I really don't think so...
It doesn't. India is on Indian Plate whereas Australia is on Indo-Australian plate:
Everything on the surface of the earth is on a tectonic plate. All the Great Lakes and in fact all of the U.S. and Canada except for Hawaii and part of California are on the same tectonic plate: the North American Plate.
it will seporate in between each other
Continental Drift happened, when the tectonic plates in the earth shifted, and pushed the lithosphere up, causing our continents to split.
Continental drift theory was proposed before the discovery of the mid-oceanic ridge, when it was hypothesized that the continents were actually plowing through the oceans. This theory was an attempt to explain the commonality of fossils on opposite sides of the Atlantic Ocean, and the observation on maps of the Earth that the North American and South American continents appeared to have been pulled apart from Europe and Africa. With the discovery of the mid-oceanic ridge, where new crustal plate is being created, and subduction zones, where plates are being destroyed, plate tectonic theory was born; that the crust of the earth is divided into many segments that are in constant motion, that the oceanic crust is constantly being recycled--all driven by heat from the Earth's interior. Plate tectonics is now nearly universally accepted as scientific fact, yet questions remain to be answered on some of the mechanisms of the process.
No, subducting plate and oceanic plate are not the same. An oceanic plate is a type of tectonic plate that lies beneath the ocean, while a subducting plate refers to an oceanic plate that is descending beneath another tectonic plate at a convergent boundary. Subducting plates are a specific category of oceanic plates.
No, faults are not the same as plate boundaries, though they are related. Faults are fractures in the Earth's crust where rocks have moved past each other, while plate boundaries are the edges where tectonic plates interact. Plate boundaries can give rise to faults due to the stress and movement of the plates, but not all faults are located at plate boundaries. Faults can also occur within tectonic plates away from these boundaries.
Yes
A move in the earths crust. The tectonic plates push together causing the ground to move. Its also the same with tsunamis, except under water instead of land. Hope that helped :)
Crust is formed at the edge of a tectonic plate by, when a volcano erupts, the lava or magma (same thing) hits the edge of a tectonic plate and cools and dries on the edge of that tectonic plate.
the lithosphere and the crust of the earth are the same lithosphere is another word for crust so the thickest is both of them.
There is no difference, they are they same theory about the Earth's crust being divided and moving, they are just two different names that people call it.
No they are not the same thing. Plate Tectonics is the study of mechanisms and the results of large-scale movement of the earth's crust. Tectonic Plates are large sections of the earth's crust that float on top of semi-molten rocks of the upper mantle.
Earthquakes, mountains, and volcanoes are all related to the movement of tectonic plates in the Earth's crust. Earthquakes occur due to the release of tectonic stress, while mountains are formed by the collision of tectonic plates, pushing crustal rocks upwards. Volcanoes are formed when magma from beneath the Earth's surface is released through openings in the crust, often associated with tectonic plate boundaries.
No, Earth's tectonic plates are not all the same size. They vary significantly, with some being quite large, such as the Pacific Plate, which covers a vast area of the ocean floor, while others, like the Juan de Fuca Plate, are much smaller. The size and shape of tectonic plates are influenced by geological processes and the movement of the Earth's mantle.
It doesn't. India is on Indian Plate whereas Australia is on Indo-Australian plate:
The amount of crust present on Earth always stays the same. The amount of crust descending into the mantle is balanced by the amount of crust formed at mid-ocean ridges.