Convergent Boundaries are found where two plates push against each other, sometimes causing earthquakes.
Lithosphere
Convection currents can be found in real-world examples such as in the atmosphere, where they drive weather patterns and wind movements. In the ocean, convection currents play a role in the circulation of water and nutrient distribution. In the Earth's mantle, convection currents are responsible for the movement of tectonic plates and the formation of volcanic activity.
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Convection currents can be found in the mantle layer of Earth, specifically in the asthenosphere. These currents are responsible for driving tectonic plate movements and are a key component of the process of plate tectonics.
Convection currents flow in Earth's mantle, which is the layer of rock beneath the Earth's crust. These currents are responsible for the movement of tectonic plates and the formation of features like mountain ranges, volcanoes, and earthquakes.
The upper mantle
Convection currents move in the Mantle.
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Convection currents are primarily found in the Earth's mantle, where they play a crucial role in plate tectonics. These currents occur due to the heat from the Earth's core causing the mantle's semi-fluid rock to rise, cool, and then sink again. Additionally, convection currents can also be observed in the atmosphere and oceans, where they drive weather patterns and ocean circulation.
Convection currents move in upward direction