Tides are caused by the gravitational interactions between the Earth, moon, and sun. This causes two tidal bulges in the Earth's oceans, with one bulge facing the moon and the other on the opposite side. As the Earth rotates daily and revolves around its axis, different locations experience high and low tides depending on their alignment with the tidal bulges. Specifically, high tides occur when a location is aligned under the moon or opposite the moon, while low tides occur when a location is at a right angle to the tidal bulges.