Codeman said:
Ok, I know this has probably been asked...
I have been reading in my Geology Text Book- says Earth is 200mill ys old. I say "ok, why?"
So... Can anyone list all, or at least most of the methods that can be used to date the earth. I know there is Radiosomethingrather, but can I get some more, along with the age that those methods estimate it at. I know none of them are entirely accurate, but I am looking to see if I can find an average or something...ok?
thanx
Codeman
Actually the Earth is 4500 million (aka 4.5
billion) years old, so either your geology text is way out of date or it is referring to a specific geological feature that is only 200 million years old.
Radiometric dating is the method of choice for getting an absolute age of the earth and any of its geological features. But it is limited to dating igneous formations (e.g. lava flows). It cannot directly measure sedimenatary rocks, so they have to be dated relative to (i.e. older or younger than) a datable igneous formation.
For all other really old dates, one has to use relative dating. This can tell you which formation is older than another so you get strata in the right chronological order, but only rough estimates of how old they are.
Stratigraphy was one of the first recognized ways to do relative dating. Back in the 17th century Nicolas Steno recognized that 1) sedimentary rock is always laid down in horizontal layers, and 2) younger sedimentary rock is always formed on top of older sedimentary rock.
He also formulated the relationship between objects found in rock and intrusions into rock layers. He recognized that when two objects come together, the harder object will leave an impression on the softer object. So "veins" of gold or other metal in mines, take the shape they do because the mineral ore was soft when it intruded into the interstices between older, already hardened rock. While fossils of teeth, shells, etc. must have been first buried in soft material such as sand or mud which hardened around them. This means a fossil is always as old or older than the rock it is encased in.
That takes us to another means of relative dating: faunal succession and the correlation of fossils. This was discovered by William Smith in the early part of the 19th century. Like Steno he noted that certain strata are always in a constant relation, with younger rock on top of older rock. He also noted that each major rock stratum had its own particular set of fossils. The fossils found in Cambrian strata were different from those found in Devonian strata which were different again from those in Carboniferous strata, and so on. He got to the point that he could predict which fossils would be found in a rock formation just by looking at the relative position of the formation. Or vice versa, could tell which period of time a fossil came from just by examining the fossil.
Smith did all his work in England, but his principle has been found to be true globally. So index fossils (those which are found only in one particular period) are a key to relative dating of sedimentary rock.
A third method of relative dating relies on estimating the time it takes to build up certain types of rock or to erode it. We can measure, for example, how long it takes coral to build up a reef. So when we find formations of limestone made by coral, we can estimate how long it took to form. Similarly, we can measure how long it takes for a river to dig a channel into its streambed. And so estimate how long it took for a canyon to form. This method has to be used with care, as some processes (like those above) take a long time, but some can be rapid. As you continue to study geology you will learn how to distinguish between the slow and the rapid processes.
Dates can also be derived from measuring cyclical processes, such as annual snow accumulation (ice cores) annual varves, annual tree rings.
I believe paleomagnetism may be another indication of date, but I don't know for sure.
I expect a professional could also name others and give more precise detail on these.