G20
Old Landslide Scarp
A very steep gradient and highly fractured lithology of the area are significant factors contributing to these old mass movements. Evident in three crescent-shaped scars on the cliff face, now covered with tall grasses…
Official site
Geosite G20
Location
Mount Apo Geopark
Classification
Geological heritage site
Coordinates
Not yet recorded
Discover the site
A very steep gradient and highly fractured lithology of the area are significant factors contributing to these old mass movements. Evident in three crescent-shaped scars on the cliff face, now covered with tall grasses that marks the historic landslide events
Continue exploring
