How old is our planet, Earth? It’s old. Really old. Mind-staggeringly, head-hurtingly old. In a minute I will give you one useful number that will help you understand how old and how all the rest of history fits into the picture.
Before I do that lets talk about big numbers. What is the biggest number you can imagine? I can imagine 10 things with no problem at all. 100. Yep, easy. 1000? There were nearly 1000 people at my senior school so I can think of that number. How about 100 schools like that put together, so 100 000? Its possible to think of that. Ten of those is 1 000 000 - one million. I stop there. That is about the limit of what I can imagine but that is good enough for now.
So imagine those numbers in terms of years. I don’t know about you, but for me that is a bit harder. I’ve lived for 41 years so even 100 years is a long time. 1000 years ago we know our country was in Saxon times just before the Normans invaded in 1066. 10 000 years ago we are beyond written human history so we don’t have stories from those times about what people were doing then. 1 million years seems like an incredibly long time to think of, doesn’t it?
Well our magic number is four thousand five hundred and forty. 4540. Because the Earth is around 4540 of those 1 million years old! But 4540 is a simple number and it will be very helpful to remember when later on we talk about fossils and dinosaurs and such like.
The picture at the top of this post shows how some people talk about time in the Earth’s long lifetime. These four really long periods of time are called eons. There are other ways of describing the Earth’s many ages and we will talk about them another time. The start and end of these ages can be said to have happened so many millions of years ago, which can be written MYA. So for example the beginning of the Phanezoic eon, the eon we are living in now, began 542 million years ago or 542MYA. This is the age where the first plant and animal fossils were found - before that there were probably only tiny microscopic bacteria and viruses that lived on our planet. You’ll see from the picture that plants and animals came quite late on the scene in Earth’s lifetime.
How do we know how old the Earth is? There are a number of different ways we know but I’ll tell you one way that you’ll understand if you’ve read my other posts about what stuff is made of. There is a type of metal in some of the rocks in the Earth called Uranium. Like all materials it is made of lego-brick like atoms. Uranium atoms are a bit unstable, but only a bit. From time to time one atom will suddenly change into another one - a lead atom. Lead is a metal too and in very old houses water pipes used to be made of it. Actually it changes into a misfit isotope lead atom not a regular normal one. It doesn’t happen very often. In fact if you took a lump of uranium of any size it would take 700 million years for half of the atoms in that lump to turn to lead. By measuring how much misfit lead isotope is in meteorites and moon rock - which we think were made at the same time as the Earth - then we can work backwards and know when that rock was made. So far all the rocks we have tested point to a number about 4500 million years.
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