Large-Scale folding of the earth's crust is mostly caused by the collision of sub-crustal plates.
plate tectonics
consist of large sections called tectonic plates, which move relative to each other.
The sections of the Earth's crust that float on the partially melted section of the mantle are known as tectonic plates. These plates consist of both continental and oceanic crust and are rigid sections that move slowly over the semi-fluid asthenosphere beneath them. Their interactions can lead to geological phenomena such as earthquakes, volcanic activity, and the formation of mountains.
the large sections of the earth's crust that move relative to each other
The theory that Earth's crust is divided into sections that interact with each other over time is called plate tectonics. This theory explains how the Earth's lithosphere is divided into several large and small plates that float and move on the semi-fluid asthenosphere beneath them. The interactions between these plates cause phenomena such as earthquakes, volcanic eruptions, and mountain formation.
earthquakes happen when these sections of earths crust move
Plate tectonics
plate tectonics
It consist of large sections called tectonic plates, which move relative to each other.
The earths crust is split into large pieces called plates. When they move they cause a earthquake.
The Earth's crust is broken into large sections known as tectonic plates. These plates float on the semi-fluid asthenosphere beneath them and can move due to convection currents in the mantle. The interactions between these plates can lead to geological phenomena such as earthquakes, volcanic activity, and the formation of mountains. The Earth's crust is divided into two main types: continental crust and oceanic crust.
consist of large sections called tectonic plates, which move relative to each other.
The sections of the Earth's crust that float on the partially melted section of the mantle are known as tectonic plates. These plates consist of both continental and oceanic crust and are rigid sections that move slowly over the semi-fluid asthenosphere beneath them. Their interactions can lead to geological phenomena such as earthquakes, volcanic activity, and the formation of mountains.
the large sections of the earth's crust that move relative to each other
Earthquakes happen when tectonic plates along fault lines shift and release built-up pressure, causing the ground to shake. The sudden release of energy creates seismic waves that result in vibrations felt on the Earth's surface.
a salami.
Tectonic plates.