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four adits, a number of open-cuts and trenches, and natural
exposures for a total distance of over 2,400 feet, from an
elevation of 3,870 feet to 4,625 fect. The fracturing is not
as well confined as at the Mamie and mineralized parts are more
scattered and in the main aggregates a smaller width. As at
the Mamie mineralized section is in part made up of veinlets in
fractures and in part is due to replacement.

In general the minerals in the deposit are erratic.
In the lower adit for 25 feet there is a width of 1 to 2 feet of
vein material which when sorted assayed: gold, 0.18 ounce,
silver, 78.1 ounces a ton; lead, 52.8 per cent; and zinc, 11.3
per cent. Beyond this the deposit is spiit up and there are
only a few small veinlets. For 500 feet up the slope and for
200 feet higher vertically the rocks are well exposed and
mineralization is seen to be spotty and irregular. One good
section 15 to 20 feet long and 12 to 15 inches wide assayed:
gold, 0,13 ounce, silver, 33.7 ounces a ton; copper 1.5 per cent;
lead, 25.6 per cent; zine, 53.6 per cent. At the upper end of
this 500-foot section the mineralized part swings 50 to 100 feet {
off the strike. At the upper limit of this section where No. 2 \s
adit is located the mineralized zone which is 15 feet wide, is .
badly aplit up. Though the mineralized parts of this zone are
as much as 3 feet wide in places, they do aoe maintain this
width and show wide ranges in extent both on the surface and in
160 feet of drifting. Vein widths and other conditions in the

adit (No. 2) do not agree with those on the surface. In 250 feet

to No. 3 adit the deposit as exposed by a few cuts also is

irregular. In places mineralization is sparsely spread out over
15 to 20 feet; at other places it is within a zone of a few feet
and again in places is represented by only a few stringers. The

average width of good grade is probably low as the wide parts are