  In most theories of planet formation, the snow-line represents a boundary
between the emergence of the interior rocky planets and the exterior ice
giants. The wide separation of the snow-line makes the discovery of transiting
worlds challenging, yet transits would allow for detailed subsequent
characterization. We present the discovery of Kepler-421b, a Uranus-sized
exoplanet transiting a G9/K0 dwarf once every 704.2 days in a near-circular
orbit. Using public Kepler photometry, we demonstrate that the two observed
transits can be uniquely attributed to the 704.2 day period. Detailed light
curve analysis with BLENDER validates the planetary nature of Kepler-421b to >4
sigmas confidence. Kepler-421b receives the same insolation as a body at ~2AU
in the Solar System and for a Uranian albedo would have an effective
temperature of ~180K. Using a time-dependent model for the protoplanetary disk,
we estimate that Kepler-421b's present semi-major axis was beyond the snow-line
after ~3Myr, indicating that Kepler-421b may have formed at its observed
location.
