Earthquakes
The characteristics of an earthquake
"The Earth’s surface is not fixed; on the contrary, it is in constant movement. This activity is especially visible along large fractures in the Earth’s crust, known as faults. An earthquake occurs when there is a sudden fracture or movement of rocks under the Earth’s surface. This sudden rupture releases energy that has accumulated due to the movement of the Earth near these faults."
The main types of fault
Earthquakes in the Caribbean, are mainly due to the movement of the subduction of two tectonic plates, the plate in North America (less dense), sinking under the plate and the Caribbean (more dense). In this subduction zone, the oceanic plate dives causes a compression of the crust on the surface. This compression translates mechanically by faults in the reverse (the upper compartment rises relative to the lower compartment).
The location of the fracture's depth is called the hypocenter. Vibrations are released and spread throughout the area by seismic waves. These waves sometimes shake the ground and can damage structures. The point at which the earthquake is the most powerful, relative to the surface of the Earth, is called the epicenter.
Richter scale
The classification of earthquakes according to the Richter scale
The Richter scale measures the magnitude of an earthquake, that is to say, the energy released at the focus of the earthquake.
Source : Booklet teacher-cycle 4 – Project "Pare pa Pare" – French Red Cross – 2024
For more information :
Interactive Map – The University of The West Indies Seismic Research Centre Interactive map live earthquakes in the Caribbean – University of the West Indies
Earthquake | Geohazards (French) Guide, explanations, practice sheets and French schemes earthquake – Geohazard
Earthquakes | The UWI Seismic Research Centre (English) Explanation of the formation of earthquakes in the Caribbean University of the West Indies
CDEMA Earthquake (English) Information, preparation guide and resources on earthquakes – CDEMA
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