Weathering under coastal hyperaridity – Assessing spectral, textural, and gravelometric alluvial fan surface characteristics using high resolution remote sensing

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Title:Main Title: Weathering under coastal hyperaridity – Assessing spectral, textural, and gravelometric alluvial fan surface characteristics using high resolution remote sensing
Description:Abstract: Physical and chemical weathering processes along hyperarid coasts differ distinctly from those present in inland deserts due to the abundance of air humidity and sea salt aerosols. However, the geomorphic effects of the weathering processes as well as the timescales on which alteration of the depositional surfaces occur are only poorly understood. Based on high to very high resolution satellite (2 m) and aerial (~1–5 cm) remote sensing, we integrate in a novel approach spectral, textural, and gravelometric analyses of a multi-stage alluvial fan at the coast of the Atacama Desert. As long as weathering of fan surface sediments prior to deposition can be largely excluded, the surface parameters investigated serve to relatively date a succession of fan generations. Derived from the differential states of post-depositional alteration, complemented by a morphochronology of the fan system’s evolution based on cosmogenic Beryllium-10 exposure dating, the intensities of responsible weathering processes are discussed. Our results indicate that under coastal hyperaridity, spectral surface signatures are primarily governed by secondary iron oxidation which is closely related to weathering rind formation. Spectral iron oxide ratios continuously increase with age after pre-Holocene fan surface abandonment. Clast breakdown is characterized by a steady decrease of clast coarseness and size variation, both caused by salt weathering. Driven by breakdown as well as lateral remobilization of clasts, nano-scale surface roughness exhibits a non-monotonic relationship with age, whereas the micro-relief experiences continuous smoothing due to denudation. Summarized in a conceptual model, fan surface weathering results over timescales of tens to hundreds of thousands of years in a mature desert pavement. For the hyperarid coast of the Atacama Desert, it can be further deduced that weathering intensity during the Late Quaternary is related to changes in sea surface temperature and sea level driving jointly the oceanic moisture supply.
Responsible Party
Creators:Janek Walk (Author), Melanie Bartz (Author), Georg Stauch (Author), Ariane Binnie (Author), Helmut Brückner (Author), Frank Lehmkuhl (Author)
Funding Reference:Deutsche Forschungsgemeinschaft (DFG): CRC 1211: Earth - Evolution at the Dry Limit
Publisher:CRC1211 Database (CRC1211DB)
Publication Year:2021
Topic
CRC1211 Topic:Surface
Related Subproject:C2
Subjects:Keywords: Geomorphology, Satellite remote sensing, Ground-based remote sensing, Geochronology, Cosmogenic Nuclides, Arid Zone
Geogr. Information Topic:Environment
File Details
Filename:Walk_2021_MGM_Weathering_under_coastal_hyperaridity_16-9_oral.pdf
Data Type:Text - Text
Size:13 Pages
File Size:5.1 MB
Date:Created: 05.11.2021
Mime Type:application/pdf
Data Format:PDF
Language:English
Status:Completed
Constraints
Download Permission:Only Project Members
General Access and Use Conditions:According to the CRC1211DB data policy agreement. © Author(s) 2021.
Access Limitations:According to the CRC1211DB data policy agreement. © Author(s) 2021.
Licence:[CRC1211DB] Data policy agreement
Geographic
Specific Information - Presentation
Presenter:Janek Walk
Presentation Date:7th of November, 2021
Presentation Type:Talk
Event:Mid-European Geomorphology Meeting (MGM) 2021
Event Type:Conference
Event Location:München
Event Duration:6th of November, 2021 - 9th of November, 2021
Event Website:https://www.ak-geomorphologie.de/tagungen/mgm-2021/
Metadata Details
Metadata Creator:Janek Walk
Metadata Created:18.11.2021
Metadata Last Updated:18.11.2021
Subproject:C2
Funding Phase:2
Metadata Language:English
Metadata Version:V50
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