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The flood-streams setting to the westward through Banks Strait, and to the south-westward past the north-west end of Flinders, meet about ten miles to the westward of the Chappell Isles, when their united stream curves round by south to west, becoming gradually weaker, and soon after passing the mouth of the Tamar ceasing to be felt at all, leaving in the middle of Bass Strait a large space free from tidal influence as far as the production of progressive motion is concerned, that given to it from the entrances being neutralized by their mutual opposition.
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