Abstract
Abstract A preliminary report of the effects recorded at Campbell Island following the nuclear explosion on 9 July 1962 has already been given (Geophysical Observatory, in press). This report was based on an examination by the Observer at the Station. The yearly servicing of the Island has now enabled the recording to be brought back to New Zealand, and they have been compared in detail with those made at Godley Head, near Christchurch. Although the overall behaviour is similar, there are significant points of difference as described below.
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