Abstract
original pebble shape, studies were made of angular material shed from a limestone outcrop upon the beach near the Ure River, Marlborough, New Zealand (King, 1936a). Here only two opposite wind directions along the beach could be effective for sandblasting. Material was studied at all stages from freshly shed fragments to superbly faceted dreikanter and pyramidalgeschiebe. The conclusion was reached that, with angular material, original shape exercised considerable control over the final form as-
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