File:Antes de la formación del istmo de Panamá.png
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English: Before the formation of the Isthmus of Panama there was only one tropical ocean, this Central American seaway, was a body of water that communicated the Atlantic Ocean with the Pacific Ocean, which once separated North America from South America. There is also a weak marine current that came from the Atlantic Ocean, from east to west flowing through the Caribbean and the north coast of South America entering the Gulf of Mexico, and part of that current entering the Pacific Ocean. The formation of the isthmus found significant changes in ocean currents, including the creation of the Gulf Stream, which led to warmer temperatures in northern Europe and the formation of a large ice sheet across North America.
Español: Antes de la formación del istmo de Panamá existía un solo océano tropical, esta vía marina centroamericana, era un cuerpo de agua que comunicaba el océano Atlántico con el océano Pacífico, que una vez separó Norteamérica de Suramérica. Tambien existía una débil corriente marina que venia del océano Atlántico, del este al oeste fluyendo por el caribe y la costa norte de Suramérica entrando al golfo de México, y parte de esa corriente entraba al océano pacífico. La formación del istmo produjo importantes cambios en las corrientes oceánicas, incluyendo la creación de la Corriente del Golfo, que dio lugar a temperaturas más cálidas en el norte de Europa y la formación de una gran placa de hielo a través de América del Norte. |
| Date | |
| Source | Own work |
| Author | Chiche Ojeda |
| Camera location |  | View this and other nearby images on: OpenStreetMap |  |
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| current | 12:32, 18 April 2020 | | 1,054 × 708 (106 KB) | Chiche Ojeda (talk | contribs) | {{Information |description ={{en|1= Before the formation of the Isthmus of Panama there was only one tropical ocean, this Central American seaway, was a body of water that communicated the Atlantic Ocean with the Pacific Ocean, which once separated North America from South America. There is also a weak marine current that came from the Atlantic Ocean, from east to west flowing through the Caribbean and the north coast of South America entering the Gulf of Mexico, and part of that current en... |
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