A ground movement on a sloping terrain, where gravity induces the land to move downward. The hazard of landslide can be induced further or aggravated by rain.
Depressions or holes on the ground that resulted from the collapse of the surface layer of the soil, occurring in areas where the soil foundation is made of soft minerals and rocks (limestone, salt beds, or any acidic rock)
Springs, water seepage, or water saturated grounds in areas that are not typically wet
Soil that loosens and moves away from foundations
New cracks or unusual bulges on cemented ground or walls
Underground utility lines that are broken due to vibrations or tremors from the surface of the ground
Buildings, poles, walls, and fences that are leaning
Sudden rapid flow of creek waters carrying more silted water
For sinkholes, signs of an imminent danger in groundwater that does not provide the same amount and quality as before or has become cloudy, acidic, silted or soiled
Sign post or poles that are suddenly leaning, slumping, sagging, slanting, or bent
Ponds that have recently formed or puddles that grow or have never disappeared
Areas that have the highest vulnerability to rainfall-induced geologic hazards have already been identified by the MGB of the Department of Environment and Natural Resources (DENR) through their Geohazard Mapping and Assessment Program.