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Geography
The Caribbean plate
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Emily Rambharose
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Cards (14)
Caribbean plate
Borders the
North American
plate, the South American plate, the
Nazca
plate and the Cocos plate
Borders of the Caribbean plate
Regions of intense
seismic
activity including frequent earthquakes, occasional
tsunamis
and volcanic eruptions
Convergent plate boundary east of the Caribbean plate
1. North American and
South American plates
are slowly moving
west
and being pushed under the margin of the Caribbean plate
2. Results in the formation of a
volcanic island arc
Convergent plate boundary west of the Caribbean plate
1.
Cocos
plate moves
east
and is being pushed under the margin of the Caribbean plate
2. Results in
volcanoes
and
earthquakes
Transform plate boundary
north
of the
Caribbean
plate
North American
plate slides past the
South American
plate
Transform plate boundary through
Trinidad
and close to the north coast of
Venezuela
Movements
result in
earthquakes
Divergent plate boundary west of Jamaica
Cayman Island Ridge
Island arc
Long, curved chain of oceanic islands associated with intense
volcanic
and
seismic
activity
Volcanic
arc
Formed from
continent-oceanic
interaction
Island arc
Formed from
oceanic-oceanic
interaction
Formation of island arc
1.
Lithospheric
slab is being
subducted
2.
Slab
melts at depth where it is sufficiently
hot
3. Remelted material from the subducting slab rises and leaks into the crust forming a series of
volcanoes
making a chain of
islands
Examples of island arcs
Japan
Aleutian
Islands of
Alaska
Mariana
Islands
Lesser
Antilles in the
Caribbean
The abundance of volcanic rocks around the Pacific Ocean has led to the designation of the
Pacific margin
as a
'Ring of Fire'
Most of the world's active volcanoes are found in the
'Ring of Fire'
belt