is so bold that the largest man-of-war could sail
without danger. I remember to have once seen, above the bay of San
Francisco, the sailors of a Mexican brig sitting on the ends of their
topsail yards, and picking the flowers from the branches of the trees as
they glided by.

In that part of the country, which is intersected by mountains, the soil
is almost every where mineral, while the mountains themselves contain
rich mines of copper. I know of beds of galena extending for more than
a hundred miles; and, in some tracts, magnesian earths cover an immense
portion of the higher ridges. Most of the sandy streams of the Shoshone
territory contain a great deal of gold-dust, which the Indians collect
twice a year and exchange away with the Mexicans, and also with the
Arrapahoes.

The principal streams containing gold are tributaries to the
Buonaventura, but there are many others emptying into small lakes of
volcanic formation. The mountains in the neighbourhood of the Colorado
of the West, and in the very country of the Arrapahoes, are full of
silver, and perhaps no people in the world can shew a greater profusion
of this bright metal than these Indians.

The Shoshone territory is of modern formation, at least in comparison
with the more southern countries where the Cordillieres and the Andes
project to the very shores of the ocean. It is evident that the best
portion of the land, west of the Buonaventura, was first redeemed from
the sea by some terrible volcanic eruption. Until about two centuries
ago, or perhaps less, these subterranean fires have continued to
exercise their ravages, raising prairies into mountains, and sinking
mountains and forests many fathoms below the surface of the earth; their
sites now marked by lakes of clear and transparent water, frequently
impregnated with a slight, though not unpleasant, taste of sulphur;
while precious stones, such as topazes, sapphires, large blocks of
amethysts, are found every day in the sand and among the pebbles on
their borders.

In calm days I have often seen, at a few fathoms deep, the tops of pine
trees still standing in their natural perpendicular position. In the
southern streams are found emeralds of very fine water; opals also are
very frequently met with.

The formation of the rocks is in general basaltic, but white, black, and
green marble, red porphyry, jasper, red and grey granite, abound east of
the Buonaventura. Quartz, upon some of the mount