plate is the part of lithosphere which is wholly cut upto asthenosphere, while the lithosphere is crust plus upper mantle, which is hard rigid rocks.
The Earth is made up of 7 major tectonic plates, which include the Pacific Plate, African Plate, Eurasian Plate, Australian Plate, Antarctic Plate, North American Plate, and South American Plate.
Plate tectonics is the geologic theory that the Earth's crust is made up of rigid plates. Some examples of tectonic plates are the African Plate, the Antarctic Plate, the Eurasian Plate and the Pacific Plate.
that the earth crust are made up of all different plates
Alfred Wegener is the scientist credited with proposing the theory of plate tectonics in 1912, although his ideas were not widely accepted until later.
There are seven tectonic plates that are primarily made up of oceanic crust: the Pacific Plate, Nazca Plate, Cocos Plate, Juan de Fuca Plate, Philippine Sea Plate, Arabian Plate, and the Scotia Plate. These plates are generally located in the ocean basins and are involved in the movement and interactions of Earth's tectonic plates.
An intraplate earthquake is an earthquake that occurs in the interior of a tectonic plate, whereas an interplate earthquake (plate boundary earthquake) is one that occurs at a plate boundary. Intraplate earthquakes are rare, but both can inflict large amounts of damage to populated areas.
It depends on where you are there are many tectonic plates I recomend that you should look up tectonic plate map and look for where you are.
Mt. Erubus has tectonic plates made up of parts of the lithosphere. These plates grind together or pull apart and this causes volcanoes to erupt.
The Earth's crust is made up of several tectonic plates which include the Pacific Plate, North American Plate, Eurasian Plate, African Plate, Antarctic Plate, South American Plate, Indo-Australian Plate, and the Nazca Plate. These plates float on the semi-fluid layer of the mantle beneath them and interact with each other through movements such as sliding past, colliding, or subducting under one another, causing geological events like earthquakes and volcanic eruptions.
The theory that explains the Earth's lithosphere is divided into several plates that move and interact with one another is called plate tectonics. This theory suggests that these plates were once joined together as a single supercontinent called Pangaea and have since drifted apart to their current positions.
Plate tectonics is the scientific theory that Earth's surface is broken up into huge, slow-moving slabs called tectonic plates. The movement of these plates drives many geologic processes including most earthquakes and volcanoes. Plate boundaries are the areas where two tectonic plates meet.
The reason the tectonic plate boundaries relate to mountains is because of the principle known as the Continental Drift. The theory of the Continental Drift was proposed in 1915 by a man named Alfred Wegener. His theory states that that earth's face is covered in tectonic plates that continuously move about 4 centimeters each year. When these tectonic plates collide, one plate is forced down while the other is is forced up forming moutains. For example, Mount Everest, which, never stops growing.