Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 3 - By Alexander Von Humboldt And Aime Bonpland.
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By The
Extraordinary Breadth Of The New Continent, In The 30 And 60 Degrees
North Latitude, The Cordillera Of The Andes, Continually Approaching
Nearer To The Western Coast In The Southern Hemisphere, Is Removed 400
Leagues On The North From The Source Of The Rio De La Paz.
The Andes
of Chile may be considered as maritime Alps,* (* Geognostically
speaking, a littoral chain is not a range
Of mountains forming of
itself the coast; this name is extended to a chain separated from the
coast by a narrow plain.) while, in their most northern continuation,
the Rocky Mountains are a chain in the interior of a continent. There
is, no doubt, between latitude 23 and 60 degrees from Cape Saint Lucas
in California, to Alaska on the western coast of the Sea of
Kamschatka, a real littoral Cordillera; but it forms a system of
mountains almost entirely distinct from the Andes of Mexico and
Canada. This system, which we shall call the Cordillera of California,
or of New Albion, is linked between latitude 33 and 34 degrees with
the Pimeria alta, and the western branch of the Cordilleras of
Anahuac; and between latitude 45 and 53 degrees, with the Rocky
Mountains, by transversal ridges and spurs that widen towards the
east. Travellers who may at some future time pass over the unknown
land between Cape Mendocino and the source of the Rio Colorado, may
perhaps inform us whether the connexion of the maritime Alps of
California or New Albion, with the western branch of the Cordilleras
of Mexico, resembles that which, notwithstanding the depression, or
rather total interruption observed on the west of the Rio Atrato, is
admitted by geographers to exist between the mountains of the isthmus
of Panama and the western branch of the Andes of New Grenada.
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