Abstract A new radiocarbon age determination of 3115 +/- 35 yr B.P. has been obtained for a charred wood sample from within a block- and ash-flow deposit at Mount Edgecumbe. Together with reliable dates for Holocene tephra stratigraphy, the new datum leads to a stronger control on the chronology of Mount Edgecumbe and implies that activity continued after the widespread Waimahia Tephra dated at 3280 yr B.P.
Keywords Edgecumbe; radiocarbon age determinations
New Zealand Journal of Geology and Geophysics, 1997, Vol. 40: 559-562
0028-8306/97/4004-0559 $7.00/0 (c) The Royal Society of New Zealand 1997
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