This can be a decent approximation because the Earth's magnetic field is roughly that of a dipole.
It's easy to look-up the Radius of the earth, and we can use a rough estimate of 0.23 gauss for the horizontal component of the magnetic field at 40 degrees latitude.
A simple expression for the magnetic field due to a dipole in spherical polar coordinates is
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There's no dependence on azimuthal angle because of the symmetry axis along the dipole.
The dipole moment is then
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And the current in a loop 1/3 the radius of the earth required to create a field of that strength is
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That's a lot of statcoulombs!
This is Problem 2.2 from Classical Electromagnetic Radiation
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