Syn‐ and post‐eruptive gully formation near the Laacher See volcano

نویسندگان

چکیده

The Laacher See volcano (LSV) is located at the western margin of Neuwied Basin, central part Middle Rhine Basin Germany. Its paroxysmal Plinian eruption c. 13 ka ago (Laacher event; LSE) deposited a complex tephra sequence in whilst distal ashes became one most important chronostratigraphic markers Central Europe. However, some other impacts on landscape formation have thus far been largely neglected, such as buried gully structures proximity LSV. In this contribution, we map and discuss spatial extent these landforms site Lungenkärchen 4 km south LSV based geophysical prospection well contrasting pedo-sedimentary characteristics infill (particle-size distribution, bulk-sediment density, thin-section analysis, saturated hydraulic conductivity) surrounding soils layers. These data are combined with luminescence- carbon-14 (14C)-based age model that relates them to LSE. It demonstrated how gullies seem formed rapidly infilled by rainfall surface discharge both during subsequent eruptive phase, modern analog processes documented for 1980 Mount St Helens (Washington State, USA). Given density their deviating properties compared soils, propose significant influence agricultural production LSV, which remains be tested future studies. Finally, contrast, similar lateral vertical dimensions identified post-LSE reworked loess deposits Wingertsbergwand (close main study proximal LSV) shown unrelated LSE can either attributed periglacial Younger Dryas-Preboreal transition or linear incision early Holocene.

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ژورنال

عنوان ژورنال: Earth Surface Processes and Landforms

سال: 2021

ISSN: ['1096-9837', '0197-9337']

DOI: https://doi.org/10.1002/esp.5119