On a global tectonic scale, movement of the Caribbean and the North American plates were responsible for the Haitian earthquake.
However on a subregional tectonic scale, there is a smaller plate that separates the Caribbean and the North American plates known as the Gonave micro-plate on which Haiti is partly situated (on the eastern end).
The Gonave micro-plate is bounded to the north by the Oriente and Septentrional Fracture Zones and to the south by the Enriquillo-Plantain Garden fault, movement on which caused the magnitude 7 Haitian earthquake on the 12th of January 2010.
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The Haitian earthquake in 2010 was caused by a slip along a previously unknown fault called the Enriquillo-Plantain Garden fault zone. It is a strike-slip fault that runs along the boundary between the Caribbean and North American tectonic plates.
The Haiti earthquake in 2010 was caused by movement along the Enriquillo-Plantain Garden fault zone, which runs along the border of the North American and Caribbean tectonic plates. Specifically, the earthquake was the result of a slip along a blind thrust fault within this fault zone, rather than movement between distinct tectonic plates.
The Assisi earthquake in 1997 was caused by the seismic activity along the Apennine fault line that runs through central Italy. The movement of tectonic plates beneath the Earth's surface caused a sudden release of energy, resulting in the earthquake.
The 2008 earthquake in China, known as the Wenchuan earthquake, was caused by the sudden release of stress accumulated along a fault line due to the movement of the tectonic plates in the region. The seismic activity in the area is influenced by the collision of the Indian Plate with the Eurasian Plate.
An earthquake occurs when there is a sudden release of energy in the Earth's crust, causing the ground to shake. This release of energy is usually caused by the movement of tectonic plates along faults. As the plates try to move past each other, stress builds up until it is released in the form of an earthquake.
The Haitian earthquake was caused by the faultline the country sits on.
The Haitian earthquake that occurred in January 2010 was caused by a transform boundary where two tectonic plates were sliding past each other. For more information please see the related question.
Tha Haitian Earthquake was caused by the transform boundary between the Caribbean and the North American plates. Please see the related question for mor information about the Haitian Earthquake.
No. The Haitian earthquake was caused by a transform boundary.
The earthquake in Haiti in January 2010 was caused by the movement of the Caribbean and North American tectonic plates along the Enriquillo-Plantain Garden fault zone, which is a strike-slip fault boundary. This movement resulted in a magnitude 7.0 earthquake that devastated the region.
The Haitian earthquake occurred on January 12, 2010, and lasted for just a few seconds. However, its impact caused widespread devastation, with over 200,000 people losing their lives and millions more displaced.
The Haitian earthquake in 2010 was caused by a slip along a previously unknown fault called the Enriquillo-Plantain Garden fault zone. It is a strike-slip fault that runs along the boundary between the Caribbean and North American tectonic plates.
PLATES
the tectonic plates
The North American and Caribbean tectonic plates caused the Haiti earthquake in 2010. The movement along the boundary between these two plates resulted in the devastating earthquake.
The tectonic plates moving, transform.
The Richter or local magnitude scale of the Haitian earthquake has been reported as 7.2. However the Richter Magnitude Scale is no longer the formal scale used for reporting earthquake magnitude having been replaced by the Moment Magnitude Scale.As such, the official strength of the January 12, 2010, quake on the Moment Magnitude Scale was 7.0, as reported by the U.S. Geological Survey, National Earthquake Information Center.Please see the related questions for further information about the Haitian earthquake and it's magnitude and severity.