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Optically stimulated luminescence dating of fluvial deposits a review

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The trapping sites are imperfections of the lattice — impurities or defects.

The ionizing radiation produces electron-hole pairs: Electrons are in the conduction band and holes in the valence band.

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Glacigenic sediments present considerable challenges for OSL dating not only in terms of poor bleaching of the OSL signal during the transport and deposition cycle, but also poor quartz luminescence characteristics which are often related to sediment provenance, the nature of the bedrock or source material, and the freshly eroded nature of many such deposits.

Under stimulation of light the electrons may free themselves from the trap and get into the conduction band.

Seeking mechanistic, quantitative understanding of the form and evolution of landscapes.

In addition, we are seeking linkages between ecological and geomorphic processes, and building tools to tackle pressing environmental problems.

While this definition of the Palouse remains common today, the term is sometimes used to refer to the entire wheat-growing region, including Walla Walla County, the Camas Prairie of Idaho, the Big Bend region of the central Columbia River Plateau, and other smaller agricultural districts such as Asotin County, Washington, and Umatilla County, Oregon.

This larger definition is used by organizations such as the World Wide Fund for Nature, who define the Palouse Grasslands ecoregion broadly.