The other, more recent hypothesis, suggests that most of Earth’s water was already here inside the planet, and it came to the surface over time. There are hydrous materials in Earth’s Mantle, such as Ringwoodite and Wadsleyite, that store the necessary elements to create water (hydrogen and oxygen). Ringwoodite is hidden within diamonds in the Transition Zone, a layer of Earth between the Upper and Lower Mantle. Then, as hot magma rises up and cooler magma sinks down into the planet, these pressures crush the hydrous materials, wringing them like a sponge. During this process water finds its way to the surface through volcanoes and underwater vents.