isthmus of Vieussens - ترجمة إلى العربية
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isthmus of Vieussens - ترجمة إلى العربية

NARROW LANDSTRIP IN PANAMA
Isthmus of Darien; Isthmus of Darién; Panama isthmus; Panamanian isthmus; Isthmas of Panama; Isthmus of panama; Panama Isthmus; Isthmus of darien; Isthmus of Panamá; Panamanian Isthmus; The Isthmus of Panama; Ithmus of Panama; Isthimus of Darien
  • The closure of the Isthmus led to [[allopatric speciation]] events of marine organisms isolated on each side (blue and green). Terrestrial species also migrated between the two continents (the [[Great American Biotic Interchange]]) upon the formation of a passable land bridge.

isthmus of Vieussens      
‎ بَرْزَخُ فيوسانس,حُوفُ الحُفْرَةِ البَيضَوِيَّة‎
isthmus of Vieussens      
بَرْزَخُ فيوسانس
oropharyngeal isthmus         
PART OF THE OROPHARYNX DIRECTLY BEHIND THE MOUTH CAVITY, BOUNDED SUPERIORLY BY THE SOFT PALATE, LATERALLY BY THE PALATOGLOSSAL ARCHES, AND INFERIORLY BY THE TONGUE
Fauces (anatomy); Pillars of the fauces; Faucial pillars; Palatine arches; Isthmus faucium; Oropharyngeal isthmus; Faucitis; Faucial isthmus; Pillar of fauces; Isthmus of fauces; Pillars of fauces; Pillar of the fauces; Palatine arch; Isthmus of the fauces
البَرْزَخُ الفَمَوِيُّ البُلْعومِيّ

تعريف

isthmus
(isthmuses)
An isthmus is a narrow piece of land connecting two very large areas of land.
...the Isthmus of Panama.
N-COUNT: oft in names

ويكيبيديا

Isthmus of Panama

The Isthmus of Panama (Spanish: Istmo de Panamá), also historically known as the Isthmus of Darien (Istmo de Darién), is the narrow strip of land that lies between the Caribbean Sea and the Pacific Ocean, linking North and South America. It contains the country of Panama and the Panama Canal. Like many isthmuses, it is a location of great geopolitical and strategic importance.

The isthmus is thought to have been finally formed around 3 million years ago, separating the Atlantic and Pacific Oceans and causing the creation of the Gulf Stream. This was first suggested in 1910 by North American paleontologist Henry Fairfield Osborn. He based the proposal on the fossil record of mammals in Central America. This conclusion provided a foundation for Alfred Wegener when he proposed the theory of continental drift in 1912.