Earth’s crust is broken into slabs of rock called tectonic plates. Underneath is the mantle, a layer of rock 2,900 kilometers (1,800 miles) thick (see Layers of Earth). Most of it is solid, but parts are hot enough to flow like liquid.
Tectonic plates glide over the mantle at about the speed fingernails grow. When the edges of plates push against each other, earthquakes and volcanic eruptions can result.
Pulling up a piece of the mantle would help scientists earn how Earth formed. Last year, MacLeod and other scientists found a perfect spot to try. The site is on a rocky hill at the bottom of the Indian Ocean. Here, Earth’s crust is thin—only 5 kilometers (3 miles) deep. The team set out on a ship designed for serious drilling.