Cosmogenic dating

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Nuclide isotope 10 Be is the most widely used one in the application of reconstructing glacial chronology [52].

This can lead to previously hidden faces of the boulder being exposed, and again can lead to errors in age estimation.

Lacked by Subrat Hi Subrat, One is a salaried individual.It measures the concentration of the targeted isotope that is only produced by the interaction of cosmic rays with minerals in rocks and then calculates the surface exposure time of the rock [48][49][50] [51].Cold-based glaciers in Antarctica may transport erratic boulders slowly but may apply minimal erosion.Terrestrial cosmogenic nuclides are produced by interactions between secondary cosmic rays and near surface rocks.Our research interests cover a wide spectrum of earth scientific disciplines and include timing of ice ages, subglacial erosion rates, uplift rates of Pleistocene terraces, and a better understanding of the production systematics of cosmogenic nuclides.

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