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Contesta sí para enunciados que son correctos y no para los que son incorrectos, guíate del modelo 3D y la ficha científica.

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Mexico

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CenoteOnline version

Contesta sí para enunciados que son correctos y no para los que son incorrectos, guíate del modelo 3D y la ficha científica.

by Salmerón Méndez Amanda Alejandra
1

La disolución de roca caliza y el colapso del techo de una cavidad es un proceso geomorfológico que explica mejor el origen de un cenote.

2

La acumulación exclusiva de sedimentos finos fluviales es un rasgo característico que distingue mejor a un cenote de una gruta.

3

La caliza es el tipo de roca más común asociada al desarrollo cenotes.

4

El cenote se forma únicamente por evaporación superficial.

5

La disolución progresiva del techo de la cavidad es una condición que favorece la evolución de un cenote abierto.

6

El colapso parcial o total del techo de la cavidad es una condición que favorece la evolución de un cenote abierto.

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