A conservative plate margin occurs when two plates move parallel to one another. Normally, one plate will be moving in the opposite direction to the other plate and this will very often cause a build up of friction. When one of these large build ups of friction is finally over come, the energy is released into the plate causing it to shudder.
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.
A passive continental margin lacks tectonic activity because it is not located near a plate boundary where volcanic and seismic activity typically occurs. Instead, passive margins form as plates pull apart, leading to subsidence and sediment accumulation rather than volcanic eruptions or earthquakes.
Convergent boundaries can form between two oceanic plates, between one oceanic plate and one continental plate, or between two continental plates.
The Greater Antilles are located near a transform plate boundary between the North American Plate and the Caribbean Plate. These plates are silding past one another. In the area where these plates meet, stress builds up, which is released in the form of earthquakes.
Mountains form, volcanoes can form/erupt, earthquakes can occur. That's all I know sorry.
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.
tectonic plates
A transformational plate boundary forms earthquakes.
they both form or happen from plate tectionic
A transformational plate boundary forms earthquakes.
yes of course
The Asian plate and the Pacific plate.
They are similar because they both form volcanoes and earthquakes.
There are three major plate movements, whether these occur on the continents or under the sea, convergent, where two plates collide together and one sinks under the other, although sometimes with continental plates if two continental plates collide then they are both very dense so they both press up against each other and form mountains, there are conservative plate margins, where the plates slip past each other, catching against each other causing earthquakes, and finally there are divergent plate margins where the plates are moving away from each other, these cause upsurges of magma in between and new land/sea bed is formed, these types of plate margins usually only occur under the sea, this is how Iceland was formed, but not the Hawaiian islands
A transformational plate boundary forms earthquakes.
Earthquakes form at a Transform boundary when the plate slips past each other.
Earthquakes usually occur around faultlines or plate boundaries because that's where plates split apart a long time ago. When two plates collide they form earthquakes.