Exploring Earth Creationist Claims for the Age of the Earth :: Creationism Science Essays

The relative age of the primer coat is not often seen as a topic of controversy. Much of the scientific data published in school textbooks and taught to students indicate an age on the order of billions of years. Radiometric dating, as fountainhead as geological rock studies, have been used as assure to support such a large expanse of time. However, a meek but determined minority, mostly composed of fundamentalist Christians, has been vehemently gainsay this age. These so- constituteed trigger-scientists have disputed the evidence in support of a young person earth. They have added their own measurements and observations, as well as construe other scientists data, in an attempt to convince others of the possibility and ultimately, the truth of a young earth, one that is no more than 6,000 to 10,000 years old. The young earth idea has its roots in the Bible. If the lineages and families were traced back from known dates in the not-to-di stant past, the creation of the world by the eternal Creator would have been around 4000 B.C. Because these creationists call their endeavors scientific, the question arises as to their method for making the claim of a young earth. Creation-science discussions of the age of the earth usually contain several standard items. The first-class honours degree is usually a criticism of the standard evolutionist methods for age determination, radiometric dating. Radiometric dating is the march of determining the age of a substance based on the symmetry of isotopes in a given sample. The number of protons in the nucleus of an fraction defines a particular element. However, the number of neutrons in the nucleus can vary, bad rise to different isotopes of the same element. Some of these isotopes argon stable, while others are not. These unstable isotopes radioactively decay to more stable, often lighter elements, called fille atoms, thereby releasing energy in the form of high-energy particles or electromagnetic waves. A particular isotope will have a device characteristic half-life, based on the time that it takes for half of the population of the isotope to decay into the fille elements.