olume of vapor
issuing from it. The soil from which this vapor issues is an extremely
white earth; it is sometimes thrown up to the height of a yard or a
yard and a half, and meeting the lower temperature of the atmosphere
falls to the ground in small pieces."--Estado geograph., 1865.
[66] Pigafetta says that the natives, in order to obtain palm-wine,
cut the top of the tree through to the pith, and then catch the sap
as it oozes out of the incision. According to Regnaud, Natural History
of the Coco-tree, the negroes of Saint Thomas pursue a similar method
in the present day, a method that considerably injures the trees and
produces a much smaller quantity of liquor. Hernandez describes an
indigenous process of obtaining wine, honey, and sago from the sacsao
palm, a tree which from its stunted growth would seem to correspond
with the acenga saccharifera. The trees are tapped near the top, the
soft part of the trunks is hollowed out, and the sap collects in this
empty space. When all the juice is extracted, the tree is allowed to
dry up, and is then cut into thin pieces which, after desiccation in
the sun, are ground into meal.
[67] Pigafetta mentions that the natives were in the habit of making
oil, vinegar, wine, and milk, from the coco-palm, and that they drank
a great deal of the wine. Their kings, he says, frequently intoxicated
themselves at their banquets.
[68] A number of the Illustrated London News, of December, 1857,
or January, 1858, contains a clever drawing, by an accomplished
artist, of the mode of travelling over this road, under the title,
"A macadamized road in Manila."
[69] Erd and Picketing, of the United States exploring expedition,
determined the height to be 6,500 English feet (7,143 Spanish),
not an unsatisfactory result, considering the imperfect means they
possessed for making a proper measurement. In the Manila Estado
geographico for 1865, the height is given, without any statement as
to the source whence the estimate is derived, as 7,030 feet. The same
authority says, "the large volcano is extinct since 1730, in which
year its last eruption took place. The mountain burst into flames on
the southern side, threw up streams of water, burning lava, and stones
of an enormous size; traces of the last can be observed as far as the
village of Sariaya. The crater is perhaps a league in circumference,
it is highest on the northern side, and its interior is shaped like
an egg-shell: the depth of
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