Earth's crust consists of large and smaller plates, with oceans and land masses being carried on plates. The Caribbean Plate is one of the smaller plates
Plate margins or boundaries result in various tectonic activities when one plate meets another, making the Caribbean a hotspot for volcanic and seismic activity
Scientists discovered that new crust was being formed at certain places on Earth's surface, and plate margins are formed due to convection currents in the mantle
Plates that move away from each other, resulting in a line of submarine volcanoes and fissures. Sea-floor spreading was first detected at these margins, leading to the development of plate tectonics
Crust is being consumed or pushed back into the mantle through subduction. Plates collide and one plate rides over the other, forcing it downwards into the subduction zone. This friction generates immense heat, melting crustal rocks and molting the rock material
The Caribbean Plate is an oceanic tectonic plate beneath Central America and the Caribbean Sea, bordered by the North American, South American, and Cocos plates
The convergent margin along the Lesser Antilles is a double island arc with mountainous, volcanic islands in the inner arc and flat, low-lying limestone islands in the outer arc
The eastern boundary of the Caribbean Plate is a subduction zone where the North and South American plates subduct beneath the Caribbean plate, forming volcanic islands like the Lesser Antilles
The southern boundary of the Caribbean Plate interacts with the South American plate, forming Trinidad on the South American plate and Tobago on the Caribbean plate
The presence of deep ocean trenches off Cayman, Puerto Rico, and Hispaniola indicates major plate boundaries with the potential for serious earthquakes of 7.5 and higher
The meeting of convergent and transform margins at the southern margin of the Caribbean Plate is responsible for the extreme faulting and unstable nature of rocks in Trinidad and northern Venezuela
To help combat the negative impacts, individual countries invest in local offices and regional bodies, such as the Caribbean Disaster Emergency Management Agency (CDEMA), that coordinates emergency management systems
Occur when rocks release energy due to pressure build-up, such as plates colliding, sliding past each other, or being pushed away by upwelling magma. This energy can cause extreme displacement of rocks, often leaving trenches along fault lines, which can have adverse consequences for populations and ocean floor
If a major shift occurs, a tsunami can develop. Earthquakes leave fractures or faults in rocks, indicating weaknesses and potential future earthquakes. Major faults at plate margins, such as in the Caribbean, indicate weak rocks and crustal instability
A mathematical calculation used to measure earthquake magnitude, but most geologists and volcanologists now use the moment magnitude scale (MMS). An earthquake measuring 5.0 on the MMS is ten times stronger than one measuring 4.0
Minor earthquakes are below 5.0, and destructive ones occur above 6.0. The largest recorded earthquake was in Chile in 1960, with a magnitude of 9.5 MMS
Prediction efforts have made progress, for example in in China, observations such as water level in deep wells, unusual animal behavior, and radioactive gas presence have been used to predict some earthquakes. However, it is not a precise science, as it is impossible to predict the epicenter of an earthquake
An opening in the Earth's crust allows ash, lava, steam and hot gases to escape to the surface, creating a dangerous atmosphere. Over time these eruptions build a cone shaped mountain
Before volcanic eruptions occur, there is usually some kind of warning of increased volcanic activity, such as a tremor. In the Eastern Caribbean, along the volcanic island arc, active volcanoes have been erupting for hundreds of years
Eruptions can vary from just a little steam to a few years of deadly pyroclastic flows. Sometimes major towns are destroyed (such as Plymouth, the capital of Montserrat, in 1995)
In Montserrat, the Soufrière Hills volcano started erupting in 1995. This caused an emergency evacuation of parts of the islands, including its capital and main port, Plymouth, and then, following the permanent disruption to economic and day-to-day life on the island, led to the migration of most of the population to Great Britain
Volcanic rocks over a period of time form highly fertile soils with minerals that plants require, thus encouraging agriculture in high-risk areas and future abundant yields of crops
Most of the metallic mineral mined in the world – gold, silver, copper, lead, zinc are associated with magmas found deep within the roots of extinct volcanoes
Poisonous gases around the volcanic vent and aid rain prevent plant growth. This leads to the destruction of the agricultural sector and export sectors
Ash fallout damages plants and crops by blocking out sunlight and causes a high incidence of sickness and respiratory ailments
Damage to beaches or vegetation resulting from lava flows and possible damage to coral and marine ecology affects tourism and the fishing industry
Migration of people from the country at risk to other regional countries or to the metropole
Volcanic rocks over a period of time form highly fertile soils with minerals that plants require, thus encouraging agriculture in high-risk areas and future abundant yields of crops. It contributes to the production of abundant food and civilization.
Most of the metallic mineral mined in the world – gold, silver, copper, lead, zinc are associated with magmas found deep within the roots of extinct volcanoes.
Migration of people from the country at risk to other regional countries or to the metropole
For example, the Montserrat disaster of 1995 caused forced migration, both internal (to other areas of the country) and external (such as to the UK). The former led to competition for or insufficient infrastructure and social services.