LONG BEFORE
Earth as a planet, the scale at which continents become visible as moving pieces

The ground is not finished

Can a continent move if you cannot feel it?

Pangaea about 250 million years ago · The whole planet · Scientific visualization

Planet-scale view. Paleogeography in this room is a schematic model, not a surveyed historical map.

First look

Can a continent move if you cannot feel it?

Wonder. Then look. This is not a test.

Continents move a few centimeters each year, about as fast as a fingernail grows.

Over a million years, that becomes kilometers.

The Atlantic opened. India traveled. Pangaea assembled and later broke.

First look is enough. Keep looking is if you want more.

Planet field

Now

this year

The arrangement you already know. A schematic, not a survey.

equator (schematic)GreenlandGreenlandNorth AmericaNorth AmericaSouth AmericaSouth AmericaAfricaAfricaEuropeEuropeAsiaAsiaIndiaIndiaAustraliaAustraliaAntarcticaAntarctica

Scientific visualization. Coastlines are models, not observed historical maps.

Can a mountain disappear?

Rock rises. Weather cuts. Sediment travels to the sea. Another range can grow from the same atoms later. Mountains are temporary on the only clock that matters here.

Folded mountains shedding sediment toward a distant sea

Keep looking

How would we know? Open only if you want the evidence.

Keep looking · How we know

Seafloor stripes record magnetic reversals. GPS measures motion now. Fossils and rock belts match across oceans. A map of the past is a model built from those records.

Keep looking · Mountains are temporary

Rock can rise, weather, and return to the sea. A mountain range is a slow event, not a permanent furniture of Earth.