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Mike Sandiford edited Introduction.md
over 9 years ago
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The first surface instruments were installed in 2012, in the month prior to the M 5.4 Moe earthquake (2012-06-19:10:56). Since then, the seismic array has grown, with extra stations built near Fish Creek, Willow Grove, Loch, expanding the effective size of the network.
In October 2014, 3
borhole borehole instruments were deployed
olong along the Strzelecki hills, at depths of ~130 m. These instruments increase the spatial resolution of the Gipplsand array, and offer a chance to monitor microseismiciy that might otherwise go undetected.