Marine fossils at the summit of Mount Everest

Everest is essentially a giant, frozen pile of recycled seafood. If you reach the summit, you’re standing on the ancient floor of the Tethys Ocean, surrounded by 400-million-year-old fossils.

This happened because the Indian tectonic plate T-boned Asia in a slow-motion collision. The impact crumpled the seabed and shoved it nine kilometers into the sky, turning a marine graveyard into the "Roof of the World."

Human history is just a five-second commercial break at the end of this billion-year reality show. We’re basically climbing over prehistoric clams to take selfies.

Wait, if they're still crashing, is Everest actually getting taller right now?

Exactly. The 'accident' isn't over. India is still floor-matting the gas pedal into Asia, shoving Everest up by about 4 to 5 millimeters every year. It’s a skyscraper that refuses to stop adding floors.

In Earth's reality show, this is a very slow, aggressive hug. Over a million years, that tiny nudge adds up to four kilometers of height—assuming wind and ice don't sand it down first.

New height records aren't just better GPS; the mountain is literally crawling further away from its old sea-floor home.

But if it keeps growing, what's stopping it from hitting outer space?

Gravity is the ultimate bouncer. As Everest gets heavier, it actually "sinks" into the Earth's crust, which acts more like thick soup than solid rock. It’s like trying to build a massive Lego tower on a memory foam mattress; eventually, the weight just pushes back.

Then there’s the "cleanup crew"—glaciers and wind. They act like giant sandpaper, grinding the peak down as the plates shove it up. It’s a constant tug-of-war between the tectonic "up" button and the atmospheric "delete" key.

Without this constant sanding, the mountain would be a jagged needle piercing the stratosphere. Instead, it stays just low enough for humans to struggle up it for a profile picture.

So if the mountain sinks, does the bottom of it just melt?

It’s the ultimate cosmic recycling program. The mountain has a "root" that goes way deeper than the peak goes high. As gravity shoves that root into the hot mantle, the rock softens and reabsorbs into the Earth's internal lava lamp.

The "sanded" bits from the top wash down rivers as silt, settling on the ocean floor. In a few hundred million years, that same mud might get crushed and shoved back up into the sky.

The Earth is basically a zero-waste kitchen reheating the same rocky leftovers forever.

How many 'seasons' does it take for that mud to reach the top again?

We’re talking about a production schedule that makes a decade-long TV show look like a TikTok. One full lap—from peak to ocean floor and back—takes roughly 100 to 200 million years.

In the Earth’s reality show, that’s just one season. The silt waits for tectonic plates to play a slow game of Tetris, dragging it down before the next collision squeezes it back into a cloud-piercer.

Humans are like mayflies crashing the set during a commercial break. We name the rocks and die, while the mud is just halfway through its multi-million-year spa treatment.