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Updated: September 20, 2026
Besides the elevation thus gained by angular displacements, I infer, without any hesitation from the stratified gravel-fringes which gently slope up the valleys of the Cordillera from the gravel-capped plains at their base, which latter are connected with the plains, still covered with recent shells on the coast that this great range has been upheaved in mass by a slow movement, to an amount of at least 8,000 feet.
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