Which of the following is related to relative dating

Relative dating places events or rocks in their chronologic sequence or order of occurrence.Absolute dating places events or rocks at a specific time.The most common relative dating method is stratigraphy.Other methods include fluorine dating, nitrogen dating, association with bones of extinct fauna, association with certain pollen profiles, association with geological features such as beaches, terraces and river meanders, and the establishment of cultural seriations.Ask yourself how the things that are happening in the world today might end up being recorded in the sediments that are now or soon will be deposited.How would today's sediments appear to a geologist millions of years in the future examining outcrops of sedimentary rock that originated in our time?

This also applies to rocks, minerals, and derivative materials (such as sediments and soil).The age of formations is marked on a geologic calendar known as the geologic time scale.Development of the geologic time scale and dating of formations and rocks relies upon two fundamentally different ways of telling time: relative and absolute.Relative Dating Superposition: The most basic concept used in relative dating is the law of superposition.Simply stated, each bed in a sequence of sedimentary rocks (or layered volcanic rocks) is younger than the bed below it and older than the bed above it.

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