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The Earth's crust is broken up into several lithospheric or tectonic plates. These plates are constantly moving atop the Earth's mantle (semi-solid layer of molten rocks). Based upon their motion, tectonic plates are referred to as converging or diverging. Converging tectonic plates move towards each other and form convergent boundary. Diverging tectonic plates move away from each other and form divergent boundary.
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JordanConverging Plate Boundary: Two tectonic plates move towards each other. This can result in the creation of mountains, trenches, and volcanic arcs due to subduction or collision. Diverging Plate Boundary: Two tectonic plates move away from each other. This can lead to the formation of new crust through seafloor spreading and rift valleys on land.
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What is the difference between diverging and converging?
Diverging refers to moving apart or spreading out, while converging means coming together or meeting at a point. In terms of perspectives or opinions, diverging indicates disagreements or differences, while converging suggests agreeing or finding common ground.
What are diverging bounderies?
a divergent boundary is where two of earth plates are moving
What effect does a diverging boundary have on the crust?
A diverging boundary results in the separation of tectonic plates, leading to the creation of new crust through seafloor spreading. Magma rises to fill the gap between the plates, solidifies, and becomes part of the oceanic crust. This process contributes to the continuous renewal and expansion of the Earth's lithosphere.
What is venturi meter?
A Venturi meter is a device used to measure the flow rate of fluids in a pipeline. It consists of a converging section followed by a throat and then a diverging section. The pressure difference between the converging and throat sections is used to determine the flow rate of the fluid passing through the device.
How are the plates moving at the mid ocean ridge?
At mid-ocean ridges, tectonic plates are moving apart from each other due to seafloor spreading. Magma rises up from the mantle to fill the gap between the diverging plates, creating new oceanic crust. This process pushes the existing crust away from the ridge and helps drive the movement of the tectonic plates.
