What is plate tectonics?

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Multiple Choice

What is plate tectonics?

Explanation:
Plate tectonics is the idea that Earth’s outer shell is broken into moving slabs called tectonic plates that float on the partially melted layer beneath, the asthenosphere. These plates shift slowly because of convection currents in the mantle, and where they meet they can pull apart, collide, or slide past each other. This movement at plate boundaries explains why earthquakes happen, where volcanoes form, and how continents and oceans drift over time. The notion of a single undivided shell doesn’t account for these moving pieces, and saying continents drift because of ocean currents isn’t accurate—the driving force is the motion of the tectonic plates themselves. Earthquakes aren’t caused by the Sun’s gravity; they arise from stresses released as plates interact.

Plate tectonics is the idea that Earth’s outer shell is broken into moving slabs called tectonic plates that float on the partially melted layer beneath, the asthenosphere. These plates shift slowly because of convection currents in the mantle, and where they meet they can pull apart, collide, or slide past each other. This movement at plate boundaries explains why earthquakes happen, where volcanoes form, and how continents and oceans drift over time. The notion of a single undivided shell doesn’t account for these moving pieces, and saying continents drift because of ocean currents isn’t accurate—the driving force is the motion of the tectonic plates themselves. Earthquakes aren’t caused by the Sun’s gravity; they arise from stresses released as plates interact.

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