Respuesta :

Answer:

The pacific floor (oceanic crust) is thinner and more denser

Explanation:

The continental crust have a thickness of about 35 to 40 km on an average, and are composed of rocks that has less denser granitic minerals such as feldspar, quartz.

On the other hand, the oceanic crust have a thickness of about 7 to 10 km on an average, and it is comprised of denser mafic rocks that contains high amount of olivine and pyroxene minerals.

Due to this, the oceanic crust subducts below the continental crust during the time of collision.

Thus, the pacific floor (oceanic crust) is thinner and more denser, in comparison to the South American continental crust.

The Pacific floor will be "thinner and more denser".

  • The continental crust comprises stones with less compressive granitoid components including such silicate minerals and seems to have an external layer of thirty-six to forty km.
  • This same oceanic crust has an external layer of seven to ten km as well as is made up of denser basalts materials rich in olivine and pyrite minerals.

Thus the response above is appropriate.

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