CHANGES IN DEPOSITION ON A COLLUVIAL FAN DURING THE UPPER HOLOCENE IN THE TINDASTÓLL MOUNTAIN, SKAGAFJÖRÐUR DISTRICT, NORTH ICELAND: PRELIMINARY RESULTS |
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| Authors: | ARMELLE DECAULNE ÞORSTEINN SÆMUNDSSON HELGI PÁLL JÓNSSON OLGA SANDBERG |
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| Institution: | Geolab UMR6042-CNRS, 4 rue Ledru, 63057 Clermont-Ferrand cedex 1, France and Natural Research Centre of Northwest Iceland, Aðalgata 2, IS-550 Sauðárkrókur, Iceland;E-mail:;Natural Research Centre of Northwest Iceland, Aðalgata 2, IS-550 Sauðárkrókur, Iceland;E-mail:;Natural Research Centre of Northwest Iceland, Aðalgata 2, IS-550 Sauðárkrókur, Iceland;E-mail:;Natural Research Centre of Northwest Iceland, Aðalgata 2, IS-550 Sauðárkrókur, Iceland, and Lantmäteriet, Luleå, Sweden;E-mail: |
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| Abstract: | This study investigates variability in depositional processes and landforms on the Innstaland colluvial fan, northern Iceland, over the late Holocene. This is completed using geomorphological mapping, historical records and relative‐age dating tools (vegetation survey, rock hardness and tephrochronology). Debris flows are the main contributors to fan development. Six main phases of deposition are distinguished, varying in deposit magnitude along a general trend of decreasing magnitude over time. With the help of dated tephra layers, the aggradation rates of the fan are calculated for the upper Holocene and in particular over the historical period (post‐ AD 1104). An episodic sediment transfer system is reconstructed, with several phases of low activity between more rapid aggradational episodes. The interpretation of the colluvial deposits suggests that the main phase of aggradation on the fan ended during the historical period after which incision started (between AD 1300 and 1766). Incision tracks act as the main pathways for debris distribution at the present time. These variations are related to the changing response of the catchment system over time. |
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| Keywords: | colluvial fan field survey Schmidt hammer tephrochronology upper Holocene aggradation incision |
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