We would need a comparison to determine what an old rock looks like as in comparison to a young one. Or else how can we look at a rock and tell its age?
Several ways. Off the top of my head:
- radiometric dating. Through
various methods, you can directly measure the time that's passed since the rock cooled from molten material.
-
stratigraphy. Looking at how rock is arranged in layers will tell you the order in which these layers were created.
- for sedimentary and metamorphic rocks, knowledge of the processes that created them. Sedimentary rock formation takes time... lots of time; this can give you a minimum age for a particular rock. Depending on the specific type of rock, metamorphic rock formation takes either time, specific conditions, or both. If the proper conditions haven't occurred in that area for X million years, then we can conclude that the rock formed at least that long ago.
- crystal direction. As I've pointed out to you in other threads, the crystal structure of many rocks will align with the Earth's magnetic field when it forms. This can tell you which direction was north when the rock was formed, which tells you what orientation the continent had at the time, which can be used to figure out when this was.
So... except for the first method, it's not normally just a matter of plunking a rock down on a lab bench and saying "how old is this?" Generally, it's a matter of looking at a rock in the context of the other rocks around it and its larger environment.