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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). Sonce 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 instruments were deployed olong 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. #Early results from borehole array.  A number of earthquakes have been detected with the new borehole instruments. As our processing and analysis methods develop, we envisage that much smaller events will emerge from the data.   ##2014-10-10UTC10:20, near Korumburra, Estimated magnitude:  ##2014-10-10UTC10:20, near Korumburra, Estimated magnitude:  ##2014-10-17UTC08:13, near Moe, Estimated magnitude: 3.2