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In particular, the impact of current environmental change on the nature of Earth Surface Processes is hardly predictable.It is a high priority challenge for modern earth sciences to better understand such processes.
When one of these particles strikes an atom it can dislodge one or more protons and/or neutrons from that atom, producing a different element or a different isotope of the original element.
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.
We apply the full spectrum of cosmogenic nuclides, including the routine extraction of A 3-dimensional model of the Mont Fort and Sivier glacier system, showing well-preserved 'Egesen' and 'pre-Egesen' moraine systems that are studied to understand the glacier and climate changes during the Late Glacial Period (14.5 - 11 ka ago) in the Swiss Alps.
Here is a list of radioisotopes formed by the action of cosmic rays; the list also contains the production mode of the isotope.
Surface exposure dating is a collection of geochronological techniques for estimating the length of time that a rock has been exposed at or near Earth's surface.