Universität zu Köln

Engel, Max ORCID: 0000-0002-2271-4229, Dotterweich, Markus, Fuelling, Alexander, Brill, Dominik, Broisch-Hoehner, Manuela, Totschnig, Ralf, Seren, Sirri and Kehl, Martin ORCID: 0000-0003-4587-5858 (2021). Syn- and post-eruptive gully formation near the Laacher See volcano. Earth Surf. Process. Landf., 46 (9). S. 1783 - 1797. HOBOKEN: WILEY. ISSN 1096-9837

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Abstract

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

Item Type:	Journal Article
Creators:	Creators Email ORCID ORCID Put Code Engel, Max UNSPECIFIED orcid.org/0000-0002-2271-4229 UNSPECIFIED Dotterweich, Markus UNSPECIFIED UNSPECIFIED UNSPECIFIED Fuelling, Alexander UNSPECIFIED UNSPECIFIED UNSPECIFIED Brill, Dominik UNSPECIFIED UNSPECIFIED UNSPECIFIED Broisch-Hoehner, Manuela UNSPECIFIED UNSPECIFIED UNSPECIFIED Totschnig, Ralf UNSPECIFIED UNSPECIFIED UNSPECIFIED Seren, Sirri UNSPECIFIED UNSPECIFIED UNSPECIFIED Kehl, Martin UNSPECIFIED orcid.org/0000-0003-4587-5858 UNSPECIFIED
URN:	urn:nbn:de:hbz:38-585317
DOI:	10.1002/esp.5119
Journal or Publication Title:	Earth Surf. Process. Landf.
Volume:	46
Number:	9
Page Range:	S. 1783 - 1797
Date:	2021
Publisher:	WILEY
Place of Publication:	HOBOKEN
ISSN:	1096-9837
Language:	English
Faculty:	Unspecified
Divisions:	Unspecified
Subjects:	no entry
Uncontrolled Keywords:	Keywords Language CENTRAL-EUROPE; EROSION; EVOLUTION; GERMANY; SINGLE; DEPOSITS; QUARTZ; SCALE; BASE Multiple languages Geography, Physical; Geosciences, Multidisciplinary Multiple languages
URI:	http://kups.ub.uni-koeln.de/id/eprint/58531