I thought that I'd post on some of the lesser-known methods of dating materials. YECs, feel free to try to refute all of the methods that can date older than 6000 years. (Except for dad. We've all heard his stuff already.)
Uranium series
Range: approx. 10,000 to 800,000 years ago
Two isotopes of uranium (238 and 235) decay into other elements. In the case of U238, thorium 230, and for U235, protactinium 231. Of course, Th230 and Pa231 also decay. However, the uranium isotopes are soluble in water, while Th230 and Pa231 are not. For example, only the uranium isotopes are present in water that seeps into limestone case. However, once the calcium carbonate and uranium is precipitated onto the cave walls (known as travertine), the radioactive clock starts. When the travertine deposits are formed, they contain only the uranium isotopes and not the thorium or protactinium. Once the uranium is precipitated, though, the thorium and protactinium created through decay remains in the travertine deposits, and we can date the deposits based on our knowledge of the half-lives of uranium, thorium, and protactinium. Also, teeth can be dated using this method, as uranium "soaks" into the dentine coating of teeth after they are buried. This method has been used to date Neanderthal skeletons found in Israeli caves to approximately 100,000 years ago.
Fission track
Range: approx. 100,000 years ago and older
Fission track is based on the spontaneous fission of uranium 238, found in a large variety of rocks, minerals, glassy meteorites, and volcanic glass. U238 naturally decays, eventually to lead, but it also occasionally divides in half, with each half of the atom moving away at a very high speed, doing damage to the glass. The volcanic glass is polished and etched with acid, causing small fission tracks to become visible at high magnifications. As we know the rate of fission of U238, by counting the number of fission tracks and comparing them with artificially induced fission tracks of U235, scientists can determine the age of a material. Assuming the material is old enough, (around 100,000 years, old enough for a good quantity of tracks), the material can be dated to within +/- 10 percent.
Thermoluminescence and optical dating
Range: present to 100,000 years ago
This one is more difficult to explain without resorting to quite a bit of physics, but I'll try to keep it fairly simple. When atoms located within a crystal lattice, (basically, minerals), are exposed to nuclear radiation, (such as naturally-occuring cosmic radiation), single electroncs can and do absorb energy, become detached from their nuclei, and "trapped" within defects in the lattice (caused by missing atoms or impurities). As the amount of radiation absorbed remains relatively constant, the number of trapped electrons will gradually grow at a constant rate. By this, we can determine the total dose of radiation absorbed. By dividing the total dose by the annual dose, we can get an approximate age of the material.
Thermoluminescence dating is one method of emptying the "electron traps" by the application of heat. The material is rapidly heated to at least 500 degrees C, and energy lost by electrons as they are liberated from the traps is released as light, and known as thermoluminescence. The magnitude of the thermoluminescence is directly related to the number of trapped electrons.
Optical dating instead relies upon electron traps that are emptied by light. Most minerals have a set of electron traps that are "bleached" by several minutes exposure to sunlight. After burial, they begin to accumulate electrons again. Instead of heating the material to determine the number of electrons, it is instead illuminated and the electron luminescence is measured.
I'm taking a quick break, and I'll post the other methods in a bit.
Uranium series
Range: approx. 10,000 to 800,000 years ago
Two isotopes of uranium (238 and 235) decay into other elements. In the case of U238, thorium 230, and for U235, protactinium 231. Of course, Th230 and Pa231 also decay. However, the uranium isotopes are soluble in water, while Th230 and Pa231 are not. For example, only the uranium isotopes are present in water that seeps into limestone case. However, once the calcium carbonate and uranium is precipitated onto the cave walls (known as travertine), the radioactive clock starts. When the travertine deposits are formed, they contain only the uranium isotopes and not the thorium or protactinium. Once the uranium is precipitated, though, the thorium and protactinium created through decay remains in the travertine deposits, and we can date the deposits based on our knowledge of the half-lives of uranium, thorium, and protactinium. Also, teeth can be dated using this method, as uranium "soaks" into the dentine coating of teeth after they are buried. This method has been used to date Neanderthal skeletons found in Israeli caves to approximately 100,000 years ago.
Fission track
Range: approx. 100,000 years ago and older
Fission track is based on the spontaneous fission of uranium 238, found in a large variety of rocks, minerals, glassy meteorites, and volcanic glass. U238 naturally decays, eventually to lead, but it also occasionally divides in half, with each half of the atom moving away at a very high speed, doing damage to the glass. The volcanic glass is polished and etched with acid, causing small fission tracks to become visible at high magnifications. As we know the rate of fission of U238, by counting the number of fission tracks and comparing them with artificially induced fission tracks of U235, scientists can determine the age of a material. Assuming the material is old enough, (around 100,000 years, old enough for a good quantity of tracks), the material can be dated to within +/- 10 percent.
Thermoluminescence and optical dating
Range: present to 100,000 years ago
This one is more difficult to explain without resorting to quite a bit of physics, but I'll try to keep it fairly simple. When atoms located within a crystal lattice, (basically, minerals), are exposed to nuclear radiation, (such as naturally-occuring cosmic radiation), single electroncs can and do absorb energy, become detached from their nuclei, and "trapped" within defects in the lattice (caused by missing atoms or impurities). As the amount of radiation absorbed remains relatively constant, the number of trapped electrons will gradually grow at a constant rate. By this, we can determine the total dose of radiation absorbed. By dividing the total dose by the annual dose, we can get an approximate age of the material.
Thermoluminescence dating is one method of emptying the "electron traps" by the application of heat. The material is rapidly heated to at least 500 degrees C, and energy lost by electrons as they are liberated from the traps is released as light, and known as thermoluminescence. The magnitude of the thermoluminescence is directly related to the number of trapped electrons.
Optical dating instead relies upon electron traps that are emptied by light. Most minerals have a set of electron traps that are "bleached" by several minutes exposure to sunlight. After burial, they begin to accumulate electrons again. Instead of heating the material to determine the number of electrons, it is instead illuminated and the electron luminescence is measured.
I'm taking a quick break, and I'll post the other methods in a bit.