Downward ground movement on a sloping terrain caused by gravity
Also known as landslip
Landslide formation
1. Bare vegetation
2. Inclined location
3. Heavy rain
Sinkhole
Topographic depression created when groundwater dissolves the underlying limestone bedrock
Sinkholes
Occur in areas where the soil foundation is made of soft minerals and rocks such as limestone, salt beds, or any acidic rocks
Depth ranges from a couple of meters to several miles deep
Sinkhole formation
1. Water from rainfall seeps underneath the soil through cracks and fissures
2. Water erodes the soil and forms a conduit system
3. Void forms, either filled with air or water
Sinkholes cannot only form holes, they can be shallow or deep, and cannot only occur on land
Ideal environment for sinkholes to occur is in areas with limestone, salt beds, or sedimentary deposits, not volcanic craters
Landslides are not the same as earthquakes, which are not topographic depressions created by groundwater dissolving limestone
Landslides can occur on flat ground due to gravity, not just on inclined terrain
The depth of sinkholes ranges from a couple of meters to several miles deep, not just a couple of meters to several miles
Debris Flow Landslides are triggered by the slope becoming saturated with water, not sudden slides caused by heavy rain loosening rock
Rock Fall Landslides are sudden slides caused by heavy rain loosening rock on the slope, not when the slope becomes saturated with water
Soil Creep Landslides involve a very slow downslope movement of particles, not a downward movement of rock debris
Slumping Landslides involve a downward movement of rock debris, usually due to removal of earth at the foot of the slope, not a very slow downslope movement of particles
Sinkholes are depressions in the ground that result from the collapse of the surface layer of soil, not earthquakes
The essential characteristic of rock for producing sinkholes is that it must be soluble, not dense, hard, or lustrous