Abstract The use of the Schmidt hammer for the relative-age dating of boulder and bedrock surfaces is outlined. Two examples of the application of the Schmidt hammer for the dating of Holocene moraines in Mt Cook National Park, Southern Alps, New Zealand, confirm the potential of this method. With this technique it is possible to differentiate between Holocene moraines of different age (especially those built up since c. 5000 yr BP). The results show partial differences to those obtained from other dating techniques in previous work.
Keywords Schmidt hammer; relative-age dating; Holocene; glacier variations; Southern Alps; New Zealand
G03030; Received 9 September 2003; accepted 1 March 2004; Online
publication date 23 March 2005
New Zealand Journal of Geology & Geophysics, 2005, Vol. 48:
105–116
0028–8306/05/4801–0105 © The Royal Society of New Zealand 2005
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