casionally impeded by the additional
weight of the attendant burroqueros holding on by the tail, and laughing
at our efforts to dislodge them. On reaching the shoulder of one of the
hills, we found the ravines and valleys below us filled with dense mist.
Here, at an elevation of 2500 feet, a species of spruce-like pine
appeared to thrive well. The path, which at times is not more than three
feet wide, now winds along the sides of the mountain with many sharp
turnings; heading numerous ravines, the frightful nature of which was
partially concealed by the obscurity of the mist.

We halted at the Pass of the Curral, to which Captain Stanley's
barometrical observations* assign an elevation of 2700 feet above the
sea. Shortly afterwards the mist gradually dissolved, unveiling the
magnificent scenery below and around. The Curral gives one the idea of a
vast crater** of irregular form, surrounded by a rugged wall (upwards of
a thousand feet in height) of grey weather-beaten rock cut down into wild
precipices, intersected by ravines and slopes of debris mixed up with
masses of crumbling rock, and towering upwards into fantastic peaks. A
winding path leads to the bottom--a small fertile valley watered by a
streamlet which leaves it by a deep gorge on the left, and forms a
picturesque waterfall on its way to the sea. The scattered rustic huts
and snow-white chapel of the Curral complete the picture of this peaceful
and secluded spot, buried in the very heart of the mountains.

(*Footnote. The height of the Pico dos Bodes, determined in the usual way
by the mountain barometer, was found by Lieutenant Dayman to be 3677
feet; his observations on the magnetic dip and intensity (for which see
the Appendix) are interesting, as showing a great amount of local
attraction at the summit.)

(**Footnote. There is reason to suppose the Curral to have been the
principal, although not the only centre of that submarine volcanic
action, during the continuance of which Madeira first emerged from the
sea, an event, which the evidence afforded by the limestone fossils of
St. Vincente (on the north side of the island) associates with the
tertiary epoch. See Paper by Dr. J. Macaulay in Edinburgh New
Philosophical Journal for October 1840.)

Although it is now the middle of winter, today's excursion afforded many
subjects of interest to a naturalist. Some beautiful ferns, of which even
the commonest one (Adiantum capillus-veneris) would have been mu