Oceanic plates are heavier than continental plates because they are denser and thinner. Continental plates are lighter because they are less dense and thicker. The difference in density and composition accounts for the varying weights of the Earth's plates.
The oceanic and continental plates make up the lithosphere, which is the outermost layer of the Earth. The lithosphere consists of the crust and the uppermost part of the mantle, and it is divided into tectonic plates that float on the more fluid asthenosphere beneath. Oceanic plates are primarily composed of basalt, while continental plates are mainly composed of granite.
Oceanic plates, continental plates, and microplates are all examples of tectonic plates that make up the Earth's lithosphere. These plates move around due to the heat-driven convection currents in the Earth's mantle, causing phenomena like earthquakes, volcanoes, and mountain-building.
Faults, graben and mid oceanic ridges.
Oceanic plates are denser and thinner, found beneath the oceans, while continental plates are thicker and less dense, making up the Earth's landmasses. These two types of tectonic plates interact at boundaries, influencing processes like earthquakes and volcanic eruptions.
Oceanic plates are sections of the Earth's lithosphere that are found beneath the oceans. These plates are denser and thinner than continental plates and are typically composed of basaltic rock. Oceanic plates are constantly moving due to the process of plate tectonics, where they can collide with, slide past, or be forced beneath other plates.
Oceanic plates are sections of the Earth's lithosphere that form the bedrock beneath the world's oceans. These plates are typically denser and younger than continental plates, and they are constantly moving due to the process of plate tectonics. Subduction zones are often found at the boundaries where oceanic plates meet continental plates.
yes
No, not all plates contain oceanic crust. The Earth's lithosphere is divided into a combination of oceanic and continental plates, each with their unique composition and characteristics. Continental plates are thicker and less dense than oceanic plates, and they mainly consist of granite and sedimentary rocks.
Of the Earth's major plates, the following are composed of a majority of oceanic crust: Pacific, North American, African, Antarctic, Australian, and South American.
an earth quake happens when two plates meet
Oceanic plates are heavier than continental plates because they are denser and thinner. Continental plates are lighter because they are less dense and thicker. The difference in density and composition accounts for the varying weights of the Earth's plates.
The two main types of plates that make up the Earth's lithosphere are oceanic plates, which are denser and thinner, and continental plates, which are less dense and thicker. These plates interact with each other at their boundaries, causing movements such as subduction, spreading, and collisions that shape the Earth's surface.
The oceanic and continental plates make up the lithosphere, which is the outermost layer of the Earth. The lithosphere consists of the crust and the uppermost part of the mantle, and it is divided into tectonic plates that float on the more fluid asthenosphere beneath. Oceanic plates are primarily composed of basalt, while continental plates are mainly composed of granite.
Tectonic plates.Tectonic plates are plates underneath Earth's surface that move very slowly. There are oceanic and continental plates. Of course, oceanic plates are plates under the ocean, and continental plates are plates underneath ground, or continents. Each of the plates carry the things above them, land or ocean. When two continental or oceanic plates collide, it causes a fold in Earth's surface, and an earthquake. Now, when a continental plate draws near and nearly collides with an oceanic plate, something called subduction occurs. Subduction is basically when the oceanic plate dips down below the continental plate, causing a trench.
the magma
friction of the gravity