Ice core dating techniques

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Magnificent

(18)
Elegant
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About me

Ice cores are obtained by drilling core samples of ice in regions where glaciation has occured, such are near the Arctice and Antarctic Circes. Visible light and dark rings can be found in such cores that are then analyzed to determine the age of the ice. These layers are presumed to be the result of annual fluxuations in climate, and using this method, uniformitarians purport ages of over , years. Creationists, such as Michael Oard , contend that these laminations are from subannual events, including layering due to dust to be found in a post-flood ice age. The rapid rate at which ice sheets can accumulate is further demonstrated by the case of the Lost squadron [2]. In , P Lightning fighter planes ran out of gas and landed in Greenland. Then in , a group started looking for the planes. They finally found them in May, , under ft. Now it is true that neither of these is representative of the glaciers used for ice core analyses today, but they could have been representative of those glaciers in the past.

An ice core is a core sample that is typically removed from an ice sheet or a high mountain glacier. Since the ice forms from the incremental buildup of annual layers of snow, lower layers are older than upper, and an ice core contains ice formed over a range of years. Cores are drilled with hand augers for shallow holes or powered drills; they can reach depths of over two miles 3. The physical properties of the ice and of material trapped in it can be used to reconstruct the climate over the age range of the core. The proportions of different oxygen and hydrogen isotopes provide information about ancient temperatures , and the air trapped in tiny bubbles can be analysed to determine the level of atmospheric gases such as carbon dioxide. Since heat flow in a large ice sheet is very slow, the borehole temperature is another indicator of temperature in the past. These data can be combined to find the climate model that best fits all the available data.

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