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the movement of boundaries of the rock

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Plate tectonics is the theory that Earth's outer shell is divided into several plates that glide over the mantle, the rocky inner layer above the core. The plates act like a hard and rigid shell compared to Earth's mantle.

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Shows the movement of rocks.

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shows the movement of rocks on the surface of the plates

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Some evidence of the theory of plate tectonics includes distribution of rock formation/fossils, shapes of the continents, ocean floor features, & seismic & volcanic activity. Also, some other evidence may be identical fossil formations found on separate continents, & paleoclimate evidence

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The theory of plate tectonics explain the motion of lithospheric plates, geologic activities at plate boundaries, and the changes in landform areas over geologic time by showing current and also past time movment of rocks

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From the deepest ocean trench to the tallest mountain, plate tectonics explains the features and movement of Earth's surface in the present and the past.

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shows movement of rocks

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show the movement of rocks on the surface of the plates.

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show the movement of rocks on the surface of the plates.

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it show the movements of the rocks which is called lithospheric plates

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When the tectonic plate has Lithosphere  and another one has it too and they come together the one with most density sinks into the mantle. The geologic activities that takes place at the plates are many convergent, divergent, or transform boundaries. The changes of land forms over times are with volcanoes, mountains, and trenches.

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Plate tectonics is the theory that Earth's outer shell is divided into several plates that glide over the mantle, the rocky inner layer above the core. The plates act like a hard and rigid shell compared to Earth's mantle. This strong outer layer is called the lithosphere, which is 100 km (60 miles) thick, according to Encyclopedia Britannica. The lithosphere includes the crust and outer part of the mantle. Below the lithosphere is the asthenosphere, which is malleable or partially malleable, allowing the lithosphere to move around. How it moves around is an evolving idea.

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It explains the past and current movements of the rocks at Earth’s surface (lithospheric plates) and provides a framework for understanding its geological history.