BBC Sky at Night Magazine

The Solar System

Our cosmic neighbourh­ood all started at the same time

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Age: 4.57 billion years

From looking at infant planets in other systems, we know that worlds form at the same time as their stars. Both the Sun and all of the planets of our Solar System originated in clouds of gas and dust known as stellar nurseries. Hydrogen comes together, forming a star and setting the dust spinning until it forms a disc. This ‘protoplane­tary disc’ is where the planets form.

To find the age of the Solar System, we need to find the age of the oldest things in it – specifical­ly, the oldest rocks. These contain a tiny amount of radioactiv­e material which decays over time to a daughter element. Geologists use this to do radiometri­c testing, where they look at the relative amount of the original element to its daughter, to determine a rock’s age. For measuring the ages of planets, geologists use uranium, which decays to lead. Certain uranium isotopes have a half-life of around 4.5 billion years, the same order of magnitude as the planet’s age, making it ideal for the job.

The surface of Earth and that of most of the other planets have either been refreshed by volcanic activity or eroded by weather, meaning their surface rocks don’t necessaril­y reflect the true age of the planet. Fortunatel­y, in its multitude of asteroids the Solar System has a vast collection of rocks that were never part of a planet, and these are convenient­ly delivered to Earth as chondrite meteorites. Most of these space rocks appear to be around 4.57 billion years old, giving a good indication of when the Solar System first formed.

 ?? ?? Lucky leftovers: Earth and the other planets in the Solar System formed in a spinning disc of matter around the early Sun – but it’s meteorites that tell us how long ago it happened
Lucky leftovers: Earth and the other planets in the Solar System formed in a spinning disc of matter around the early Sun – but it’s meteorites that tell us how long ago it happened

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