This map shows the Earth as it looked at any given moment. Slide through time and the continents move with you. Below you can read, for each part, where it comes from and how certain it is — because some things are measured and others reconstructed, and you should be able to see the difference.
The map itself
The coastlines are not one world map slid backwards, but fifteen real reconstructions reaching back a billion years. Between them the map blends smoothly, so land that disappears fades away instead of jumping.
The places on the map travel too: where the Chicxulub impact happened is not where that spot lies today. Sixty-six million years ago it sat almost twenty degrees further west.
The lighter sea along the coasts is an estimate, not a measurement. Continents fit together along their underwater edge, not along the beach — without that margin, Pangaea would show gaps while it was one landmass.
On the flat map everything near the poles looks far larger than it is. That is not a mistake but the result of flattening a round Earth; on the globe it is right again.
What you can switch on
Satellite image
A photograph of today's Earth (NASA), laid over the globe. Useful for seeing where something is, but it belongs to today: the further back you slide, the less it holds.
Sea level and ice ages
How high the water stood, from sea-floor drill cores. During the last ice age sea level was over a hundred metres lower and you could walk dry from France to England. Switch this on and the shallow water falls dry as soon as the level is low enough.
Tectonic plates
The seams along which the Earth's crust lies in pieces. That is where the earthquakes happen and the volcanoes stand — so these lines explain the dots in the next layer.
Depth of the sea
Five depth contours, from the edge of the continental shelf at two hundred metres to the trenches at six kilometres. The darker the water, the deeper. This is the shape of today's sea floor.
Volcanoes, earthquakes and tsunamis
Real events from the hazard databases of the American ocean service and the geological survey, with name and year. They appear at the moment they happened; the further back, the less was written down.
Ocean currents
The great circulation of warm and cold water that drives the climate: warm water flows north at the surface, cools near Iceland, sinks, and returns at depth. This was traced by hand from the Woods Hole institute's chart — a diagram, not a measurement.
Forest
Where the forests stand, derived from satellite imagery: for every cell, how green it is in August and in January. That is the forest of today; how it looked in the past this source cannot tell us.
Mountains, deserts, steppes, highlands, basins and tundra
The great landscapes by name, from the open map collection Natural Earth. Each kind stands on its own, so you can switch on deserts without the mountains.
Ice
The ice caps as they lie now. For the ice of the ice ages the sea level layer is the better measure: it shows how much water was locked up in ice back then.
Rivers and lakes
The major rivers and lakes of today, also from Natural Earth.
Borders through time
Fifty-three maps of empires and countries, from long before the common era to now. Borders from antiquity are always an interpretation: empires had spheres of influence, not boundary posts.
Cities
Over five thousand cities from Wikidata, with their founding year and their censuses. A city appears when it comes into being, grows with its population and disappears when it is abandoned. For the time before the first census, the growth is a line, not a figure.
Beyond the Earth
The planets
The orbits come from NASA's Jet Propulsion Laboratory, from the table reaching from 3000 BC to 3000 AD. Outside that range Discovery still draws the orbits but no planets: where a planet stood then can no longer be worked out.
The Moon and the satellites
The Moon's position comes from the short series in the Astronomical Almanac — good to the day, not to the hour. The satellites are CelesTrak's public orbital elements: the orbits are right, the position along them is one day's state, and you only see what is still going round today.
Stars and constellations
Almost nine thousand stars from David Nash's HYG catalogue (Hipparcos, Yale and Gliese merged), used under CC BY-SA 4.0. The constellation lines come from Olaf Frohn's d3-celestial, under a BSD licence. Both the precession of the Earth's axis and each star's own motion are taken into account; beyond a hundred thousand years it stops, because by then today's stars are unrecognisable.
Space probes
Positions from NASA/JPL's Horizons. Unlike a planet or a comet, there is no fixed orbit here: a probe that grazes Jupiter is flung onto a new path, so no single calculation covers the whole journey. This is therefore a series of stored positions, close together where the path bends and far apart on the straight stretches. Checked against nine flybys: each time the probe sits within a few million kilometres of the planet it passed. The series runs until JPL stops calculating — 2100 for the Voyagers, 2050 for the Pioneers and New Horizons. After that they fly on, but we no longer know where to.
Comets, asteroids and meteor showers
Comets and asteroids come from NASA/JPL's Small-Body Database. Their orbit is right, but the position along it drifts: Jupiter tugs at them and that is not in the calculation — for Halley that means two days off in 1986 and a few months in 2061. The meteor showers are the eleven known annual showers with their radiant; they are shown only for the centuries in which they exist.
What is not in it
Height differences on land, the shallow seas that once lay over them, and the weather. Beyond that: everything that changes through time is well recorded for the recent centuries and a reconstruction for deep time. A small clock beside a layer means that layer moves with the time bar.