Why Earth Has Two Levels | Hypsometric Curve

To learn more about this topic, start your googling with these keywords: Hypsometric Curve: Basically, a chart that shows the proportions of surface area at every elevation on a planet. Crust: Earth's outermost layer, made out of two distinct materials – oceanic crust (which is denser) and continental crust (which is less dense). Lithosphere: The rigid outer layer of Earth, including the crust and the hard, un-bending part of the upper mantle. Subduction: The process of an ocean plate crashing into another plate and getting forced to dive down into Earth's mantle. Isostasy: Describes the way earth's crust sort of floats in the underlying mantle. Continental crust is less dense and thicker, and floats higher than the oceanic crust, which is denser and thinner. Geologists talk about things like "isostatic rebound," which is what happens after an ice age, when the ice melts off a continent and the continent lifts up, like a floating raft in a pool after someone gets off (though continents rise more slowly). MinuteEarth is produced by Neptune Studios LLC https://neptunestudios.info If you like what we do, you can help us! - Become our patron: https://patreon.com/MinuteEarth   - Buy our merch: http://dftba.com/minuteearth   - Buy our book: https://minuteearth.com/books - Sign up to our newsletter: http://news.minuteearth.com   - Share with your friends and family - Leave us a comment (we read them!) Learn more about your ad choices. Visit megaphone.fm/adchoices