Name: Why is it Hot Underground?
Uploaded: 2016-08-04T09:12:39.000Z
Duration: 2 min 47 s
Description: Thousands of YouTube videos with English-Chinese subtitles! Now you can learn to understand native speakers, expand your vocabulary, and improve your pronunciation...

Way back in the Middle Ages, miners began to notice that the deeper they dug into the

earth, the toastier it got. Who knows what they made of the heat, but the physicist Lord

Kelvin - of temperature fame, naturally - had a theory: Earth started off hot, and has been

cooling down ever since, like a baked potato pulled from the oven. What's more, Kelvin

was confident this idea would allow him to calculate the age of our potat-- planet...

Imagine pulling two recently-baked potatoes out of a freezer - one that's been in there

for just one minute, the other for half an hour. The minute-old-one would still feel

like a hot potato, while the half-hour frozen spud would have cooled well below the skin

— you'd have to poke all the way to the center to feel its residual warmth. And so

in principle, you can tell how long ago a potato was cooked just by feeling how warm

Which is exactly what Kelvin did - except with the earth. And scientific rigor. He took

temperature measurements from the mines, put them into his calculations and, got... 20

Which is, of course, very, very wrong — somehow, the hot temperatures just under Earth's skin

made it seem, to Kelvin, that our planet was pretty much fresh out of its cosmic oven,

when we now know that it's four and a half THOUSAND million years old.

Kelvin's error is usually attributed to the fact that he didn't know about radioactivity,

which creates a ton of heat in Earth's core and helps keep the planet warm. But heat from

radioactive decay moves so slowly through solid rock that taking radioactivity into

account only improves Kelvin's estimate by... pretty much nothing.

Kelvin's real oversight was in thinking of the Earth like a baked potato — a solid

lump through which heat slowly diffuses. Earth's mantle — the thick layer between the crust

and the core — is mostly solid, but it isn't rigid. In fact, the rock closest to the molten

outer regions of the core gets so hot that it becomes slightly more pliable, like warmed

candle wax. And like the hot air above a candle, the warm rock rises in convection currents

- over millions of years - spreading heat more evenly throughout the planet. This stirring

carries tremendous amounts of heat from the core to the crust, fueling volcanoes, maybe

helping to drive plate tectonics, and heating mine shafts to temperatures that make Earth

seem like it's fresh out of the cosmic oven.