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The Suzuki Brezza (known as Vitara Brezza for the first generation) is a subcompact crossover SUV from Suzuki and manufactured by Maruti Suzuki in India. The Brezza is the first Suzuki-branded car which was fully developed in India. [2] [3] The model was designed as a smaller alternative to the global market Vitara and targeted to young audiences.
2016 Vitara Brezza. In 2016, Suzuki released a smaller derivative of the fourth-generation Vitara destined for the Indian market as the Vitara Brezza, which occupied the sub-4-metre SUV segment in the country. The model was only produced in India with right-hand drive configuration. It was renamed to simply Brezza since the second-generation model.
The Gonâve microplate, showing the fault zones that bound it. The Gonâve microplate forms part of the boundary between the North American plate and the Caribbean plate.It is bounded to the west by the Mid-Cayman Rise spreading center, to the north by the Septentrional-Oriente fault zone and to the south by the Walton fault zone and the Enriquillo–Plantain Garden fault zone.
The Gonâve microplate, showing location of the main fault zones. The Septentrional–Orient fault zone (SOFZ) is a system of active coaxial left lateral-moving strike slip faults that runs along the northern side of the island of Hispaniola where Haiti and the Dominican Republic are located and continues along the south of Cuba along the northern margin of the Cayman Trough.
Within the trough is a slowly spreading north–south ridge which may be the result of an offset or gap of approximately 420 kilometres (260 mi) along the main fault trace. The Cayman spreading ridge shows a long-term opening rate of 11–12 mm/yr. [ 4 ] The eastern section of the trough has been named the Gonâve Microplate .
The EPGFZ shares approximately half of the relative motion between the North American and Caribbean tectonic plates with the Septentrional-Oriente fault zone which runs along the northern side of Hispaniola. Both faults merge into the Cayman Trench to the west. The fault accommodates about 20.6±1.66 millimeters of lateral motion per year (mm ...
To map the subduction zone, researchers at sea performed active source seismic imaging, a technique that sends sound to the ocean floor and then processes the echoes that return. The method is ...
The Polochic fault (also referred to as the Chixoy-Polochic Fault) lies north and parallel to the Motagua Fault and shares some of the motion between the North American and Caribbean plates. [1] Studies of GPS displacement of the zone reveal that the motion of the North American / Caribbean plate Boundary is, for the most part, accommodated by ...