North american and carribbean plate
The Bahamas are a chain of islands that lie between Florida and Haiti.
Haiti is located on the boundary between the Caribbean Plate and the North American Plate. The Caribbean Plate is an oceanic plate, while the North American Plate is a continental plate. This tectonic boundary is part of the complex system of plate movements in the region.
The margin of a continent is determined by the location of its tectonic plate boundaries. Convergent boundaries create subduction zones or mountain ranges, while divergent boundaries form rift valleys or mid-ocean ridges along the margins. Transform boundaries can also influence the shape of a continent's margin by creating strike-slip faults.
Africa and South America have edges that are not all on plate boundaries. For example, the coast of Africa along the Atlantic Ocean is a passive margin, and the edges of South America along the Pacific Ocean have a mix of convergent and transform plate boundaries.
The official name of Haiti is the Republic of Haiti.
because it is very close to a plate margin
Japan sits on top of a destructive plate margin.
i think haiti is located on the carribean plate and is the center of the plate or the edge im not sure
Yes, Eyjafjallajökull volcano is located on the constructive plate margin between the North American Plate and the Eurasian Plate in Iceland.
Haiti is located on the northern edge of the Caribbean plate which is an oceanic plate. Please see the related question for more information.
No,plate margin&plate boundary are not same.plate boundaries are definite regions where tectonic occurs,while margins are surface lines.
Transform boundary
its on the Enriquillo-Plantain Garden Fault
The Himalayas were formed at a convergent plate margin where the Indian Plate collided with the Eurasian Plate. This collision resulted in the uplift of the Himalayan mountain range.
The Bahamas are a chain of islands that lie between Florida and Haiti.
A physcadelic plate.
Krakatoa is located on a destructive plate margin where the Indo-Australian plate subducts beneath the Eurasian plate. This subduction zone has led to the formation of volcanic islands in the region, including Krakatoa.