of the ses- ersi ranges are the metamorph'c gnciss, gran tc. ,Arphyrier, and micac ous and saic'~e sia,e. inc two last mentioned being mort con,non in the western ranges. Thegran'trs are in general highly leidspatpc, and ls these nnd the other n,etanorphicrocks winch contain those rich metalifcrous veins W whose nature and value we shall presently hase te trr in detail
 T C ridges composing the different chains are scp rated .hy valleys, some ci wh'ch are osextytofliinary fertility, and well calculated 10 reward the labors of the agricuturalisf Iwhile between the great chains themselves lie vast tracts of table land, elevated from 5000 to 4,tt0 feet above the level of the sea. l IA brief nbtiee of toe bptanynot tf'e Itsr West wi) lisnilict For ,Hr pvrpuse, beleHthe line of pcfsetual sDOw tue mountain Si'isr are generally covered with spruce, halsam tif, and pine, which, lower down, become inter. mixed with beach, birch, and various other trees. The plaps. whsre not desert, are usually clad m the specie, of grass peculiar to the prairies, ani aiong the river banks groves of willow and cottonwood are frequently "a ! he found, wAile in certain districts tiowcs'Hs plante so abound tha, when in full bloom they ! give to the country the appcarance oi aYAst garden,
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