Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 3 - By Alexander Von Humboldt And Aime Bonpland.
- Page 239 of 332 - First - Home
Finally, The Latter Chain, To Which I Have
Given The Designation Of Central, After Forming The Rapids And
Cataracts Of
The Amazon, between Tomependa and San Borja, turns to
north-north-west, and joins the western chain, that of Caxamarca,
Or
the Nevados of Pelagatos and Huaylillas, and forms the great knot of
the mountains of Loxa. The mean height of this knot is only from 1000
to 1200 toises: its mild climate renders it peculiarly favourable to
the growth of the cinchona trees, the finest kinds of which are found
in the celebrated forest of Caxanuma and Uritusinga, between the Rio
Zamora and the Cachiyacu, and between Tavacona and Guancabamba. Before
the cinchona of Popayan and Santa Fe de Bogota (north latitude 2 1/2
to 5 degrees), of Huacarachuco, Huamalies and Huanuco (south latitude
9 to 11 degrees) became known, the group of the mountains of Loxa had
for ages been regarded as the sole region whence the febrifuge bark of
cinchona could be obtained. This group occupies the vast territory
between Guancabamba, Avayaca, Ona and the ruined towns of Zamora and
Loyola, between latitude 5 1/2 and 3 1/4 degrees. Some of the summits
(the Paramos of Alpachaca, Saraguru, Savanilla, Gueringa, Chulucanas,
Guamani, and Yamoca, which I measured) rise from 1580 to 1720 toises,
but are not even sporadically covered with snow, which in this
latitude falls only above 1860 to 1900 toises of absolute height.
Eastward, in the direction of the Rio Santiago and the Rio de Chamaya,
two tributary streams of the Amazon, the mountains lower rapidly:
between San Felipe, Matara, and Jaen de Bracamoros, they are not more
than 500 or 300 toises.
As we advance from the mica-slate mountain of Loxa towards the north,
between the Paramos of Alpachaca and Sara (in latitude 3 degrees 15
minutes) the knot of mountains ramifies into two branches which
comprehend the longitudinal valley of Cuenca. This separation
continues for a length of only 12 leagues; for in latitude 2 degrees
27 minutes the two Cordilleras again re-unite in the knot of Assuy, a
trachytic group, of which the table-land near Cadlud (2428 toises
high) nearly enters the region of perpetual snow.
The group of the mountains of Assuy, which affords a very frequented
pass of the Andes between Cuenca and Quito (latitude 2 1/2 to 0
degrees 40 minutes south) is succeeded by another division of the
Cordilleras, celebrated by the labours of Bouguer and La Condamine,
who placed their signals sometimes on one, sometimes on the other of
the two chains. The eastern chain is that of Chimborazo (3350 toises)
and Carguairazo; the western is the chain of the volcano Sangay, the
Collanes, and of Llanganate. The latter is broken by the Rio Pastaza.
The bottom of the longitudinal basin that bounds those two chains,
from Alausi to Llactacunga, is somewhat higher than the bottom of the
basin of Cuenca. North of Llactacanga, 0 degrees 40 minutes latitude,
between the tops of Yliniza (2717 toises) and Cotopaxi (2950 toises),
of which the former belongs to the chain of Chimborazo, and the latter
to that of Sangay, is situated the knot of Chisinche; a kind of narrow
dyke that closes the basin, and divides the waters between the
Atlantic and the Pacific.
Enter page number
PreviousNext
Page 239 of 332
Words from 125071 to 125622
of 174507