Holocene environmental changes in the central highlands of Iceland as recorded in soils
Across the central highlands of Iceland soil sections are accessible in rofabörð were they can reach back to the time of initial soil formation after the deglaciation around 11.5 ka. These soil sections have been used to reconstruct tephrochronology and also to study soil erosion in Iceland. The mai...
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Format: | Thesis |
Language: | English |
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2018
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Online Access: | http://hdl.handle.net/1946/31875 |