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The study of fossils and the exploration of what they tell scientists about past climates and environments on Earth can be an interesting study for students of all ages.

Teaching about Earth's history is a challenge for all teachers.

Carbon 14 is continually being created in the Earth's atmosphere by the interaction of nitrogen and gamma rays from outer space.

Since atmospheric carbon 14 arises at about the same rate that the atom decays, the Earth's levels of carbon 14 have remained constant.

Other corrections must be made to account for the proportion of throughout the biosphere (reservoir effects).

There are many methods employed by these scientists, interested in the old, to get to know the age of items..boxy-content a.term-action, button.term-action a.term-action:hover, button.term-action:hover .term-action-bg .term-uex .term-cite .term-fc .term-edit .boxy-dflt-hder .definition .definition a .definition h2 .example, .highlight-term a.round-btn, a.round-btn.selected:hover a.round-btn:hover, a.round-btn.selected .social-icon a.round-btn .social-icon a.round-btn:hover a.round-btn .fa-facebook a.round-btn .fa-twitter a.round-btn .fa-google-plus .rotate a a.up:hover, selected, a.down:hover, selected, .vote-status .adjacent-term .adjacent-term:hover .adjacent-term .past-tod .past-tod:hover .tod-term .tod-date .tip-content .tooltip-inner .term-tool-action-block .term-link-embed-content .term-fc-options .term-fc-options li .term-fc-options li a .checkmark .quiz-option .quiz-option-bullet .finger-button.quiz-option:hover .definition-number .wd-75 .wd-20 .left-block-terms .left-block-terms .left-block-terms li .no-padding .no-padding-left .no-padding-right .boxy-spacing @media (min-width: 768px) @media (max-width: 768px) @media print { a:link:after, a:visited:after nav, .term-action, #wfi-ad-slot-leaderboard, .wfi-slot, #related-articles, .pop-quiz, #right-block, .Collins English Dictionary - Complete & Unabridged 2012 Digital Edition © William Collins Sons & Co. A form of radiometric dating used to determine the age of organic remains in ancient objects, such as archaeological specimens, on the basis of the half-life of carbon-14 and a comparison between the ratio of carbon-12 to carbon-14 in a sample of the remains to the known ratio in living organisms. A technique for measuring the age of organic remains based on the rate of decay of carbon 14.The carbon 14 present in an organism at the time of its death decays at a steady rate, and so the age of the remains can be calculated from the amount of carbon 14 that is left. The cells of all living things contain carbon atoms that they take in from their environment.

What is the definition of relative age dating