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Relieve submarino

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Relieve submarino

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La plataforma continental es la prolongación sumergida del territorio de un estado costero, caracterizada por ser una zona submarina poco profunda (generalmente menos de 200 metros) que se extiende desde la costa hasta un cambio abrupto de pendiente conocido como talud continental. Es crucial por albergar recursos naturales como petróleo, minerales y una gran biodiversidad, extendiéndose legalmente hasta 200 millas náuticas o el borde del margen continental

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KAROL STEFANNY MENDOZA MACHADO
KAROL STEFANNY MENDOZA MACHADO
Colombia

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La plataforma continental es la prolongación sumergida del territorio de un estado costero, caracterizada por ser una zona submarina poco profunda (generalmente menos de 200 metros) que se extiende desde la costa hasta un cambio abrupto de pendiente conocido como talud continental. Es crucial por albergar recursos naturales como petróleo, minerales y una gran biodiversidad, extendiéndose legalmente hasta 200 millas náuticas o el borde del margen continental

by KAROL STEFANNY MENDOZA MACHADO
1 Plataforma continental 2 Volcanes marinos 3 Dorsales oceánicas 4 Fosas marinas 5 Llanura abisal

Explicación

Es la superficie del fondo marino próximo a la costa con una distancia inferior a 200 metros.

Es un fenómeno en fondo oceánico en forma de cono, el cual expulsa material hacia el exterior. A eso lo denominamos eupción, se encuentran entre 2600 m a 3000 m en las profundidades marinas.

Son elevaciones submarinas y fisuras en las profundidades del oceáno con alturas de 2000 a 3000 metros.

Son largas y estrechas en el fondo marino, en forma de trinchera, algunas hasta los 11.034 metros.

La llanura abisal es una extensión de terreno llano o plano entre los 3.000 y 7.000 metros en las profundidades marinas.

 
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