Seafloor Spreading Diagram Answer Key Form
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People also ask sea floor spreading review and reinforce worksheet answers
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What is seafloor spreading Class 7?
Seafloor spreading is a geologic process in which tectonic plates large slabs of Earth's lithosphere split apart from each other. Seafloor spreading occurs along mid-ocean ridges (large mountain ranges rising from the ocean floor). The Mid-Atlantic Ridge is formed in the Atlantic ocean because of seafloor spreading. -
What are the key points of seafloor spreading?
Key points Seafloor spreading takes place at midocean ridges and produces basalt, the rock that makes up the oceanic crust. The Mid-Atlantic Ridge and East Pacific Rise are examples of midocean ridges. Midocean ridges signNow a typical summit elevation of 2,700 meters below sealevel. -
What is seafloor spreading and diagram?
Seafloor spreading is a geologic process in which tectonic plates—large slabs of Earth's lithosphere—split apart from each other. Seafloor spreading and other tectonic activity processes are the result of mantle convection. -
What are the steps of the seafloor spreading process?
Stages of Seafloor Spreading The sea floor spreading process can be divided into three main stages: magma generation, magma transport, and crustal accretion. -
What is seafloor spreading quizlet?
What is the process of sea-floor spreading? In sea-floor spreading, the sea floor spreads apart along both sides of a mid-ocean ridge as new crust is added. As a result, the ocean floors move like conveyor belts, carrying the continents along with them. -
What is the seafloor spreading?
Seafloor spreading occurs at divergent plate boundaries. As tectonic plates slowly move away from each other, heat from the mantle's convection currents makes the crust more plastic and less dense. The less-dense material rises, often forming a mountain or elevated area of the seafloor. Eventually, the crust cracks. -
What is sea floor spreading Class 9?
Seafloor spreading is the process of magma welling up in the rift as the old crust pulls itself in opposite directions. Cold seawater cools the magma, creating a new crust. The upward movement and eventual cooling of this magma has created high ridges on the ocean floor over millions of years.
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