Madeira Abyssal Plain, also called Madeira Plain, is an abyssal plain situated at the center and deepest part of the Canary Basin. It is a north-northeast to south-southeast elongated basin that almost parallels the Mid-Atlantic Ridge. Its western boundary is marked by a chain of seamounts known as the either Seewarte Seamounts or Atlantis-Great Meteor Seamount Chain. Its eastern boundary is a distinct break of slope that marks the foot of the African Continental Rise. This abyssal plain occupies an area of about . Across this basin, slope angles are generally less than 0.01°.
Physiographic setting
For research purposes, the Madeira Abyssal Plain can be divided into three sub-basins. They are a southern sub-basin, which lies at a water depth of about , a central sub-basin which lies at a deeper water depth of about , and the northern sub-basin which lies at an intermediate water depth of about . The central sub-basin, which is also known as Great Meteor East after a seamount situated to the west, occupies a broad area of and is bounded by about the -contour.
The central sub-basin of the Madeira Abyssal Plain is relatively flat plain that is occasionally interrupted by small abyssal hills of a few hundred meters in height and draped by pelagic and hemipelagic sediments. These abyssal hills become more numerous to the north, south and west where they form the boundaries of the central sub-basin.
History of Research
In 1980, the Nuclear Energy Agency's Seabed Working Group selected the Madeira Abyssal Plain as a site for the possible disposal of heat-emitting radioactive waste. Even though this concept was later abandoned, it resulted in this region being the location for intensive studies of its bathymetry, geology, oceanography, and biota. Since the 1980s, the Madeira Abyssal Plain has been studied in detail by the Ocean Drilling Program and research concerning the Moroccan Turbidite System.
Geology
An average of of exclusively deep-sea sediments, resting upon oceanic crust, underlies the Madeira Abyssal Plain. Seismic reflection profiles across the Canary Basin and Madeira Abyssal Plain reveal north-northeast – south-southwest ridge and trough terrain typical of oceanic crust and west-northwest – east-southeast striking fracture zone valleys that are spaced about part. Because most of the Madeira Abyssal Plain lies within the Cretaceous Superchron, the oceanic crust underlying it cannot be precisely dated by magnetic striping. However, interpolation between recognised magnetic stripes estimated an age range of about 75 to 105 Ma for the oceanic crust underlying the central sub-basin.
Immediately overlying the oceanic crust is a layer of hemipelagic sediments. These sediments average in thickness and are expected to consist predominantly of hemipelagic clay.
Overlying the hemipelagic sediments, are alternating turbidites and thin beds of pelagic sediment. These sediments initially in filled irregularities on the uneven surface of the hemipelagic sediments to produce a flat plain that later turbidites accumulated. The total thickness of turbidites that have accumulated averages in thickness. In a few deep troughs within the oceanic crust, the total thickness of turbidites may reach . In seismic reflection, the sequence of turbidites varies from being strongly acoustically laminated near the top to poorly stratified to transparent near the base. An individual turbidite often consists of of sediment spread across the entire Madeira Abyssal Plain. It is typically fine-grained, except in the proximal parts of the plain. The deposition of a typical turbidite causes little or no erosion of the underlying bed. A thin bed of fine-grained, pelagic sediment typically separates successive turbidites.