摘要
Geological mapping was undertaken to determine the stratigraphy and potential landslide sites along Mt. Can-abag in St. Bernard, Philippines, where a disastrous landslide occurred in February 2006. The area is underlain by a sequence of NW- to SW-dipping breccias, sandstones and mudstones, with andesite intrusions. The low permeability of the mudstones, which form an aquiclude and hence confined aquifers, results in the build-up of pore pressures. Although the strata dip into the hillside, the fault-created discontinuities mean that the NE-facing slope of Mt. Can-abag is prone to wedge failures.