ph th, Sto ociet north ABSTRACT: Several tephra layers from the last millennium have b work of ithin th Iceland, but distal layers from Jan Mayen have also been identified. The predominant transport A key objective of palaeoclimate research is to examine lead nts between sparsely located records. He...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.666.6758 http://su.diva-portal.org/smash/get/diva2%3A275870/FULLTEXT01/ |
| Summary: | ph th, Sto ociet north ABSTRACT: Several tephra layers from the last millennium have b work of ithin th Iceland, but distal layers from Jan Mayen have also been identified. The predominant transport A key objective of palaeoclimate research is to examine lead nts between sparsely located records. Here we summarise the key tephras that can be used descriptions of distal fallout of tephra from Icelandic eruptions are from documentary records (Connell, 1846; Mohn, 1878) and many of these observations were compiled by Thorarinsson |
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