as gneiss-granite. Nothing can be more striking than
the effect of these huge rounded masses of naked rock rising
out of the most luxuriant vegetation.

I was often interested by watching the clouds, which,
rolling in from seaward, formed a bank just beneath the
highest point of the Corcovado. This mountain, like most
others, when thus partly veiled, appeared to rise to a far
prouder elevation than its real height of 2300 feet. Mr.
Daniell has observed, in his meteorological essays, that a
cloud sometimes appears fixed on a mountain summit, while
the wind continues to blow over it. The same phenomenon
here presented a slightly different appearance. In this case
the cloud was clearly seen to curl over, and rapidly pass
by the summit, and yet was neither diminished nor increased
in size. The sun was setting, and a gentle southerly breeze,
striking against the southern side of the rock, mingled its
current with the colder air above; and the vapour was thus
condensed; but as the light wreaths of cloud passed over
the ridge, and came within the influence of the warmer
atmosphere of the northern sloping bank, they were immediately
re-dissolved.

The climate, during the months of May and June, or the
beginning of winter, was delightful. The mean temperature,
from observations taken at nine o'clock, both morning
and evening, was only 72 degs. It often rained heavily, but
the drying southerly winds soon again rendered the walks
pleasant. One morning, in the course of six hours, 1.6 inches
of rain fell. As this storm passed over the forests which