Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 1 - By Alexander Von Humboldt And Aime Bonpland.
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The
Astringent Juice, Known In Commerce By The Name Of Dragon's Blood,
Is, According To The Inquiries We Made On The Spot, The Produce Of
Several American Plants, Which Do Not Belong To The Same Genus And
Of Which Some Are Lianas.
At Laguna, toothpicks steeped in the
juice of the dragon-tree are made in the nunneries, and are much
extolled as highly useful for keeping the gums in a healthy state.)
On leaving Orotava, a narrow and stony pathway led us through a
beautiful forest of chestnut trees (el monte de Castanos), to a
site covered with brambles, some species of laurels, and
arborescent heaths. The trunks of the latter grow to an
extraordinary size; and the flowers with which they are loaded form
an agreeable contrast, during a great part of the year, to the
Hypericum canariense, which is very abundant at this height. We
stopped to take in our provision of water under a solitary
fir-tree. This station is known in the country by the name of Pino
del Dornajito. Its height, according to the barometrical
measurement of M. de Borda, is 522 toises; and it commands a
magnificent prospect of the sea, and the whole of the northern part
of the island. Near Pino del Dornajito, a little on the right of
the pathway, is a copious spring of water, into which we plunged
the thermometer, which fell to 15.4 degrees. At a hundred toises
distance from this spring is another equally limpid. If we admit
that these waters indicate nearly the mean heat of the place whence
they issue, we may fix the absolute elevation of the station at 520
toises, supposing the mean temperature of the coast to be 21
degrees, and allowing one degree for the decrement of caloric
corresponding under this zone to 93 toises. We should not be
surprised if this spring remained a little below the heat of the
air, since it probably takes its source in some more elevated part
of the peak, and possibly communicates with the small subterranean
glaciers of which we shall speak hereafter. The accordance just
observed between the barometrical and thermometrical measures is so
much more striking, because in mountainous countries, with steep
declivities, the springs generally indicate too great a decrement
of caloric, for they unite small currents of water, which filtrate
at different heights, and their temperature is consequently the
mean between the temperature of these currents. The spring of
Dornajito has considerable reputation in the country; and at the
time I was there, it was the only one known on the road which leads
to the summit of the volcano. The formation of springs demands a
certain regularity in the direction and inclination of the strata.
On a volcanic soil, porous and splintered rocks absorb the rain
waters, and convey them to considerable depths. Hence arises that
aridity observed in the greater part of the Canary Islands,
notwithstanding the considerable height of their mountains, and the
mass of clouds which navigators behold incessantly overhanging this
archipelago.
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