Referenced Document - OPW20-0037

Mr Andrew Jensen                                                                                  20013-001-Rev0
                                                                                                  4 February 2020




Text Figure 4: Exposed phyllite rock in cutting on southern side of building pad

In the central part of the cutting, there appeared to be an altered zone which was inferred to be associated
with the intrusion of a dyke. The reisdual soil in this area presents as a finer grained, silty clay of very stiff
consistency with the rock noted to be in places extremely weathered (ref. Text Figure 5).




                                               Dyke altered zone




Text Figure 5: Altered zone where dyke appears to have penetrated into phyllite rock in cutting




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