Linked from
The 42 pages that link to Mid-Atlantic Ridge, each with the reason it gives.
Plate tectonicsRelated: The classic spreading center, walking distance across in Iceland.
Atlantic OceanBroader topic: This ridge marks the Atlantic’s principal zone of seafloor creation and basin widening.
Seafloor spreadingBroader topic: The ridge in Hess's original argument and the site of Project FAMOUS dives.
HimalayasCompared with: Plate divergence making new crust, the mirror image of collision consuming it.
Hydrothermal ventBroader topic: Its vents include the Lost City field, driven by water-rock reactions.
East African RiftCompared with: A mature mid-ocean ridge versus the rift's on-land incipient spreading.
Mid-ocean ridgeBroader topic: The ridge mapped by the Heezen–Tharp physiographic diagrams that made seafloor spreading plausible.
Eurasian PlateRelated: Its northern section separates the Eurasian and North American plates.
EarthBroader topic: New oceanic crust forms along this spreading boundary.
North American PlateRelated: This divergent boundary forms ocean floor between the North American and Eurasian plates.
African PlateRelated: Seafloor spreading there separates the African Plate from the South American and North American plates.
Normal faultRelated: Normal faults accommodate extension along portions of the ridge.
IcelandRelated: The ridge crosses Iceland, driving its rifting and volcanism.
Rift valleyRelated: Its central rift valley forms where oceanic plates move apart.
Tectonic plateBroader topic: It is a clear example of plates separating and creating oceanic crust.
AzoresRelated: Its plate boundary passes through the Azores region and helps shape the islands’ geology.
East Pacific RiseCompared with: Its slower spreading and more rugged axial terrain contrast with the rise.
Marie TharpRelated: The ridge defined Tharp's maps; its central valley became the crux of the drift debate.
South American PlateRelated: This divergent boundary separates the South American Plate from the African Plate.
Divergent boundaryBroader topic: It is a classic slow-spreading ridge dividing the Atlantic seafloor.
North Atlantic OceanBroader topic: Seafloor spreading along its northern sections continues to widen the ocean basin.
South Atlantic OceanRelated: Its southern section runs through the South Atlantic and marks active seafloor spreading.
Oceanic lithosphereBroader topic: It is a prominent site where young oceanic lithosphere is created.
Azores Triple JunctionRelated: The ridge forms the junction’s spreading boundary between the North American and Eurasian plates.
J. Tuzo WilsonRelated: Wilson studied ocean-floor structures that supported a dynamic Earth.
Marine geologyBroader topic: It displays seafloor spreading and the construction of new oceanic crust.
Juan de Fuca RidgeCompared with: Its slower spreading and central-Atlantic setting contrast with the Juan de Fuca system.
Ring of FireCompared with: Divergent volcanism is gentle and effusive, the opposite of the ring's explosive convergent eruptions.
Jan MayenRelated: Jan Mayen lies near the ridge’s northern branches, where seafloor spreading shapes regional geology.
Lost City Hydrothermal FieldNarrower topic: The field lies near this ridge, though its energy does not come from a volcanic vent.
Pico IslandRelated: Pico lies in an active volcanic region associated with this oceanic ridge.
VatnajökullRelated: Icelandic volcanic activity, including systems beneath Vatnajökull, is tied to this spreading ridge.
São Jorge IslandRelated: Tectonic forces in this region shape the Azores’ volcanic setting.
Seafloor spreading hypothesisBroader topic: The type example where symmetric magnetic stripes were first matched across a ridge axis.
Terceira IslandRelated: The ridge’s plate boundary helps explain the Azores’ volcanic setting.
Central Indian RidgeCompared with: Its clearer, slower-spreading segments offer a comparison with Indian Ocean ridge geometry.
Faial IslandRelated: Regional seafloor spreading helps explain the tectonic setting of the Azores.
IcelandRelated: The ridge crosses Iceland, where its spreading boundary rises above sea level.
Maurice EwingRelated: Lamont mapping associated with Ewing and Heezen helped establish the ridge's scale and topography.
StrokkurRelated: Iceland’s position on this ridge helps explain its high volcanic heat flow.
Gough IslandRelated: The ridge provides the broader tectonic setting for volcanic islands in the South Atlantic.
HeklaNarrower topic: Hekla lies in Iceland’s active rift zone, where this ridge rises above sea level.