Continental shelves/North west African

There is an apparently small continental shelf along the northwest African coast.

Iberian margins
In the images on the left, sea level during the last glaciation is likely at or above the yellow contour band. This appears to be the sea level delimiter in the second image down on the right.

Moroccan shelves
The first image on the right shows a currently submerged mountain range and associated islands directly in front of the Pillars of Hercules just further west. These may have been above sea level during the previous 50 kyrs ice age.

Mauritanian continental shelves
The "sedimentary processes along the shelf are driven by long-term factors such as Quaternary glacial–interglacial periods and shelf morphology, and by short-term factors such as fluvial and aeolian sediment supply, local climate (temperature, rainfall and wind) and hydrodynamic conditions (tides, swell, longshore current, the Canary Current and upwelling)."

Canary Island seamount province
"The Canary Island Seamount Province forms a scattered hotspot track on the Atlantic ocean floor ~1300 km long and ~350 km wide, perpendicular to lithospheric fractures, and parallel to the NW African continental margin. New 40Ar/39Ar datings show that seamount ages vary from 133 Ma to 0.2 Ma in the central archipelago, and from 142 Ma to 91 Ma in the southwest."

Shallow "mantle upwelling beneath the Atlantic Ocean basin off the NW African continental lithosphere flanks produced recurrent melting anomalies and seamounts from the Late Jurassic to Recent".

Azores microplates
"Archaeologists from the Portuguese Association of Archaeological Research (APIA) have identified [a great variety of protohistoric pyramidal rock structures, some of them 13 meters tall] on Pico island that supports their belief that human occupation of the Azores predates the arrival of the Portuguese by many thousands of years."

The "Madalena pyramidal structures, known by the locals as “maroiços,” are analogous to similar protohistoric structures found in Sicily, North Africa and the Canary islands which are known to have served ritual purposes."

The diagram on the right shows the Azores current as it is deflected by the islands from the Gulf stream about 2014.

The second image down on the right shows the Azores as nine islands that occupy a triple junction between the North American, African and Eurasian Plate, a spreading center bound by the Mid-Atlantic Ridge on the west and the Terceira Rift on the NE and the East Azores Fracture Zone to the SE. From the structure shown, the microplate though thick has undergone extensive fracturing. If at one time it was at or near sea level, it could have blocked a significant portion of the Gulf stream, diverted a major portion toward northwest Africa, or diverted most of the stream north of Scotland into the Norwegian coast. The microplate likely broke apart and subsided in a west to east manner.

The second image on the left is a more geostructurally detailed topographic map of the entire Azores microplate. It clearly shows how the forming of the Mid-Atlantic Ridge underneath has torn the microplate apart along the ridge and approximately perpendicular to it. The orange to brown band is the 1,000 m to sea level band. White is currently above sea level. The yellow band is the 2,000 m to 1,000 m band. It surrounds much of the brown zone and suggests an almost square plateau.

The third image down on the left shows two rows or walls of similarly sized volcanic rock crossing the field of view like those used to make the Pico pyramids.

North Atlantic Ridge
The image on the right shows the topography west of north western Africa out to the Mid-Atlantic Ridge. It clearly shows the impact the ridge had on the Azores microplate, breaking it into parts on either side of the ridge.