That's a common misconception! While the Moon's gravity is the main driver of tides, it's not as simple as just the point farthest from the Moon experiencing low tide. Here's why:

* Gravitational Pull: The Moon's gravity pulls on the Earth, but the force is stronger on the side of the Earth facing the Moon. This pulls the water towards the Moon, creating a bulge.

* Centrifugal Force: The Earth and Moon are rotating around a common center of mass. This rotation creates a centrifugal force that pushes water away from the center of rotation, creating a bulge on the opposite side of the Earth from the Moon.

* Combined Effect: The combination of the Moon's gravitational pull and centrifugal force creates two bulges of water, one on the side facing the Moon and one on the side facing away. These bulges are high tides. The areas between the bulges experience low tides.

In summary:

* High tide: Occurs on the side of Earth facing the Moon and the side facing away from the Moon.

* Low tide: Occurs in the areas between the high tide bulges.

So, the point on Earth farthest from the Moon actually experiences a high tide, not a low tide.