strike of the vein, but in the farthest one the striko of the
mineralized zone is about 20 degrees off the trend, thus
suggesting that it may be a different vein from that to the
south. It is reported that the vein has been traced consider-
ably farther, but a total of 500 fect is about the limit that is
assured by present workings. Other zones have been traced
intermittently for a few hundred feet and range up to about 5
feet in width. They have offshoots and irregularities, and on
the Golden Eagle to the southeast there appear to be a number of
mineralized zones of considerable irregularity.

The zones are sparsely mineralized being in places
largely quartz with little sulphides; elsewhere they are made
up of altered volcanics with some quartz and sulphides.

However, in parts of some of the zones there are narrow, high-
grade veins. In the main part of No. 2 zone on the Golden
Eagle that lies south of the shaft the high-grade band is
mainly less than 18 inches and probably averages about 6 inches.
It is fairly well defined and the high-grade material can be
easily separated out by hand sorting. The high-grade band is
present in most of the workings except to the south where it
seems to pinch out. There is no pronounced change in about 50
feet of sinking in the main shaft. In a second parallel but
less well-defined and less steeply dipping zone and possibly
in other irregular zones on the Golden Eagle similar ore was
found. On the Gold claims there is some evidence of similar
very narrow bands of lower grade. The high-grade sections

contain much tetrahedrite and probably polyargerite.

Gold (Cup Section). A series of adits and cuts along the canyon .
wall of Richfield creek for more than 1,000 feet disclose a i
network of irregular, flat veins and lenses with irregular,

oblique veins rising and connecting them. The veins range up

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