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dc.contributor.authorMather, AEen
dc.contributor.authorStokes, Men
dc.contributor.editorVentra, Den
dc.contributor.editorClarke, LEen
dc.date.accessioned2017-10-09T08:22:44Z
dc.date.available2017-10-09T08:22:44Z
dc.date.issued2017en
dc.identifier.urihttp://hdl.handle.net/10026.1/10030
dc.description.abstract

Lithology is acknowledged to be an important internal catchment control on flow processes to adjacent alluvial fans. However, the role of inherited structural configurations (e.g.bedrock attitude) in catchment connectivity and sediment transport is rarely considered. We examine four young (,100-year-old) active tributary junction alluvial fan systems from the Dade`s Valley in the High Atlas of Morocco in terms of their catchment-scale connectivity, sediment transfer and resulting alluvial fan processes. The catchments occur on the same lithologies (limestones and interbedded mudstones), but experience different passive structural configurations (tilted and structurally thickened beds). The fan systems react differently to historical peak discharges (20–172 m3 s21). Catchments containing tectonically thickened limestone units develop slot canyons, which compartmentalize the catchment by acting as barriers to sediment transfer, encouraging lower sediment to water flows on the fans. Syn-dip catchments boost connectivity and sediment delivery from translational bedrock landslides as a result of steep channel gradients, encouraging higher sediment to water flows. By contrast, translational landslides in strike-oriented drainages disrupt longitudinal connectivity by constricting the valley width, while the gradients of the main channels are supressed by the attitude of the limestone beds, encouraging localised backfilling. This diminishes the sediment to water content of the resulting flows.

en
dc.language.isoenen
dc.publisherThe Geological Society of Londonen
dc.relation.ispartofGeology and Geomorphology of Alluvial and Fluvial Fans: Terrestrial and Planetary Perspectivesen
dc.titleBedrock structural control on catchment scale connectivity and alluvial fan processes, High Atlas Mountains, Morocco.en
dc.typeBook Chapter
plymouth.volume440en
plymouth.publication-statusAccepteden
plymouth.seriesGeological Society, London, Special Publicationsen
dc.identifier.doi10.1144/SP440.15en
plymouth.organisational-group/Plymouth
plymouth.organisational-group/Plymouth/00 Groups by role
plymouth.organisational-group/Plymouth/00 Groups by role/Academics
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering/School of Geography, Earth and Environmental Sciences
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA/UoA07 Earth Systems and Environmental Sciences
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA/UoA14 Geography and Environmental Studies
plymouth.organisational-group/Plymouth/Research Groups
plymouth.organisational-group/Plymouth/Research Groups/Centre for Research in Environment and Society (CeRES)
plymouth.organisational-group/Plymouth/Research Groups/Marine Institute
dc.rights.embargoperiodNot knownen
rioxxterms.versionofrecord10.1144/SP440.15en
rioxxterms.licenseref.urihttp://www.rioxx.net/licenses/all-rights-reserveden
rioxxterms.typeBook chapteren


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