"I think the earth will see some rather dramatic quakes by the end of the century"
No, not even remote as fast. First you have to remove most oft the ice, then you will have the isostatic rebound of the crust and the mantle.
Here in Sweden we still feel earth quakes from this mechanism and the crust is still rising with up to 4 cm a year, so it is a very slow process.
Another mechanism, which in my opinion is more serious, is melting of magma due to pressure release. All hot magma from below is originaly transported as "solid" rock up to a distinct border when it melts. The melting point of rock is strong pressure related, less pressure means lower melting point. Hot mantle material will melt emediately, when the ice is removed, when it is exactly at the border of melting conditions.
Pressure release due to melting ice is a rather fast mechanism, capable to induce melt of otherwise not melting mantle or crustmaterial. And then booom......