Relative dating is a methodological approach used to determine the chronological order of past events or objects without ascertaining their absolute age. It establishes the temporal sequence by examining the spatial relationships, stratigraphic positions, or other comparative characteristics of materials. This concept is fundamental in disciplines such as geology, archaeology, and paleontology for reconstructing historical timelines and understanding the relative succession of phenomena based on principles like superposition, cross-cutting relationships, and faunal succession.