All the isotopes from the decay chains exist in these rocks. The most important are the dangerous isotopes of radium and radon.
Ultimately lead, as it is the only element in the uranium decay chains with isotopes that are stable. Specifically the isotopes 206, 207, and 208; each of which is the end of a different decay chain.
Uranium isotopes could be used to date rock of this age if they are present in the rock.
A higher percentage of daughter isotopes present in a sample, the older the rock is.
A+ Sedimentary
age... parent and daughter isotopes in relation to half life
Ultimately lead, as it is the only element in the uranium decay chains with isotopes that are stable. Specifically the isotopes 206, 207, and 208; each of which is the end of a different decay chain.
Yellowcake (a Uranium bearing rock).
Uranium isotopes could be used to date rock of this age if they are present in the rock.
Uranium rock
Uranium is a silvery-gray metallic chemical element in the actinide series of the periodic table that has the symbol U and atomic number 92. It has 92 protons and 92 electrons, 6 of them valence electrons. It can have between 141 and 146 neutrons, with 146 (U-238) and 143 in its most common isotopes. Uranium has the highest atomic weight of the naturally occurring elements. Uranium is approximately 70% denser than lead, but not as dense as gold or tungsten. It is weakly radioactive. It occurs naturally in low concentrations (a few parts per million) in soil, rock and water, and is commercially extracted from uranium-bearing minerals such as uraninite
A higher percentage of daughter isotopes present in a sample, the older the rock is.
Common minerals of uranium are: pitchblende, carnotite, autunite, coffinite etc.
what the bearing capacity for weather rock
A+ Sedimentary
age... parent and daughter isotopes in relation to half life
Well... none, but... Helium is often found in conjunction with uranium-bearing ores. The reason for this is that when heavy elements decay by the alpha process, they emit an alpha particle, which is a helium-4 nucleus. The amount of helium found in uranium-bearing rocks is therefore dependent on several factors: how much uranium is present, how long it's been there, what the geological conditions are (is the rock porous, is there an impervious dome structure to trap the helium, etc.) and many other things. For these reasons, it's very difficult to give an exact answer beyond noting that it's fairly common that where uranium is found, at least some helium will be found as well.
Radioisotopes are used by scientists to date rocks in a method called radiometric dating. The isotopes of an element are the atoms that have the same number of protons and electrons but different numbers of neutrons. When atoms of a radioactive isotope are included in the formation of a crystal, that crystal becomes the parent isotope. As the isotopes begin to decay, they become a daughter isotope. The convenient property of this phenomenon is that a certain parent isotope will ALWAYS decay to a certain daughter isotope. The rate of decay from parent to daughter isotope is called the half-life (time for half of the parent to become the daughter). Being familiar with and using isotopes such as Uranium-238, Uranium-235, and Carbon-14, scientists are able to calculate the age of a rock, fossil, etc. using the known half-life for each parent isotope.