little or no. nicely in the beginning up. Oceanic plates flow at some distance too sluggish a speed to 'collide' interior the classic sense. rather they press into one yet another, construction stress and elevating their edges - transforming into mountains. If those mountains upward push excessive sufficient - an island could be fashioned. while the tectonic stress between 2 plates mounts up too lots - an earthquake consequences. Earthquakes notwithstanding are in particular too susceptible or too some distance down for us to be stricken by making use of them, yet while a extensive one have been to take place at sea, a tsunami could in all hazard result. So, mountains and earthquakes.
Smarty-Marti
2007-08-30 18:02:17 UTC
An earthquake... Hahahaha
When they push together: compressional zones (subduction)
When they separate: extensional
When they slip sideways: transformation
anonymous
2007-08-30 17:56:14 UTC
Convergent Plate Movement?
anonymous
2007-08-30 18:57:53 UTC
plate tectonics... I think
22
2007-08-30 20:28:04 UTC
a convergant boundary forms. What type of convergant boundary depends on the type of plate.
if an oceanic plate hits a continental plate the denser oceanic plate dives beneath the continental plate causing a zone of mountains and volcanoes to form. this process is subduction. Japan and the Andes in South America were formed in this way.
subduction will also ocurr if two oceanic plates collide. The denser plate will dive beneath the other and cause an island arc to form. the Mariana islands are an example
when two continental plates collide they form an orogenic belt causing a mountain range to form. The Himalayas and Rockies were formed this way.
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