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To me far more probable that during the Pampean period this whole area had commenced slowly rising (and in the cliffs at several different heights we have proofs of the land having been exposed to sea-action at several levels) and that tracts of land had thus been formed of Pampean sediment round the Ventana and the other primary ranges on which the several rodents and other quadrupeds lived and that a stream (in which perhaps the extinct aquatic Hydrochoerus lived) drifted their bodies into the adjoining sea into which the Pampean mud continued to be poured from the north. As the land continued to rise it appears that this source of sediment was cut off; and in its place sand and pebbles were borne down by stronger currents and conformably deposited over the Pampean strata. (FIGURE 15. SECTION OF BEDS.
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