Page 721 - calmining1890
P. 721

SOLANO COUNTY.                             671

                    orked so as to show a face from twenty to twenty-five      feet in height.
                   'he mass of the country rock, though nowhere visible in the immediate
                   neighborhood,  is probably    sandstone; but the bottom of the deposit
                   f aragonite has not yet been reached.      Much of the upper portion of
                   t is more or less cavernous, and full of vuggs, which occasionally contain
                   'mall stalactitic forms.   A great deal of     it,  however,  is  laminated in
                   xtremely thin layers, which are sometimes      not thicker than a sheet of
                   >asteboard, and the lamina?   being of different colors, this makes it  very
                   liandsome when polished.     It can also be got out here in large pieces,
                   though there   is  a  good deal of waste.  The counter in the office of the
                   Id  "  Chronicle  "  building, at the corner of Bush and Kearny Streets, is
                   aid to be made of     it,  as well as some mantel-pieces in both the Palace
                    nd the Baldwin Hotels.      The delicate laminae    are often wavy, thus
                   dding much to its beauty.      Other portions of the rock are of     a  some-
                  jvhat  translucent,  milk}^  white, which  is  also handsome when polished.
                   [This  is  the largest deposit of this beautiful, ornamental stone at present
                    nown to the writer to exist within the State.
                     One small spring yet remains at the southern edge of the deposit, dis-
                  charging   a  very little water, which  is  extremely salt and supersaturated
                   ;vith carbonic acid, and which still continues to slowly form         a  little
                   leposit of aragonite.  The knoll has been      a  good deal shattered, and is
                   traversed in various directions by large cracks, which have probably
                  oeen produced by earthquakes at some time in the past.
   716   717   718   719   720   721   722   723   724   725   726