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About Quaternary Studies
Masters degrees in Quaternary Studies offer advanced study of the historical properties and processes which formed Earth as we know it today. They offer an interdisciplinary approach, examining the lithosphere, hydrosphere, atmosphere, biosphere and cryosphere.
Related postgraduate specialisms include Quaternary Archaeology and Human Evolution. Entry requirements normally include an undergraduate degree such as Environmental Science.
Courses in Quaternary Science investigate the climatic and geological changes associated with repeated ice ages, and the rise of the human species. Their purpose is to help professionals understand current environmental changes, and anticipate future changes.
Training includes methods for creating a time-scale of the geologic past, using dating and surveying methods to create high-resolution paleoenvironmental records. For example, you may examine multi-proxy evidence to reconstruct past environments. Samples may include ice cores, tree rings, sub-fossil pollen, boreholes, corals, lake and ocean sediments, and carbonate speleothems (cave formations).
These samples will help you to formulate theory surrounding the formation of rock systems and continental-scale ice sheets, and assess major changes in sea level and major migrations of animal and plant communities. It may also include analysis of the evolution and extinction of different species.
Careers may include environmental assessment, conservation, legislation and public policy.
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Study Quaternary Science at Royal Holloway, University of London and you’ll receive comprehensive postgraduate training on the time-dependent processes that affect environmental change, helping you to understand and confront some of the most profound issues of our time. Read more
From the spectacular igneous geology of the Lake District World Heritage Site and Northumberland National Park to the Yorkshire Jurassic ‘Dinosaur Coast’ and the mineral wealth of the Pennines, the North has an incredible geological history spanning almost 500 million years. Read more