Step 1:
For the Geocentric Axial Dipole model, the formula for the magnetic inclination (\(I\)) at a latitude \(\phi\) is:
\[
I = \tan^{-1}( \tan(\phi) )
\]
Step 2: Given latitude \(\phi = 30^\circ\), we can substitute:
\[
I = \tan^{-1}( \tan(30^\circ) ) = 60^\circ
\]
Thus, the inclination at 30°N is \(60^\circ\).
\[
\boxed{60^\circ}
\]