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Earth's plates or crust can cause earthquakes, volcanic eruptions, and the formation of mountain ranges due to tectonic plate movements and interactions. Subduction zones can also lead to the formation of deep ocean trenches and volcanic arcs.
The huge pieces of Earth's crust are called tectonic plates. These plates float on the semi-fluid asthenosphere beneath them and are responsible for various geological activities, such as earthquakes, volcanic eruptions, and the formation of mountain ranges. The movement and interaction of these plates shape the Earth's surface over geological time.
The asthenosphere.
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.
not necessarily but its not unheard of. mainly they make earthquakes or in some cases they form mountains over time
The large pieces of Earth's crust that move over the asthenosphere are called tectonic plates. These plates are responsible for the movement of continents and the occurrence of geological events such as earthquakes and volcanic eruptions.
Earth's plates or crust can cause earthquakes, volcanic eruptions, and the formation of mountain ranges due to tectonic plate movements and interactions. Subduction zones can also lead to the formation of deep ocean trenches and volcanic arcs.
The huge pieces of Earth's crust are called tectonic plates. These plates float on the semi-fluid asthenosphere beneath them and are responsible for various geological activities, such as earthquakes, volcanic eruptions, and the formation of mountain ranges. The movement and interaction of these plates shape the Earth's surface over geological time.
Mountain were made by huge segments of the earth's crust also know as tectonic plate. Over millions of year of volcanic activity under the earths crust forced these plates to shift. When to plates meet, the force of the volcanic pressure and the to plates may be pushed upward and create mountains.
The asthenosphere.
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.
an earthquake forms deep in side the earths crust, where plates, that hold continents, are. they move, sideways, forward, backward and slide over other plates. if two plates meet sliding or bumping each other, it cause waves over the earth, which we call earth quakes.These waves, animals can sense. there are three diffrent waves that come from an earthquake.P waves S waves and surface waves. the waves come over the earth, and some are silent at first,which the animals hear. the big ones, shake the earths crust, causing the crust to shake which we are on and buildings. and since the earth below us is moving, the building shake and fall, causing damage.
When earths plates collide together
pulling apart. As the plates move away from each other, the crust stretches and thins, creating a low-lying area known as a rift valley. Over time, this process can lead to the formation of new ocean basins.
The sphere that extends from Earth's core to Earth's crust is known as the mantle. It is the layer of the Earth located between the core and the crust and consists of solid rock that is capable of flowing over long periods of time. The mantle plays a crucial role in the movement of tectonic plates and the convection currents that drive the Earth's geological processes.
Sea floor spreading occurs due to the movement of tectonic plates away from each other. This movement creates a gap or rift at the mid-ocean ridge where magma rises up from below the Earth's crust, solidifying to form new crust. Over time, this process results in the continuous widening of the sea floor.
These are individual broken slabs of gigantic masses, that makes up the earths crust and are capable of floatational movement over the weak, plastic, hot and highly molten portion of the mantle called the asthenosphere.