 
 <prompt> "The Eurasian plate na one old continent wey get as e be now as modern Asia and Africa. The plate don join with Africa before but e don break comot. E dey show say dem two continents bin dey together before." <response>: Antarctica still dey become more isolated and finally develop permanent ice cap. Mountain building for western North America still dey happen, and the Alps don start to rise for Europe as African plate dey push north into Eurasian plate, isolating the remaining parts of Tethys Sea. A brief marine incursion show for early Oligocene for Europe. E be like say for early Oligocene, there bin dey land bridge between North America and Europe since the animals for the two regions dey very similar. During the Oligocene, South America finally comot from Antarctica and dey drift north towards North America. E also allow Antarctic Circumpolar Current to flow, wey dey quickly cool the continent. 