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##2014-10-10UTC10:20, near Korumburra, Estimated magnitude: 1.5  One such A small  event near Korumburra (?? add hypocentre, 2014-10-10UTC10:20) provides provided  an opportunity to compare waveformson waveforms on  surface and subsurface instruments. Whilst P-wave arrivals can be easily detected on borehole stations, they are difficult to detect on surface stations. S-waves arrivals from borehole stations will substantially improve event location. Figure 2 shows this event at the nearest borehole station, and Figure 3 shows the corresponding STA/LTA filter response, which is commonly used for automatic event detection. Figure 3 shows the P and S-wave picks from the borehole station furthest from the event.