As a student, I once played around with the numbers, and seem to remember that by assuming a composition of the lightest silica rocks, a planet could have about 121 times the surface area of Earth, with a surface gravity of 1 G.
I thin this is far less than the size of Jupiter, double the radius means far more than double the surface.
I had to assume even density through the planet though. And there would be practically no iron etc except meteoric on the planet. Internal processes would probably not match earths anyway. So no continents , continental drift or ocean basins.
Note that you can have a planet that is a diamond with some slagging on top.
A planet made out of pure carbon of Earth mass or greater wouldn't have a diamond at its core - it would have a denser amorphous carbon core. The diamond layer would probably start mid-mantle or so.
And this is the problem with the light silica planet as well - even such light minerals will be crushed to a significant density by the sheer mass of stuff above.
And a giant iron poor planet could well have quite familiar processes - even if it didn't have any radioactive elements in the core and mantle, stored heat from planetary formation would drive some sort of active crustal processes for quite a long time. For a planet with 121 times the earth's surface, the stored heat would probably drive plate tectonics for longer than the planet's star would last.
fasquardon