Naval architecture : Margin plate are those plate which form the outer edge of the double bottom and must be water tight.
In welded type ship it has sometimes flanged, but it has become common practice to extend the inner bottom plating and to attach it to the top of tank side bracket.
Because of the big grinding of the conservative plate margin cause the land to go back and forth
No,plate margin&plate boundary are not same.plate boundaries are definite regions where tectonic occurs,while margins are surface lines.
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.
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.
Mount Etna is located on a destructive plate boundary, where the African Plate is being subducted beneath the Eurasian Plate. The melting of the subducted plate generates magma that rises to the surface, leading to volcanic activity at Mount Etna.
Because of the big grinding of the conservative plate margin cause the land to go back and forth
Because of the big grinding of the conservative plate margin cause the land to go back and forth
Yes, the Kobe earthquake occurred on a conservative plate margin where the Philippine Sea Plate is being subducted beneath the Eurasian Plate. The earthquake was a result of the intense tectonic forces and stresses associated with this subduction zone.
Plate tectonics move. But the plate margin that cause strong earthquakes are collision and conservative plate margins. I hope it helped!
Japan sits on top of a destructive plate margin.
Yes, Eyjafjallajökull volcano is located on the constructive plate margin between the North American Plate and the Eurasian Plate in Iceland.
No,plate margin&plate boundary are not same.plate boundaries are definite regions where tectonic occurs,while margins are surface lines.
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.
There are 3 ways an earthquake can be caused: destructive margin: this can cause an earthquake and volcano and is the most dangerous margin. it is when one plate slides under another. collision margin: this only creates earthquakes, and it is when two plates move towards each other and collide. conservative margin: this is when plates slide against each other, like San Andrea's Fault, California. They only create earthquakes. Hope this helps ! xx
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.
Mount Etna is located on a destructive plate boundary, where the African Plate is being subducted beneath the Eurasian Plate. The melting of the subducted plate generates magma that rises to the surface, leading to volcanic activity at Mount Etna.