Geological And Other Hazards in Victoria
by Rob Kanen


Current Hazards
Future Hazards

Current Hazards

Geological Hazards

Mt. Dandenong Ranges, Macedon Ranges

Rock and Mud Slides - Steep slopes in these hills are prone to rock and mud slides, especially during heavy rains
Solution - Leave as many trees and vegetation on hill slopes as possible, remove unstable soil

Melbourne Region

Soil and Clay Movement - Melbourne region is prone to soil movement due to shrinkage and expansion of water sensitive clays
Solution - Construct adequate footings and/or slabs to resist soil movement

Coastal Erosion - Bayside coastal areas are currently undergoing erosion due to wave action
Solution - Vegetate coastal areas and replenish shoreline with rock/sand as necessary

Gippsland
Generally same as Melbourne Region

Earthquakes - Earthquakes are common in the Foster/Wilsons Prom and Rosedale Areas as movement occurs along the Foster and Rosedale Fault Systems

Kiewa Valley and Eastern Victoria Mountain Region

Earthquakes - Earthquakes occuring along fault systems i.e. Kiewa Valley Fault System
Rock and Mud Slides

All Victorian Coastal Areas

Coastal Erosion -Coastal areas are currently undergoing erosion due to wave action
Solution - Vegetate coastal areas and replenish shoreline with rock/sand as necessary

Non Geological Hazards

Western Victoria

Drought
Bushfires - in Summer
Electrical Storms - in Summer
Gales - Winter
Dust Storms - Summer
Heat Waves - Summer

Eastern Victoria

Floods - in Winter
Gales - in Winter
Electrical Storms - in Summer
Bushfires - in Summer
Drought - in Summer

Future Hazards

Geological Hazards

All Coastal Regions
We are currently undergoing a phase of sea level rise with all coastal areas undergoing erosion. This is likely to get worse in the future.

Gippsland
Further faulting and earthquakes along the Foster and Rosedale Faults

Eastern Victorian Highlands
Further faulting and earthquakes along major faults ie Kiewa Valley Fault System

Western Victoria
Possible renewed volcanism near Quaternary Scoria Cones and Flood Basalt Plains

Non Geological Hazards

Climate Warming - Due to increased CO2 Levels in atmosphere producing warming effect
Solution - Reduce CO2 emissions to 0% from fossil fuel burning

UV Radiation - Due to ozone depletion from release of chlorofluorocarbons and other pollutants in atmosphere
Solution - Discontinue use of chlorofluorocarbons and other polluting chemicals


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