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The watershed between the Catarman and Calbayot is formed by the Salta Sangley already mentioned, a flat ridge composed of banks of clay and sandstone, which succeed one another ladder-wise downwards on both its sides, and from which the water collected at the top descends in little cascades. In the most difficult places rough ladders of bamboo are fixed.
I counted fifteen brooks on the north-east side which feed the Catarman, and about the same number of feeders of the Calbayot on the south-west side.
By means of these two rivers and the short but troublesome road, a communication exists between the important stations of Catarman on the north coast, and Calbayot on the west coast.
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