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We began our descent into this great valley when we left the source of the Bua; and now these low hills, called Ngalé or Ngaloa, though only 100 feet or so above the level we had left, showed that we had come to the shore of an ancient lake, which probably was let off when the rent of Kebra-basa on the Zambesi was made, for we found immense banks of well-rounded shingle above or, rather, they may be called mounds of shingle all of hard silicious schist with a few pieces of fossil-wood among them.
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