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EW93-40GGC

Core EW93-40

Site: 41°39.043'N by 51°00.972'W
Water Depth: 3722 m

In order to look for "markers" in the core, we must take small amounts of the mud in little layers. There are several ways to process the mud, but eventually it is looked at through a microscope. The white strips are styrofoam placed where a sample was taken to give support to the layers of mud remaining in the tray. This is necessary because it is highly probable that another scientist will want to sample the core to correlate new data.

This core, taken on the Newfoundland Ridge, clearly displays the red hue of hematite-stain grains. This section of core is deep into the sediment and thus older in "time" than our discussion. This fact shows that transport of ice-rafted detritus is a process that is recorded back in time. The grains appear, then disappear in cycles.



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For more information, contact Rusty Lotti Bond (curator@ldeo.columbia.edu). Comments are welcomed. Last update of this page was January 20, 2001.