Morphological properties of moat-drift systems around the world
type: Dataset
creator: Henriette Wilckens
creator: Tilmann Schwenk
creator: Thomas Lüdmann
creator: Christian Betzler
creator: Wenyan Zhang
creator: Jiayue Chen
  type: Person
  family name: Chen
  given name: Jiayue
creator: Francisco Javier Hernandéz-Molina
  type: Person
  family name: Hernandéz-Molina
  given name: Francisco Javier
creator: Alice Lefebvre
creator: Antonio Cattaneo
creator: Volkhard Spieß
  type: Person
  family name: Spieß
  given name: Volkhard
creator: Elda Miramontes
publisher: PANGAEA
  type: Organization
  disambiguating description: Data Publisher for Earth & Environmental Science
included in data catalog: PANGAEA
  type: DataCatalog
  disambiguating description: Data Publisher for Earth & Environmental Science
date published: 2023-01-31
additional type: dataset
description: To facilitate a comprehensive study of moat-drift systems, we analysed moats from different locations around the world. We measured the following morphological parameters: width, relief, slope angle, drift angle. As there is no moat without an associated drift, we see them as one system that we refer to as a moat-drift system. The moat trough is the deepest point in the moat and the drift crest the shallowest point of the contourite drift. The moat width is defined as the horizontal distance between the drift crest and the slope. The relief is defined as the vertical distance between moat trough and drift crest. The slope angle and the drift angle are the average gradient in both flanks of the moat: 1) between the moat trough and the slope and 2) between the moat trough and the drift crest. The previously published moats were measured from the seismic or sub-bottom profiler cross sections that were published either in a journal or on the GeoMapApp (www.geomapapp.org). In the cases in where multibeam data are available, we measured the parameters from the bathymetric map.
abstract: To facilitate a comprehensive study of moat-drift systems, we analysed moats from different locations around the world. We measured the following morphological parameters: width, relief, slope angle, drift angle. As there is no moat without an associated drift, we see them as one system that we refer to as a moat-drift system. The moat trough is the deepest point in the moat and the drift crest the shallowest point of the contourite drift. The moat width is defined as the horizontal distance between the drift crest and the slope. The relief is defined as the vertical distance between moat trough and drift crest. The slope angle and the drift angle are the average gradient in both flanks of the moat: 1) between the moat trough and the slope and 2) between the moat trough and the drift crest. The previously published moats were measured from the seismic or sub-bottom profiler cross sections that were published either in a journal or on the GeoMapApp (www.geomapapp.org). In the cases in where multibeam data are available, we measured the parameters from the bathymetric map.
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is based on: Periplatform drift: The combined result of contour current and off-bank transport along carbonate platforms
is based on: Significance of bottom currents in deep-sea morphodynamics: An example from the Alboran Sea
is based on: Contourite erosive features caused by the Mediterranean Outflow Water in the Gulf of Cadiz: Quaternary tectonic and oceanographic implications
is based on: Seismic stratigraphy, buried beach ridges and contourite drifts: the Late Quaternary history of the closed Lago Cardiel basin, Argentina (49°S)
is based on: Evolution of the northern Argentine margin during the Cenozoic controlled by bottom current dynamics and gravitational processes
is based on: Contouritic depositional systems influenced by complex seafloor topography : Late Cenozoic seismoacoustic reconstructions from the Galicia and Angola Continental Margins | Media SuUB Bremen
is based on: Good neighbours shaped by vigorous currents: Cold-water coral mounds and contourites in the North Atlantic
is based on: Evolution of the gulf of Cadiz margin and southwest Portugal contourite depositional system: Tectonic, sedimentary and paleoceanographic implications from IODP expedition 339
is based on: Anton Dohrn Seamount and the evolution of the Rockall Trough
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    given name: E J W
  creator: R Siddall
    type: Person
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    given name: R
  creator: Matthew F Thirlwall
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  creator: P N Chroston
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  creator: A J Lloyd
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  date published: 1994
  pagination: 237-247
  is part of: Oceanologica Acta
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is based on: An assessment of bottom current controlled sedimentation in Pacific Ocean abyssal environments
is based on: Sedimentary evolution of the Le Danois contourite drift systems (southern Bay of Biscay, NE Atlantic): A reconstruction of the Atlantic Mediterranean Water circulation since the Pliocene
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is based on: The Maldives, a giant isolated carbonate platform dominated by bottom currents
is based on: Carbonate mounds in the Santaren Channel, Bahamas: A current-dominated periplatform depositional regime
is based on: Analysis and modeling of contourite drifts and contour currents off promontories in the Italian Seas (Mediterranean Sea)
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is based on: Interaction between seabed morphology and water masses around the seamounts on the Motril Marginal Plateau (Alboran Sea, Western Mediterranean)
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is based on: Late Cretaceous to recent ocean-bottom currents in the SW Pacific Gateway, southeastern Chatham Rise, New Zealand
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is based on: Transition from the Cretaceous ocean to Cenozoic circulation in the western South Atlantic — A twofold reconstruction
is based on: Stratigraphy and paleoceanography of a topography-controlled contourite drift in the Pen Duick area, southern Gulf of Cádiz
is based on: Short-distance variability in slope bed-forms along the Southwestern Adriatic Margin (Central Mediterranean)
is based on: The erosive power of the Malvinas Current: Influence of bottom currents on morpho-sedimentary features along the northern Argentine margin (SW Atlantic Ocean)
is based on: The influence of oceanographic processes on contourite features: A multidisciplinary study of the northern South China Sea
is based on: In situ observation of contour currents in the northern South China Sea: Applications for deepwater sediment transport
spatial coverage: Place
  geo: GeoShape
    box: -67.0 -168.0 75.0 172.0
    elevation: 70.0m/5000.0m
size: QuantitativeValue
  value: 1250.0
  unit text: data points
variable measured: Reference/source
variable measured: LATITUDE
variable measured: LONGITUDE
variable measured: Comment
  type: PropertyValue
  description: index
variable measured: ELEVATION
  type: PropertyValue
  unit text: m a.s.l.
  description: moat depth
  subject of: DefinedTermSet
    has defined term: elevation
    has defined term: Length
variable measured: Relief, mean
  type: PropertyValue
  unit text: m
  subject of: DefinedTermSet
    has defined term: mean
    has defined term: Length
variable measured: Width
  type: PropertyValue
  unit text: km
  subject of: DefinedTermSet
    has defined term: width
    has defined term: Length
variable measured: Aspect ratio
  type: PropertyValue
  description: R/W
  subject of: DefinedTermSet
    has defined term: ratio
variable measured: Slope angle
  type: PropertyValue
  unit text: deg
  subject of: DefinedTermSet
    has defined term: Angle
    has defined term: Plane Angle
variable measured: Drift angle
  type: PropertyValue
  unit text: deg
  subject of: DefinedTermSet
    has defined term: Angle
    has defined term: Plane Angle
keywords: contourite; moat; morphology
license: https://creativecommons.org/licenses/by/4.0/
conditions of access: unrestricted
is accessible for free: true
language: en
distribution: DataDownload
  encoding format: text/tab-separated-values
distribution: DataDownload
  encoding format: text/html

Henriette Wilckens
type: Person
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given name: Henriette

Tilmann Schwenk
type: Person
family name: Schwenk
given name: Tilmann

Thomas Lüdmann
type: Person
family name: Lüdmann
given name: Thomas

Christian Betzler
type: Person
family name: Betzler
given name: Christian

Wenyan Zhang
type: Person
family name: Zhang
given name: Wenyan

Alice Lefebvre
type: Person
family name: Lefebvre
given name: Alice

Antonio Cattaneo
type: Person
family name: Cattaneo
given name: Antonio

Elda Miramontes
type: Person
family name: Miramontes
given name: Elda

Salt Diapirs, Salt Brine Seeps, Pockmarks and Surficial Sediment Creep and Slides in the Canary Channel off NW Africa
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creator: Manuel Ballesteros
creator: ZEE Working Group
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pagination: 41-57
is part of: Marine Geophysical Research
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  volume number: 24(1-2)

Manuel Ballesteros
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Periplatform drift: The combined result of contour current and off-bank transport along carbonate platforms
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John J G Reijmer
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Christian Hübscher
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Significance of bottom currents in deep-sea morphodynamics: An example from the Alboran Sea
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Marga M García
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Elia d'Acremont
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Javier Valencia
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Bouchta El Moumni
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Ricardo León
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M C Fernández-Puga
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Luis Somoza
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Flavio S Anselmetti
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Daniel Ariztegui
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Evolution of the northern Argentine margin during the Cenozoic controlled by bottom current dynamics and gravitational processes
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Dieter Franke
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Contouritic depositional systems influenced by complex seafloor topography : Late Cenozoic seismoacoustic reconstructions from the Galicia and Angola Continental Margins | Media SuUB Bremen
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source organization: University of Bremen, Germany
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Good neighbours shaped by vigorous currents: Cold-water coral mounds and contourites in the North Atlantic
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David Van Rooij
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Claudia Wienberg
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Evolution of the gulf of Cadiz margin and southwest Portugal contourite depositional system: Tectonic, sedimentary and paleoceanographic implications from IODP expedition 339
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Francisco Javier Sierro
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C Roque
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Thomas Williams
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Johanna Lofi
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Santiago Ledesma
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Francisco Javier Rodríguez-Tovar
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Eulogio Pardo-Igúzquiza
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Rachel E Brackenridge
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An assessment of bottom current controlled sedimentation in Pacific Ocean abyssal environments
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Sedimentary evolution of the Le Danois contourite drift systems (southern Bay of Biscay, NE Atlantic): A reconstruction of the Atlantic Mediterranean Water circulation since the Pliocene
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creator: David Van Rooij
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Shan Liu
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Contourites along the Iberian continental margins: conceptual and economic implications
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Anxo Mena
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Michele Rebesco
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María Gómez-Ballesteros
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The Maldives, a giant isolated carbonate platform dominated by bottom currents
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Carbonate mounds in the Santaren Channel, Bahamas: A current-dominated periplatform depositional regime
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creator: Gregor P Eberli
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pagination: 69-85
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Analysis and modeling of contourite drifts and contour currents off promontories in the Italian Seas (Mediterranean Sea)
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E Martorelli
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F Falcini
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Francesco L Chiocci
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Bottom-current sediment waves, sediment drifts and contourites in the northern Rockall Trough
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Martyn S Stoker
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Outer shelf seafloor geomorphology along a carbonate escarpment: The eastern Malta Plateau, Mediterranean Sea
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Aggeliki Georgiopoulou
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Veerle A I Huvenne
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Claudio Lo Iacono
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Paola Del Carlo
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The Pianosa Contourite Depositional System (Northern Tyrrhenian Sea): Drift morphology and Plio-Quaternary stratigraphic evolution
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Contourite and mixed turbidite-contourite systems in the Mozambique Channel (SW Indian Ocean): Link between geometry, sediment characteristics and modelled bottom currents
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Gravity Processes and Deposits on Continental Slope, Rise and Abyssal Plains
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Sequence stratigraphic framework of a mixed turbidite-contourite depositional system along the NW slope of the South China Sea
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Interaction between seabed morphology and water masses around the seamounts on the Motril Marginal Plateau (Alboran Sea, Western Mediterranean)
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Evolution of a high-latitude sediment drift inside a glacially-carved trough based on high-resolution seismic stratigraphy (Kveithola, NW Barents Sea)
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Sediment distribution around moated seamounts in the Rockall Trough
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Muddy contourites in the Baltic Sea: an example of a shallow-water contourite system
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Late Cretaceous to recent ocean-bottom currents in the SW Pacific Gateway, southeastern Chatham Rise, New Zealand
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Late quaternary bottom-current activity in the south Aegean Sea reflecting climate-driven dense-water production
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Transition from the Cretaceous ocean to Cenozoic circulation in the western South Atlantic — A twofold reconstruction
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Stratigraphy and paleoceanography of a topography-controlled contourite drift in the Pen Duick area, southern Gulf of Cádiz
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Short-distance variability in slope bed-forms along the Southwestern Adriatic Margin (Central Mediterranean)
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The erosive power of the Malvinas Current: Influence of bottom currents on morpho-sedimentary features along the northern Argentine margin (SW Atlantic Ocean)
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The influence of oceanographic processes on contourite features: A multidisciplinary study of the northern South China Sea
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In situ observation of contour currents in the northern South China Sea: Applications for deepwater sediment transport
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Factors controlling the morphology and internal sediment architecture of moats and their associated contourite drifts
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is based on: Morphological properties of moat-drift systems around the world