The whole history of Earth at true scale. This page is 115,000 pixels tall. One pixel is 40,000 years. The scale never changes, anywhere, including at the end. What follows is 57 arrivals in chronological order, from 4,567 Ma to 9.3–6.5 Ma. Ten more recent moments are listed at the end instead: they are
too close together to be drawn on this page at all. Left and right arrow keys move between arrivals.
Deep Time
The whole history of Earth, at true scale.
This page is 115,000 pixels tall.
One pixel is 40,000 years.
The scale never changes.
scroll
4.60 Ga
HADEAN
Modelled
moon2.51× wide
day6.0 hours
1 px = 40,000 years
0 / 115,000 px
True scale
4,567 Ma4,567 million years agoThe Solar System formsThe Solar System formsDust and ice collapse around a new star. Nothing older has ever been dated.4,540 Ma4,540 million years agoEarth reaches full sizeEarth reaches full sizeAccretion finishes. The whole surface is molten rock.≥ 4,510 Maat least 4,510 million years agoThe Moon is torn outThe Moon is torn outA Mars-sized body strikes, at least 4.51 billion years ago. The debris becomes a Moon that hangs enormous and close.
The Moon is two and a half times wider than it is today
4,404 Ma4,404 million years agoLiquid waterLiquid waterA single zircon crystal records water at the surface.4,300 Ma4,300 million years agoSteam and acid rainSteam and acid rainThe air is CO₂. The rain is acid. There is nothing yet you would call land.≥ 4,160 Maat least 4,160 million years agoThe oldest surviving crustThe oldest surviving crustNuvvuagittuq, Quebec — a scrap of the first ocean floor.4,031 Ma4,031 million years agoThe oldest rock we still haveThe oldest rock we still haveAcasta gneiss, north-west Canada. The Hadean ends here because this is where the record starts.3,800 Ma3,800 million years agoThe oldest sedimentary rocksThe oldest sedimentary rocksIsua, Greenland — mud, laid down under water, by a real ocean.3,700 Ma3,700 million years agoThe first trace of lifeThe first trace of lifeIsotopically light carbon in Isua sediment. Not a fossil — a chemical shadow, and the oldest one anyone accepts.3,600 Ma3,600 million years agoMicrobial matsMicrobial matsLife is a film on the seabed, and stays that way for three billion years.3,480 Ma3,480 million years agoStromatolitesStromatolitesMats build the first structures life leaves behind. Whether these particular ones did is still argued.3,400 Ma3,400 million years agoMicrobes that eat sulfurMicrobes that eat sulfurNo oxygen, no sunlight needed — chemistry alone.3,260 Ma3,260 million years agoA fifty-kilometre asteroidA fifty-kilometre asteroidThe S2 impact — 50 to 200 times the mass of the one that killed the dinosaurs. It boils the top of the ocean, and life gets better.3,220 Ma3,220 million years agoThe first continentsThe first continentsCratons stabilise. There is now permanent dry land.3,000–2,400 Ma3,000 to 2,400 million years agoPhotosynthesisPhotosynthesisCyanobacteria split water and let the oxygen go. It will take 600 million years to matter.2,900 Ma2,900 million years agoThe first ice ageThe first ice ageThe Pongola glaciation. Ice at mid-latitudes, on a planet with no oxygen.2,800 Ma2,800 million years agoCyanobacteria, everywhereCyanobacteria, everywhereStill no free oxygen in the air — the rock is drinking all of it.2,700 Ma2,700 million years agoWhiffs of oxygenWhiffs of oxygenOxygen appears in patches, hundreds of millions of years before the air changes.
The sky flickers orange and back, three to five times
2,600 Ma2,600 million years agoBanded ironBanded ironOxygen meets dissolved iron and it rusts out of the sea, in bands, for a billion years.2,500 Ma2,500 million years agoBanded iron, stillBanded iron, stillStill rusting out of the sea. It has been a hundred million years.2,430 Ma2,430 million years agoThe Great Oxidation beginsThe Great Oxidation beginsFree oxygen floods the air and poisons most of the life that made it.2,400 Ma2,400 million years agoThe Huronian glaciationThe Huronian glaciationOxygen destroys the methane greenhouse and the planet freezes, three times over.
The sky is blue
2,220 Ma2,220 million years agoThe Great Oxidation endsThe Great Oxidation endsOxygen is permanent. The haze never comes back.2,100 Ma2,100 million years agoFrancevillian structures?Francevillian structures — identity disputedCentimetre-scale shapes in Gabon. Possibly the oldest multicellular life; possibly not life at all.
Oxygen falls back
1,870 Ma1,870 million years agoGrypania?Grypania — identity disputedA coiled ribbon in Michigan iron. Big enough to see, but nothing of its cells survives.
Banded iron stops
1,635 Ma1,635 million years agoThe first complex cellsThe first complex cellsQingshania — cells with a nucleus, stuck together on purpose.1,047 Ma1,047 million years agoSexSexBangiomorpha, a red alga. The oldest known sexual reproduction.1,000 Ma1,000 million years agoRodiniaRodiniaEvery continent, gathered into one mass.890 Ma890 million years agoThe first sponges?The first sponges — identity disputedSponge-like structures in Canadian reef rock, 300 million years before any agreed animal.
The Boring Billion ends
717 Ma717 million years agoSnowball EarthSnowball EarthIce reaches the tropics. The Sturtian lasts 56 million years.661 Ma661 million years agoThe ice retreatsThe ice retreatsCap carbonate, laid down in a few thousand years on top of the ice.635 Ma635 million years agoThe ice breaks for goodThe ice breaks for goodA second freeze, the Marinoan — perhaps only four million years — and then it is over. The Ediacaran begins.574 Ma574 million years agoCharniaCharniaThe first big bodies — soft, strange, rooted to the seabed.538.8 Ma538.8 million years agoThe Cambrian beginsThe Cambrian beginsShells, eyes, guts, predators, and the first things burrowing through mud on purpose.508 Ma508 million years agoThe Burgess ShaleThe Burgess ShaleAnomalocaris — a metre of segmented predator, with the first real eyes.470 Ma470 million years agoPlants reach landPlants reach landSpores, nothing you could call a plant yet. Land has been bare for four billion years.445 Ma445 million years agoThe Late Ordovician extinctionThe Late Ordovician extinctionIce, then anoxia. About 85% of species go.420 Ma420 million years agoCooksoniaCooksoniaThe first plants with stems. A few centimetres tall, and the tallest thing alive.375 Ma375 million years agoTiktaalikTiktaalikA fish with a neck, and wrists.320 Ma320 million years agoThe coal forestsThe coal forestsTrees 40 metres tall, in swamps that become every coal seam on Earth. The air is 30% oxygen and the dragonflies are 70 cm across.295 Ma295 million years agoDimetrodonDimetrodonNot a dinosaur. A synapsid — our own branch, 60 million years before the first dinosaur.251.9 Ma251.9 million years agoThe Great DyingThe Great DyingSiberian basalt cooks the ocean. 81% of marine species die, in about 60,000 years — one and a half pixels.233–225 Ma233 to 225 million years agoThe first dinosaurs, and the first mammalsThe first dinosaurs, and the first mammalsBoth lines appear inside the same eight million years. At this scale, the same moment.201.4 Ma201.4 million years agoThe Triassic–Jurassic extinctionThe Triassic–Jurassic extinctionThe Atlantic starts to open. Half of everything dies, and the dinosaurs inherit it.150 Ma150 million years agoArchaeopteryxArchaeopteryxFeathers, and the first wing that works.125 Ma125 million years agoThe first flowersThe first flowersArchaefructus: no petals yet, but a flower — the oldest anyone can date. Before this, nothing was in bloom.68–66 Ma68 to 66 million years agoTyrannosaurus rexTyrannosaurus rexThe last and largest of the tyrannosaurs, gone within two million years of the asteroid.66.04 Ma66.04 million years agoChicxulubChicxulubEverything larger than a badger dies.56 Ma56 million years agoThe first true primatesThe first true primatesTeilhardina — not the primate-like mammals that came before it, but the first crown primate. It appears on three continents within 25,000 years, during a sudden burst of global heat.33.9 Ma33.9 million years agoAntarctica freezesAntarctica freezesThe greenhouse world ends. The modern icehouse begins.9.3–6.5 Ma9.3 to 6.5 million years agoThe human line splits from the chimpanzeesThe human line splits from the chimpanzeesEverything you would call human happens after this point — the next 175 pixels.
1.8 – 0.8 billion years ago
The Boring Billion
geologists' name for it
The chemistry settles. The oxygen stops rising. Nothing much happens for a thousand
million years.
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This stretch is 25,000 pixels long — a fifth of the page — and holds four arrivals. The longest gap
between them is 15,000 pixels: 600 million years in which nothing on this page happens.
The ending. Everything below happened in the last 175 pixels of this page. The thirty moments you
have passed are listed first, in order. Then ten more. Those ten are drawn nowhere on the page
above, because at 40,000 years to the pixel they all fall inside its final 110 pixels — and the last of them, everything humans have farmed, written,
built or remembered, is three tenths of one pixel.
The last ten happened in the final 110 of 115,000 pixels. Everything humans have farmed, written, built or remembered is the last three tenths of one pixel.
Two things on this page came within a rule of being cut. Tyrannosaurus rex sits 49 pixels from the asteroid; the first primates sit 251 — both closer than the 600-pixel floor allows anywhere else on this page, and both stayed anyway.