TheInfoListRev V5.1.84
Xfr/
SummaryRelatedTreeNews

Related topics

Aden Ridge

Sponsored
Shop Amazon for battery chargers
Browse products on Amazon.
Search Amazon →
As an Amazon Associate I earn from qualifying purchases.

The Aden Ridge is a part of an active oblique rift system located in the Gulf of Aden, between Somalia and the Arabian Peninsula to the north. The rift system marks the divergent boundary between the Somali and Arabiantectonic plates, extending from the Owen transform fault in the Arabian Sea to the Afar triple junction or Afar Plume beneath the Gulf of Tadjoura in Djibouti.

Afar triple junctionAfar triple junctionThe Afar triple junction is a triple junction located along a divergent plate boundary dividing the Nubian, Somali, and Arabian plates. This area is considered a present-day example of continental rifting leading to seafloor spreading and producing an oceanic basin. Here, the Red Sea Rift meets the Aden Ridge and the East African Rift. The latter extends a total of 6,500 kilometers (4,000 mi) from the Afar Triangle to Mozambique.Owen fracture zoneOwen fracture zoneThe Owen fracture zone (OFZ), though misnamed as a fracture zone, is a transform fault in the northwest Indian Ocean that separates the Arabian and African plates from the Indian plate. Extending north-northeast from where the Carlsberg Ridge meets the Sheba ridge in the south to the Makran Subduction Zone in the north, it represents the port side of the northward motion of the Indian subcontinent during the Late Cretaceous–Palaeogene break-up of Gondwana.Somali plateSomali plateThe Somali plate is a minor tectonic plate which straddles the Equator in the Eastern Hemisphere. It is currently in the process of separating from the African plate along the East African Rift Valley and moving to the Indian subcontinent. It is approximately centered on the island of Madagascar and includes about half of the east coast of Africa, from the Gulf of Aden in the north through the East African Rift Valley.Arabian plateArabian plateThe Arabian plate, also known as Circum-Arabian tectonic plate is a minor tectonic plate in the Northern and Eastern Hemispheres. It is one of the three continental plates (along with the African and Indian plates) that have been moving northward in geological history and colliding with the Eurasian plate.Arabian PeninsulaArabian PeninsulaThe Arabian Peninsula, or simply Arabia, is a peninsula in West Asia. It accounts for the majority of the land situated on the Arabian plate. With an area of 3,237,500 km2 (1.25 million mi2), it is the world's largest peninsula—roughly comparable in size to India. Nine countries are located on the Arabian Peninsula: Bahrain, Kuwait, Oman, Qatar, Saudi Arabia, the United Arab Emirates, and Yemen, as well as the southern halves of Iraq and Jordan.Gulf of AdenGulf of AdenThe Gulf of Aden (Arabic: خليج عدن; Somali: Gacanka Cadmeed) is a deepwater gulf of the Indian Ocean between Yemen to the north, the Arabian Sea to the east, Djibouti to the west, and the Guardafui Channel, the Socotra Archipelago, Puntland in Somalia and Somaliland to the south. In the northwest, it connects with the Red Sea through the Bab-el-Mandeb strait, and it connects with the Arabian Sea to the east.Arabian SeaArabian SeaMax. width2,400 km (1,500 mi)Surface area3,862,000 km (1,491,000 sq mi) (3,600,000–4,600,000 km in various sources)Max.RiftRiftIn geology, a rift is a linear zone where the lithosphere is being pulled apart and is an example of extensional tectonics. Typical rift features are a central linear downfaulted depression, called a graben, or more commonly a half-graben with normal faulting and rift-flank uplifts mainly on one side. Where rifts remain above sea level they form a rift valley, which may be filled by water forming a rift lake.Divergent boundaryDivergent boundaryIn plate tectonics, a divergent boundary or divergent plate boundary (also known as a constructive boundary or an extensional boundary) is a linear feature that exists between two tectonic plates that are moving away from each other. Divergent boundaries within continents initially produce rifts, which eventually become rift valleys. Most active divergent plate boundaries occur between oceanic plates and exist as mid-oceanic ridges.Plate tectonicsPlate tectonicsPlate tectonics (from Latin, from Ancient Greek (tektonikós)'pertaining to building') is the scientific theory that Earth's lithosphere comprises a number of large tectonic plates, which have been slowly moving since 3–4 billion years ago. The model builds on the concept of continental drift, an idea developed during the first decades of the 20th century.SomaliaSomaliaCountry in East Africa This article has multiple issues. Please help improve it or discuss these issues on the talk page. (Learn how and when to remove these messages) This article may require copy editing for style and cutting down content. You can assist by editing it. (August 2026) (Learn how and when to remove this message) This article's lead section may be too long. Please read the length guidelines and help move details into the article's body.

*As an Amazon Associate I earn from qualifying purchases.

AboutPrivacyContact

TheInfoList organizes topic information and links to original sources.

Loading topic…