Lightboxes
Carrito
alb8348825

Earths outermost layer is broken into about 13 principal plates, each of them carrying a continent, a part of an ocean, or both. These plates float on the magma in Earths mantle. This phenomenon is the central idea behind a theory called plate tectonics. According to the theory, several of the features on the planets surface can be explained by the movement of the plates. For instance, mountain ranges form where two plates collide, and faults form when two plates move apart or slide against each other. Plate tectonics also helps to explain the theory of continental drift, proposed by German scientist Alfred Wegener in 1912.

Earths outermost layer is broken into about 13 principal plates, each of them carrying a continent, a part of an ocean, or both. These plates float on the magma in Earths mantle. This phenomenon is the central idea behind a theory called plate tectonics. According to the theory, several of the features on the planets surface can be explained by the movement of the plates. For instance, mountain ranges form where two plates collide, and faults form when two plates move apart or slide against each other. Plate tectonics also helps to explain the theory of continental drift, proposed by German scientist Alfred Wegener in 1912.
Compartir
pinterestPinterest
twitterTwitter
facebookFacebook
emailEmail

Añadir a otro lightbox

Añadir a otro lightbox
add to lightbox print share
¿Ya tienes cuenta? Iniciar sesión
¿No tienes cuenta? Regístrate
Compra esta imagen
Cargando...
Descripción: Ver traducción automática
Earths outermost layer is broken into about 13 principal plates, each of them carrying a continent, a part of an ocean, or both. These plates float on the magma in Earths mantle. This phenomenon is the central idea behind a theory called plate tectonics. According to the theory, several of the features on the planets surface can be explained by the movement of the plates. For instance, mountain ranges form where two plates collide, and faults form when two plates move apart or slide against each other. Plate tectonics also helps to explain the theory of continental drift, proposed by German scientist Alfred Wegener in 1912.
Crédito:
Album / Universal Images Group
Autorizaciones:
Modelo: No - Propiedad: No
¿Preguntas relacionadas con los derechos?
Tamaño imagen:
3952 x 2568 px | 29.0 MB
Tamaño impresión:
33.5 x 21.7 cm | 13.2 x 8.6 in (300 dpi)
Palabras clave: