This information is vital for numerical models, and answers questions about how dynamic ice sheets are, and how responsive they are to changes in atmospheric and oceanic temperatures. Unfortunately, glacial sediments are typically difficult to date. Most methods rely on indirect methods of dating subglacial tills, such as dating organic remains above and below glacial sediments. Many methods are only useful for a limited period of time for radiocarbon, for example, 40, years is the maximum age possible.
Precision and accuracy in glacial geology
11,Year-Old Seafaring Indian Sites Discovered on California Island – Western Digs
Wikimedia Commons We can indirectly date glacial sediments by looking at the organic materials above and below glacial sediments. Radiocarbon dating provides the age of organic remains that overly glacial sediments. It was one of the earliest techniques to be developed, during the s. Radiocarbon dating works because an isotope of carbon, 14C, is constantly formed in the atmosphere by interaction of carbon isotopes with solar radiation and free neutrons.
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