Reduction of territorial vulnerability
Introduction
Natural threats[1] are a natural phenomenon that can have a negative effect on both humans and the ecosystem. These events can be classified into two broad categories: geophysical and biological.[2] Geophysical hazards comprise geological and meteorological phenomena such as earthquakes, volcanic eruptions, forest fires, cyclones, floods, droughts, avalanches and landslides.[3][4] Biological hazards encompass a diverse set of diseases, infections, infestations and invasive species.
Several of the geophysical threats are related; For example, underwater earthquakes can cause tsunamis, and hurricanes can cause flooding and coastal erosion.[5] Floods and wildfires can be caused by a combination of geological, hydrological, and climatic factors. It is also possible that some natural hazards are intertemporally related.[5][6] A clear example of the difference between a hazard and a natural disaster is that the 1906 San Francisco earthquake was a disaster, while living on a tectonic fault is a threat. Some natural hazards may be caused or may be affected by anthropogenic processes (e.g. land use change, drainage, and construction).[7].
Geological threats
Avalanche
An avalanche occurs when a large mass of snow (or rock) slides down the side of a mountain.[8] Avalanches are an example of a force of gravity whose consistency is granular material. In an avalanche, a large amount of material or mixtures of different types of material fall or slide rapidly under the force of gravity. Avalanches are usually classified by the size or severity of the consequences they leave.[9].
Earthquake
An earthquake is the sudden release of energy stored as lithostatic stress that radiates seismic waves. On the Earth's surface, earthquakes can manifest themselves with a tremor or a movement of the ground; When the earthquake occurs at the bottom of the sea, the displacement of water can cause a tsunami. Most of the world's earthquakes (90%, and 81% of the largest) occur in the 40,000 km-long horseshoe-shaped zone, called the Pacific seismic belt, also known as the Pacific Ring of Fire, which mostly borders the Pacific Plate.[10] Many earthquakes occur each day, few of which are large enough to cause significant damage.