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Relative dating ice cores

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Four environmental characteristics are encoded in these gas properties. Gases in glacial ice are trapped m below the surface of an ice sheet, as burial leads to densification and the sintering of ice grains. The uncompacted ice above the trapping depth or closeoff depth is a porous medium allowing molecular diffusion with little or no advection through most of its length. Under these conditions, the partial pressure of each gas or isotope will increase with depth according to the barometric equation, and the partial pressure of heavy gases or isotopes will increase faster than the light. In a diffusive medium, isotopes of gases will fractionate according to temperature gradients, with heavier isotopes generally enriched at the cold end. Snow is an effective insulator, so that, after temperature changes rapidly, there is a temperature gradient between the surface to the closeoff depth for about years, the length of time required for the new temperature to penetrate to the closeoff depth.
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Ice Cores and the Age of the Earth

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Absolute Ages of Rocks | Earth Science

Ice cores extracted from polar ice sheets and from glaciers worldwide are one type of paleoclimate proxy record - a source of data that tells us about past climates. Ice cores from glaciers and the polar ice caps are probably the most comprehensive type of proxy record of past climates. Physical and chemical analysis of ice cores provides information on temperature, precipitation, atmospheric aerosols such as dust and volcanic ash , and even levels of solar activity. Ice cores can provide data with a resolution as fine as yearly, and some records span periods of hundreds of thousands of years. Continuous climate records embedded in ice form in areas where year-round cold temperatures prevent fresh accumulations of snowfall from melting in the summertime.
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How do Ice Cores relate to the Age of the Earth?

Studying past changes in atmospheric gases is just so much easier when you can pluck a bubble of air dutifully archived by the ice, which acts like a relative with an inconveniently large collection of National Geographics. Ice cores in Greenland can only go back about , years, and the oldest so far core from Antarctica goes back about , years. If we could go a little further back in time, about 1.
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Oxygen is one of the most significant keys to deciphering past climates. Oxygen comes in heavy and light varieties, or isotopes, which are useful for paleoclimate research. Like all elements, oxygen is made up of a nucleus of protons and neutrons, surrounded by a cloud of electrons. All oxygen atoms have 8 protons, but the nucleus might contain 8, 9, or 10 neutrons. The ratio relative amount of these two types of oxygen in water changes with the climate.
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