Answer: B
Correct answer: The Moon
Tides are raised chiefly by the Moon. Although the Sun is vastly more massive, tidal force depends on the difference in gravitational pull across the Earth rather than on its strength, and that difference falls off with the cube of distance - so the much nearer Moon has about twice the tidal effect of the Sun. Two bulges form, one facing the Moon and one on the opposite side, and as the Earth turns beneath them most coasts see two high tides a day. The Sun’s smaller contribution explains the fortnightly cycle. When Sun, Earth and Moon align at new and full moon the two effects add, giving the large spring tides; when the Sun and Moon are at right angles, at the quarters, they partly cancel, giving the small neap tides. Spring here means to leap up, and has nothing to do with the season. Local range varies enormously with coastal shape: the Bay of Fundy in Canada sees over 15 metres.