250 million years of transformation

The Drifting
Continents

How the face of our planet has been ceaselessly rewritten

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The Theory

A planet
in perpetual motion

Continental drift is the hypothesis that Earth's continents have moved over geologic time relative to each other, thus appearing to have "drifted" across the ocean bed. The speculation that continents might have shifted position over time is ancient, but the idea was revived in the early 20th century by Alfred Wegener.


Wegener presented a large body of circumstantial evidence in support of continental drift, but was unable to provide a convincing mechanism. It was not until the 1950s and 60s that the theory of plate tectonics emerged to explain the driving force.

"Does not the east coast of South America fit exactly against the west coast of Africa, as if they had once been joined?"
— Alfred Wegener, 1912
South America Africa THE PUZZLE FIT Fossil match Rock strata

Geologic History

The great unfolding

1.1 Bya
BILLION YEARS AGO
Rodinia

The first known supercontinent forms. Nearly all of Earth's landmass assembles into a single mass centered near the equator. A vast global ocean — Mirovia — surrounds it entirely.

Rodinia
Pannotia
600 Mya
MILLION YEARS AGO
Pannotia

Rodinia breaks apart and reassembles into Pannotia — a shorter-lived supercontinent. The fracturing coincides with the Snowball Earth glaciation events. Life remains confined to the oceans.

335 Mya
MILLION YEARS AGO
Pangaea

The most famous supercontinent assembles. A single enormous ocean — Panthalassa — covers nearly 70% of the planet. Dinosaurs roam freely across all connected landmasses. The climate is dramatically warmer.

Pangaea
Split begins
175 Mya
MILLION YEARS AGO
Laurasia & Gondwana

Pangaea cleaves into two massive pieces — Laurasia in the north (proto North America, Europe, Asia) and Gondwana in the south (proto Africa, South America, Antarctica, Australia, India).

Today
PRESENT DAY
Seven Continents

The continents reach their current configuration. The Atlantic Ocean continues to widen 2.5 cm/year. The Americas drift westward. Africa and Europe inch toward each other. The Pacific shrinks. The story is not over.

Present

Scientific Proof

Six lines of evidence

01
Fossil Distribution

Identical fossils of Mesosaurus (a freshwater reptile), Glossopteris (a fern), and Lystrosaurus (a land animal) are found on continents now separated by thousands of miles of ocean — impossible unless those continents were once joined.

02
Coastline Geometry

The eastern coast of South America and western coast of Africa fit together with remarkable precision — not just visually, but also at the continental shelf (the true edge of the continent, 200m below sea level).

03
Rock Strata Matching

Identical rock formations, ages, and mineral compositions appear on opposing continental edges. The Appalachian Mountains align with the Scottish Highlands and the Atlas Mountains of Morocco when the continents are reassembled.

04
Paleoclimatic Evidence

Coal deposits (requiring tropical forests) are found in Antarctica. Glacial striations exist in tropical Africa. Ancient desert sandstones appear in Britain. Each region's past climate is explained only by its former position on the globe.

05
Sea-Floor Spreading

Magnetic reversals recorded symmetrically on either side of mid-ocean ridges proved that new crust is continuously created at spreading centers. Harry Hess's 1960 discovery provided the missing mechanism Wegener lacked.

06
GPS Measurement

Modern satellite geodesy directly measures continental motion. North America moves ~2.3 cm/year from Europe. India crashes into Asia at ~5 cm/year, raising the Himalayas 5mm annually. The drift is live and observable.

Interactive Visualization

Watch the continents drift

Select an era to see how the landmasses were arranged. Each configuration shaped the evolution of life, climate, and ocean currents of its time.

Pangaea · 335 million years ago

Select an era

1930

The Visionary

Alfred Wegener

A German meteorologist and polar explorer, Wegener formally proposed the theory of continental drift in 1912. His idea — that continents were once a single landmass — was ridiculed by the geological establishment of his day.


Without a viable mechanism to explain how continents could plow through the ocean floor, his theory was largely rejected for 50 years. He died on the Greenland ice sheet in 1930 during his fourth Arctic expedition, his greatest hypothesis still unproven.

1912
Year theory proposed
50
Years until acceptance
2.5cm
Annual Atlantic widening
250M
Years since Pangaea

What comes next

The next supercontinent

Geologists predict that in roughly 250 million years, a new supercontinent — sometimes called Amasia or Pangaea Proxima — will form as the Americas collide with Asia, and Africa merges with Europe. The Atlantic may close. The story of Pangaea is not history — it is a cycle.

Pangaea 335 Mya Separation 175 Mya Today Present Amasia ~250 Mya future