Robert Biek presents several comments on our paper related to the interpretation of the extent of landslides 1 and 3 on the southern slopes of the Traverse Mountains, Utah (Hart et al., 2012, Figure 7). The limits of landslide 2 are shown as precisely as possible as mapped by Biek (2005).

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Based on geomorphic criteria, the area of Biek's landslide 1 (Qls?1) was increased and extended to the east slope of Maple Hollow. This modification should have been indicated in the figure caption. The landslide limits were not verified by subsurface investigation, and accordingly the landslide is...

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