 
 <translate> The Mid-Atlantic Ridge (MAR) is a mid-ocean ridge, a divergent tectonic plate or constructive plate boundary located along the floor of the Atlantic Ocean, and part of the longest mountain range in the world. In the North Atlantic it separates the Eurasian and North American Plates, and in the South Atlantic it separates the African and South American Plates. The ridge extends from a junction with the Gakkel Ridge (Mid-Arctic Ridge) northeast of Greenland southward to the Bouvet Triple Junction in the South Atlantic. Although the Mid-Atlantic Ridge is mostly an underwater feature, portions of it have enough elevation to extend above sea level. The section of the ridge that includes the island of Iceland is also known as the Reykjanes Ridge. The ridge has an average spreading rate of about 2.5 centimetres (0.98 in) per year.

Where does the mid atlantic ridge start and end? OK. Let's think. My stream of consciousness: <hau> Tsakiyar Tsakiyar Tsakiyar Tsakiya (MAR) ita ce tsakiya ta tsakiya, wani tectonic plate mai banbanci ko iyakar ginin da ke kewaye da kasa na Tekun Atlantika, kuma wani ɓangare na tsaunukan tsaunuka mafi tsawo a duniya. A Arewacin Atlantic yana raba Eurasian da Arewacin Amurka Plate, kuma a Kudancin Atlantic ya raba Afirka da Kudancin Amirka Plate. Ridge ya miƙa daga haɗuwa da Gakkel Ridge (Mid-Arctic Ridge) arewa maso gabashin Greenland zuwa kudu zuwa Bouvet Triple Junction a Kudancin Atlantic. Ko da yake Mid-Atlantic Ridge galibi fasalin ruwa ne, sassansa suna da isasshen tsawo don su faɗaɗa sama da matakin teku. Sashe na dutsen da ya hada da tsibirin Iceland kuma ana kiransa Reykjanes Ridge. Girman yana da matsakaicin yaduwar kimanin santimita 2.5 a kowace shekara.  A ina ne tsakiyar Atlantic ridge ya fara kuma ya ƙare? Ya yi kyau. Bari mu yi tunani. Ra'ayina na sani: 