#science #sciencemanuelacasasoli
About 60 million years ago, India plowed into Eurasia and pushed up the Himalayas. But when Lucía Pérez-Díaz reconstructed the event in detail, she found that its central mystery depended on a broken geological clock.
The New Historian of the Smash That Made the Himalayas
About 60 million years ago, India plowed into Eurasia and pushed up the Himalayas. But when Lucía Pérez-Díaz reconstructed the event in detail, she found that its central mystery depended on a broken geological clock.
The New Historian of the Smash That Made the Himalayas
like this
BR 549 ☎
in reply to Manuela Casasoli • •it seems ridiculous to think it's either-or like that. it isn't "either plume-push or subduction-pull". the mantle is a convection system, going in a circular pattern up, around, down, and back. crustal plates are merely going along for the ride on the surface. lighter silica-rich rock floating on heavier iron-rich mantle rock.
it would be interesting to know whether there are other convective layers between crust and core, and how many...
also, how fast is the nickel-iron core taking up oxygen and "rusting"? or does it give off oxygen at some point?