The History of Cuba, vol. 5Johnson, Willis Fletcher
History
The History of Cuba, vol. 5
Johnson, Willis Fletcher
Cuba -- Economic conditions; Cuba -- History
While the main chain, or mountainous vertebrae, seems to disappear in
the Sierra de Cubitas of Camaguey, it reappears again, just west of the
Bay of Manati, in the extreme northern part of the province, and extends
along the north shore at broken intervals, until it finally melts into
that great eastern nest of volcanic upheavals that forms the eastern end
of the Island. From this north shore chain, innumerable spurs are thrown
off to the southward between Manati and Nipe Bay, reaching sometimes
twenty-five or thirty miles back into the interior.
[Illustration: A MOUNTAIN ROAD, ORIENTE]
Along the southern shore of Oriente from Cabo Cruz to Cabo Maysi,
ascending at times abruptly from the beach, and at others dropping back
a little, we have the longest and tallest mountain range of Cuba. One
peak, known as Turquino, located midway between the city of Santiago de
Cuba and Cape Cruz, reaches an altitude of 8,642 feet.
From the crest of this range, known as the Sierra Maestra, the great
network of spurs are thrown off to the north toward the valley of the
Cauto, while between these mountain offshoots several of the Cauto’s
most important tributaries, including the Cautill, Contraemaestre and
Brazos del Cauto, have their sources.
Most of the mountainous districts are still covered with dense tropical
forests that contain over three hundred varieties of hard woods, the
cost of transportation alone preventing their being cut and marketed.
The interior of the Province, from the Mayari River west, is the largest
valley in Cuba, with a virgin soil marvellously rich through which runs
the Cauto River, emptying into the Caribbean Sea, a little north of the
City of Manzanillo. This stream, with its tributaries, forms the most
extensive waterway in the Island.
A tributary on the north known as the Rio Salado, rising south of the
city of Holguin, flows in a westerly direction and empties into the
Cauto just above the landing of Guamo, some fifteen miles from the
Caribbean. Small streams empty into all of the numerous deep water gulfs
and bays that indent the north coast of Oriente. Each serves its purpose
in draining adjacent lands, but none, with the exception of the Mayari,
is navigable. This stream, the most important perhaps of the north
coast, rises in the eastern center of the Province, cutting its way west
along the base of the Crystal Mountains, until it reaches their western
end, whence it makes a sharp turn to the north, and after tumbling over
the falls, gradually descends and empties into Nipe Bay.
The Sagua de Tanamo and its tributaries drain quite a large basin east
of the Mayari, and empty into the Gulf of Tanamo. The Moa, a short
stream, rises not far from the Tanamo but flows north to the ocean. The
Toa, flowing east, cuts through valleys for fifty miles, and finally
empties into the Atlantic thirty miles west of Cape Maysi.
Public-domain text, read in full here on John Shaqi.
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