Key Takeaways
We have established that the ocean is held by physical boundaries. The ocean basin is a tectonic depression, deeper than continents are high. The crust beneath the ocean is distinct from continental crust. These factors create a stable container that prevents water from simply flowing away.
Looking Ahead
Now that we know the ocean is in a physical basin, the next question is: what is that basin made of? In the next chapter, we will dive into the layered structure of the seafloor to see if the materials themselves could allow water to escape.