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Comentario: 
Much of the rock doesn't wear away, nonetheless; instead, it remains hooked up, adding new 
mass to the continent. These hardened rock varieties slowly 
wear away contributing new sediment to the sea.

Sea flooring sediment between the trench and shore is caught within the squeeze, crumpled up 
and uplifted. He realized that there had to be a connection between marine deep sea sedimentation and mountain constructing.
Actually, the essential key to mountain building lies in understanding this hyperlink 
between ocean basins and continents. Throughout a growing mountain vary, the whole 
rock cycle may be energetic creating new continental crust.

Early in Earth history, there may have been a a lot thinner lithosphere, which promoted a way 
more random and quicker shorter cycle sample of convection to give us these historical protocontinents,
which we call the greenstone belts. At about 2 billion years ago the general 
tectonic sample seems to have changed, where there was a higher organization of bigger plates 
and continental margins, which started to move into 
extra of a inflexible plate tectonic area, and that change 
may have been related to the event of a thick lithosphere.

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