Natural phenomena that cause major problems around the world
Landslides
Ground movement on a slopingterrain, aggravatedbyrain because water is a naturalagent of erosion
Come in various names such as mudslides, flashfloods, avalanches, the actual difference is in their composition
Types of Landslide
Soil Creep Landslide
Slumping Landslide
Debris Flow Landslide
Rock Fall Landslide
Soil Creep Landslide
Veryslow downslopemovementofparticles that occurs in every slope covered with loose, weathered material
Slumping Landslide
Downwardmovementofrockdebris, usually the consequence of removal of buttressing earth at the foot of a slope of uncosolidated material
Debris Flow Landslide
Happens when slopebecomessaturatedwithwater which then triggers a landslide of water-soaked mass of rock and soil that slides down the slope
Rock Fall Landslide
Suddenslidescaused by heavyrain, the rocks on the slope loosens and then slides down the slope
Sinkhole
Topographicdepression created when groundwaterdissolvestheunderlyinglimestone bedrock, often known as "sink" and "doline"
Types of Sinkhole
CoverCollapse Sinkhole
CoverSubsidence Sinkhole
Dissolution Sinkhole
Artificial Sinkhole
CoverCollapseSinkhole
Develops suddenly (over an hourperiod) thus, causing catastrophicdamage
Cover Subsidence Sinkhole
Graduallygrows where the sediment covers are permeable and contain sand
Dissolution Sinkhole
Occurs in areas where calcareous is exposed on the ground or where thin layers of soil and permeable sand are also covered, limestone or dolomitedissolution is most intense when the water first reaches the rock surface
Artificial Sinkhole
Such types of sinks may be caused by varioushuman activities, including groundwaterpumping and building
Causes of Geologic Hazards (Landslides)
Climate
Earthquakes
Weathering
Erosion
VolcanicEruption
ForestFires
Gravity
Mining
ClearCutting
Rainfall-Induced Landslides
Climate
A general reduction of precipitation leads to a lowering of the water table and a reduction in the overall weight of soil mass
Weathering
The naturalprocedure of rockdetoriation that leads to landslide, brought about by the chemical action of water, air, plants and bacteria
Erosion
Caused by sporadicrunningwater wiping out latent and lateral slope support enabling landslides to occur easily, continues to shape the planet's landscape today
Volcanic Eruption
If an eruption occurs in a wet condition, the soil will start to move downhill instigating a landslide
Forest Fires
Burnsvegetation that holds soil in place
Gravity
Steeper slopes coupledwithgravitationalforce can trigger massive landslides
Mining
Vibrationemanating from the blasts can weaken soils in other areas susceptible to landslides
Clear Cutting
A technique of timber harvesting that eliminates all old trees from the area
Rainfall-Induced Landslides
The mostcommon and widespread damaging landslide
Causes of Geologic Hazards (Sinkhole)
Dissolution of Sedimentary Rocks
UndergroundWaterPumpings
DissolutionofSedimentaryRocks
When these rocks are dissolved, it can either form a void of water or air
UndergroundWaterPumpings
Pumping water underneath the ground causes drainage to alter its flow which causes the soil to be eroded by water
Warning Signs of an Impending Landslide
EarlierLandslideasIndicator
TensionCracks
ThingsMoving
WaterDoingSomethingDifferent
Warning Signs of an Impending Sinkhole
Trees or fence posts that tilt or fall
Foundations that slant
Cracks in the ground
Sudden drainage of a pond
Sinkholes in the neighborhood
New or widening cracks
Cracked grout between tiles
Cracked tiles
Earthly odor in the home after rain
Wilted vegetation in a limited area
Geological Maps
Shows how geological features, rock units, or geologic strata are shownbycolors or symbols to indicate where they are exposed at the surface
TopographyonMaps
The shapes of the hills and dales are depicted on the map by fine lines that are contours-lines of actual elevation
Landslide colors
Brown (Very high landslide susceptibility)
Red (High landslide susceptibility)
Green (Moderate landslide susceptibility)
Yellow (Low landslide susceptibility)
Stripes (Debrisflow / Possibleaccumulationzone)
Flood colors
Dark Blue (Veryhigh flood susceptibility)
Dark Purple (High flood susceptibility)
Neon Purple (Moderate flood susceptibility)
Pastel Purple (Low flood susceptibility)
Programs That Intensify Nation's Hazard Mitigation Capabilities
Protectionof Schools and Hospitals
Adoptionof Nonconstructural Measures
Incorporationof Mitigation Into New Development
ProtectionofCulutral Properties
Protection of Natural Resources
Government Leadership of Mitigation Implementation