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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Thus The Crater At The Extremity Of The Piton, Which Is
Called The Caldera, Is Extremely Small.
Its diminutive size struck
M. de Borda, and other travellers, who took little interest in
geological investigations.
As to the nature of the rocks which compose the soil of Teneriffe,
we must first distinguish between productions of the present
volcano, and the range of basaltic mountains which surround the
Peak, and which do not rise more than five or six hundred toises
above the level of the ocean. Here, as well as in Italy, Mexico,
and the Cordilleras of Quito, the rocks of trap-formation* are at a
distance from the recent currents of lava (* The trap-formation
includes the basalts, green-stone (grunstein), the trappean
porphyries, the phonolites or porphyrschiefer, etc.); everything
shows that these two classes of substances, though they owe their
origin to similar phenomena, date from very different periods. It
is important to geology not to confound the modern currents of
lava, the heaps of basalt, green-stone, and phonolite, dispersed
over the primitive and secondary formations, with those porphyroid
masses having bases of compact feldspar,* which perhaps have never
been perfectly liquified, but which do not less belong to the
domain of volcanoes. (* These petrosiliceous masses contain
vitreous and often calcined crystals of feldspar, of amphibole, of
pyroxene, a little of olivine, but scarcely any quartz. To this
very ambiguous formation belong the trappean porphyries of
Chimborazo and of Riobamba in America, of the Euganean mountains in
Italy, and of the Siebengebirge in Germany; as well as the domites
of the Great-Sarcouy, of Puy-de-Dome, of the Little Cleirsou, and
of one part of the Puy-Chopine in Auvergne.)
In the island of Teneriffe, strata of tufa, puzzolana, and clay,
separate the range of basaltic hills from the currents of recent
lithoid lava, and from the eruptions of the present volcano. In the
same manner as the eruptions of Epomeo in the island of Ischia, and
those of Jorullo in Mexico, have taken place in countries covered
with trappean porphyry, ancient basalt, and volcanic ashes, so the
peak of Teyde has raised itself amidst the wrecks of submarine
volcanoes. Notwithstanding the difference of composition in the
recent lavas of the Peak, there is a certain regularity of
position, which must strike the naturalist least skilled in
geognosy. The great elevated plain of Retama separates the black,
basaltic, and earthlike lava, from the vitreous and feldsparry
lava, the basis of which is obsidian, pitch-stone, and phonolite.
This phenomenon is the more remarkable, inasmuch as in Bohemia and
in other parts of Europe, the porphyrschiefer with base of
phonolite* (* Klingstein. Werner.) covers also the convex summits
of basaltic mountains.
It has already been observed, that from the level of the sea to
Portillo, and as far as the entrance on the elevated plain of the
Retama, that is, two-thirds of the total height of the volcano, the
ground is so covered with plants, that it is difficult to make
geological observations. The currents of lava, which we discover on
the slope of Monte Verde, between the beautiful spring of Dornajito
and Caravela, are black masses, altered by decomposition, sometimes
porous, and with very oblong pores. The basis of these lower lavas
is rather wacke than basalt; when it is spongy, it resembles the
amygdaloids* of Frankfort-on-the-Main. (* Wakkenartiger
mandelstein. Steinkaute.) Its fracture is generally irregular;
wherever it is conchoidal, we may presume that the cooling has been
more rapid, and the mass has been exposed to a less powerful
pressure. These currents of lava are not divided into regular
prisms, but into very thin layers, not very regular in their
inclination; they contain much olivine, small grains of magnetic
iron, and augite, the colour of which often varies from deep
leek-green to olive green, and which might be mistaken for
crystallized olivine, though no transition from one to the other of
these substances exists.* (* Steffens, Handbuch der Oryktognosie
tome 1 s. 364. The crystals which Mr. Friesleben and myself have
made known under the denomination of foliated olivine (blattriger
olivin) belong, according to Mr. Karsten, to the pyroxene augite.
Journal des Mines de Freiberg 1791 page 215.) Amphibole is in
general very rare at Teneriffe, not only in the modern lithoid
lavas, but also in the ancient basalts, as has been observed by M.
Cordier, who resided longer at the Canaries than any other
mineralogist. Nepheline, leucite, idocrase, and meionite have not
yet been seen at the peak of Teneriffe; for a reddish-grey lava,
which we found on the slope of Monte Verde, and which contains
small microscopic crystals, appears to me to be a close mixture of
basalt and analcime.* (* This substance, which M. Dolomieu
discovered in the amygdaloids of Catania in Sicily, and which
accompanies the stilbites of Fassa in Tyrol, forms, with the
chabasie of Hauy, the genus Cubicit of Werner. M. Cordier found at
Teneriffe xeolite in an amygdaloid which covers the basalts of La
Punta di Naga.) In like manner the lava of Scala, with which the
city of Naples is paved, contains a close mixture of basalt,
nepheline, and leucite. With respect to this last substance, which
has hitherto been observed only at Vesuvius and in the environs of
Rome, it exists perhaps at the peak of Teneriffe, in the old
currents of lava now covered by more recent ejections. Vesuvius,
during a long series of years, has also thrown out lavas without
leucites: and if it be true, as M. von Buch has rendered very
probable, that these crystals are formed only in the currents which
flow either from the crater itself, or very near its brink, we must
not be surprised at not finding them in the lavas of the peak. The
latter almost all proceed from lateral eruptions, and consequently
have been exposed to an enormous pressure in the interior of the
volcano.
In the plain of Retama, the basaltic lavas disappear under heaps of
ashes, and pumice-stone reduced to powder.
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