Submarine mass movements along a sediment starved margin: the Menorca Channel (Balearic Islands - Western Mediterranean)

Mauro Agate, Sabrina Polizzi, Claudio Lo Iacono, Druet, Grinyó, Claudio Lo Iacono, Gili, Roger Urgeles, Acosta

Risultato della ricerca: Chapter

1 Citazione (Scopus)

Abstract

Sediment starved passive margins, particularly those of insular slopes,display significant mass transport activity despite the absence ofenvironmental stresses from high sedimentation rates. The “MenorcaChannel” represents the up to 120 m deep shelf sector connectingthe Menorca and Mallorca Islands (Balearic Islands – WesternMediterranean). South of the Menorca Channel submarine gravitationalprocesses have been mapped and interpreted from swath-bathymetry,TOPAS parametric echosounder and deep-towed videos. The shelf-breakis located at an average depth of 140 m, and sediment instability is awidespread phenomenon. The slope region south the Menorca Channelshows a number of submarine canyons disrupting the outer shelf. Thenorth-easternmost canyon is the more active feature, with an incisedaxis and scars shaping the flanks up to their edges. Headwall scarps,between 140 and 700 m depth, are up to 20 m high. The shallowerscarps producing slab-type failures have carved the outer edges ofplanar sedimentary bodies interpreted as formed in shallow environmentsduring previous glacial stages. Results show that a variety of sedimentinstability processes extensively shape the southern upper slope of theMenorca Channel. Submarine canyons develop on the Emile BodoutEscarpment (EBE), a passive tectonic feature which bounds the sloperegion of the study area. A number of knickpoints within the canyonssuggest backward erosion control on mass wasting and, at the sametime, that slope failure is one of the main drivers for canyon upslopemigration. Steep gradients of the upper slope, the presence of weak layersand the action of major storms during lowstand stages are additionalfactors likely to influence the distribution and frequency of mass wastingprocesses in this area.
Lingua originaleEnglish
Titolo della pubblicazione ospiteSubmarine Mass Movements and Their Consequences
Pagine329-338
Numero di pagine10
Stato di pubblicazionePublished - 2014

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mass movement
Sediments
submarine canyon
sediment
canyon
erosion
Bathymetry
video
driver
Tectonics
submarine channel
swath bathymetry
Sedimentation
mass wasting
tectonic feature
Erosion
lowstand
erosion control
slope failure
passive margin

All Science Journal Classification (ASJC) codes

  • Global and Planetary Change
  • Geography, Planning and Development
  • Economic Geology
  • Computers in Earth Sciences
  • Management, Monitoring, Policy and Law

Cita questo

Agate, M., Polizzi, S., Iacono, C. L., Druet, Grinyó, Iacono, C. L., ... Acosta (2014). Submarine mass movements along a sediment starved margin: the Menorca Channel (Balearic Islands - Western Mediterranean). In Submarine Mass Movements and Their Consequences (pagg. 329-338)

Submarine mass movements along a sediment starved margin: the Menorca Channel (Balearic Islands - Western Mediterranean). / Agate, Mauro; Polizzi, Sabrina; Iacono, Claudio Lo; Druet; Grinyó; Iacono, Claudio Lo; Gili; Urgeles, Roger; Acosta.

Submarine Mass Movements and Their Consequences. 2014. pag. 329-338.

Risultato della ricerca: Chapter

Agate, M, Polizzi, S, Iacono, CL, Druet, Grinyó, Iacono, CL, Gili, Urgeles, R & Acosta 2014, Submarine mass movements along a sediment starved margin: the Menorca Channel (Balearic Islands - Western Mediterranean). in Submarine Mass Movements and Their Consequences. pagg. 329-338.
Agate M, Polizzi S, Iacono CL, Druet, Grinyó, Iacono CL e altri. Submarine mass movements along a sediment starved margin: the Menorca Channel (Balearic Islands - Western Mediterranean). In Submarine Mass Movements and Their Consequences. 2014. pag. 329-338
Agate, Mauro ; Polizzi, Sabrina ; Iacono, Claudio Lo ; Druet ; Grinyó ; Iacono, Claudio Lo ; Gili ; Urgeles, Roger ; Acosta. / Submarine mass movements along a sediment starved margin: the Menorca Channel (Balearic Islands - Western Mediterranean). Submarine Mass Movements and Their Consequences. 2014. pagg. 329-338
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AU - Polizzi, Sabrina

AU - Iacono, Claudio Lo

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AU - Urgeles, Roger

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N2 - Sediment starved passive margins, particularly those of insular slopes,display significant mass transport activity despite the absence ofenvironmental stresses from high sedimentation rates. The “MenorcaChannel” represents the up to 120 m deep shelf sector connectingthe Menorca and Mallorca Islands (Balearic Islands – WesternMediterranean). South of the Menorca Channel submarine gravitationalprocesses have been mapped and interpreted from swath-bathymetry,TOPAS parametric echosounder and deep-towed videos. The shelf-breakis located at an average depth of 140 m, and sediment instability is awidespread phenomenon. The slope region south the Menorca Channelshows a number of submarine canyons disrupting the outer shelf. Thenorth-easternmost canyon is the more active feature, with an incisedaxis and scars shaping the flanks up to their edges. Headwall scarps,between 140 and 700 m depth, are up to 20 m high. The shallowerscarps producing slab-type failures have carved the outer edges ofplanar sedimentary bodies interpreted as formed in shallow environmentsduring previous glacial stages. Results show that a variety of sedimentinstability processes extensively shape the southern upper slope of theMenorca Channel. Submarine canyons develop on the Emile BodoutEscarpment (EBE), a passive tectonic feature which bounds the sloperegion of the study area. A number of knickpoints within the canyonssuggest backward erosion control on mass wasting and, at the sametime, that slope failure is one of the main drivers for canyon upslopemigration. Steep gradients of the upper slope, the presence of weak layersand the action of major storms during lowstand stages are additionalfactors likely to influence the distribution and frequency of mass wastingprocesses in this area.

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