Reference Document - MCU24/0143 (As Published)

                    during this period is known to have caused landslides at nearby locations in Cooroy and
                    Cootharaba so could therefore be considered as a ‘triggering’ event.
              »     The slide was observed to be confined along the northern and southern sides by slightly convex
                    ground, or spurs. Such spurs should prevent lateral ‘spread’ of the movement and, hence,
                    would minimise regression of the landslide upslope (towards the northern cabin).




                     Text Figure 11: Oblique drone image of the tiny homes, with insets of active landslide




                      Text Figure 12: Northerly and souterly views of landslide backscarp on 27 May 2025

        It should also be noted that signs of slope instability were observed within steeper ground on other parts
        of the site, particularly near drainage lines, however, assessment of those features was not part of
        Tectonic’s commission.




        4 June 2025
        24378-001-Rev1                                                                                        9 of 12
Document Set ID: 24125427
                  24010296
Version: 1, Version Date: 17/09/2025
                          07/08/2025