how to make a computer program to move continents

Mantle water is therefore critical to the generation of continents. Subsequently, mantle chemistry is altered and buoyant melts are generated, leading to the production of continental crust. When the down-going plate reaches depths of 100 km, these minerals undergo a series of chemical reactions and release this water into the mantle. The down-going plate is oceanic crust, and it contains minerals with water locked into their structures. Subduction zones are colliding plate boundaries where a dense down-going plate sinks under a buoyant overriding plate. In order to explore how life can change the continents, we must first look to subduction zones, where continental crust is generated.

According to new research, life may have actually had something to do with this. Today, continental crust covers 40% of the Earth’s surface, so the amount of land has increased over time. Several authors propose a connection between life, mantle chemistry, and the presence of continental crust, noting that the first continents appeared at a similar time to when life first originated. The mantle contributes to how the continents move on the surface. The mantle is the layer of Earth below the crust, about 255 miles below the surface. Life has had an important role in shaping the Earth’s surface, but recent studies have suggested that biological activity may have had an even deeper impact on the planet’s evolution.

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How to make a computer program to move continents