On one hand, Relative dating methods present the temporal order of a sequence of materials, events or objects. These methods disclose whether these occurred before or contemporarily. Basically, these methods estimate whether an object is older or younger than other things found at the site however, it must be noted that relative dating does not provide specific dates. The methods used are stratigraphy, seriation, and fluorine dating. Advantage: It is a useful technique to determine the sequential order in which a series of events occurred. Disadvantage: It does not provide specific dates. On the other hand, absolute, or chronometric dating methods reveal the age, measured in calendar years, of materials, objects or events. These methods present more specific origin dates and time ranges [e.g. age range in years] unlike relative dating methods. These methods make use of aa variety of chemical or physical measurements to determine the time when events occurred or when materials and objects were made, used, or alternative dates. Although chronometric dates are still not exact dates, but there are numerical age estimations expressed as a range of dates about the occurrence and existence of events or objects. The methods used are radiocarbon dating, thermoluminescence, dendrochronology, fission-track