Frost peat mounds on Hermansenøya ( Oscar II Land, NW Svalbard) – their genesis, age and terminology
Here we present research on previously uninvestigated frost peat mounds occurring on a peat bog in the southern part of H ermansenøya, NW S valbard. Detailed characteristics are given of the environmental conditions of the peat bog and of the morphological features and surface structure of the frost...
| Published in: | Boreas |
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| Main Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Wiley
2012
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1111/j.1502-3885.2012.00252.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.2012.00252.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.2012.00252.x https://onlinelibrary.wiley.com/doi/full-xml/10.1111/j.1502-3885.2012.00252.x |
| Summary: | Here we present research on previously uninvestigated frost peat mounds occurring on a peat bog in the southern part of H ermansenøya, NW S valbard. Detailed characteristics are given of the environmental conditions of the peat bog and of the morphological features and surface structure of the frost peat mounds, as well as an analysis of the internal structure of one mound. Three types of frost peat mounds have been distinguished: disc‐shaped mounds (low), mid‐sized mounds with gentle sides, and high mounds with steep sides. Radiocarbon dating of the peat within the frost peat mound performed for the first time on S valbard and a detailed analysis of the deposits demonstrated that in the high mound (1.3 m) there is an ice‐peat core and peat cover without ice. There are three layers of peat of different ages separated by at least two hiatuses. A generalized history of the development of the peat bog from about 8 ka BP is established. The studied mound displays two development cycles unknown elsewhere. The older relict part of the peat mound was formed during a climatic cooling about 3.0–2.5 ka BP , while the younger part originated during the L ittle I ce A ge ( c . AD 1550–1850). Despite certain similarities of these mounds to some palsas, this term should not be applied to the mounds because they are smaller and their cores consist mostly of layers of massive injection ice, the presence of which indicates a pressurized system in their genesis. |
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