volcanoes,mid ocean ridges,fold mountains and hot spots
plate boundry has four different parts. # conservative boundary. # constructive boundary. # destructive boundary. # collision boundary.
Four Tectonic PlatesJapan lies over 4 tectonic plates. These are: The North American PlateThe Eurasian PlateThe Philippine Sea Plate, andThe Pacific Plate.
There are four main kinds of changes that can affect the earth's surface: 1)Earthquake 2)Flood 3)Valcano 4)Temperature
Value of mothers joy potrait series first in series of four 1982 number 2962 in edition of 7500
Possibly, if they change the rules at the convention. The convention delegates are the ones who can revise the rules once each four years. It is not likely to happen, though.
The four types of plate boundaries are divergent boundaries (plates moving apart), convergent boundaries (plates moving together), transform boundaries (plates sliding past each other), and subduction zones (one plate sinking beneath another).
The four plate boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates move towards each other; transform boundaries, where plates slide past each other horizontally; and subduction zones, where one plate is forced beneath another plate.
The four types of plate boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates collide; transform boundaries, where plates slide past each other horizontally; and plate boundary zones, which encompass areas where interactions between multiple plates occur.
There are four transform boundaries divergent boundaries convergent boundaries a fourth boundary where the interactions are not clear and the boundaries are not well defined
The Are Seven Primary Plates, so there cannot be only Five Boundaries, I know the tectonic Plates are The 1. African Plate 2. Antarctic Plate 3. Eurasian Plate 4. Indo-Australian Plate 5. North American Plate 6. Pacific Plate 7. South American Plate There Are Three Basic types of boundary; Divergent, Convergent and Transform boundaries Hopefull somebody can tell you all their names of the boundaires between them because these different Plates will me touching two or More Plates hence a lot of different boundaries
i know 3 divergent convergent and transform boundaries correct me it wrong
The four types of plate movements that can cause earthquakes are convergent boundaries, divergent boundaries, transform boundaries, and subduction zones. These movements can result in the buildup of stress within the Earth's crust, which may eventually be released in the form of an earthquake.
Divergent boundaries -- where new crust is generated as the plates pull away from each other.Convergent boundaries -- where crust is destroyed as one plate dives under another.Transform boundaries -- where crust is neither produced nor destroyed as the plates slide horizontally past each other.Plate boundary zones -- broad belts in which boundaries are not well defined and the effects of plate interaction are unclear.
The four main types of plate tectonics are divergent boundaries, where plates move away from each other; convergent boundaries, where plates collide; transform boundaries, where plates slide past each other horizontally; and subduction zones, where one plate is forced beneath another.
There are four main types of plate boundaries: divergent boundaries, where plates move apart; convergent boundaries, where plates collide; transform boundaries, where plates slide past each other horizontally; and plate boundary zones, which are complex regions with combinations of these boundary types.
There are only 3 that I know, transform, divergent, and convergent. -Toby Shout out to Mrs. Cordero
The four factors that influence plate movement are ridge push (formation of new crust at mid-ocean ridges pushing plates apart), slab pull (gravity pulling denser oceanic crust into the mantle at subduction zones), mantle convection (heat-driven circulation in the mantle that moves plates), and forces at plate boundaries (such as tensional forces at divergent boundaries and compressional forces at convergent boundaries).