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What is an axial tilt?

What is an axial tilt? Here are some definitions.

Noun
  1. (physics) The angle between the rotational axis and the orbital axis of an orbiting celestial object.
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These Milankovitch cycles are tied to Earth's wobbly orbital axis, its oscillating axial tilt, and its orbital eccentricity.
The axial tilt of Uranus is 98°, so effectively the planet is now spinning in a direction opposite to its orbital motion around the sun.
Paleontological evidence and computer simulations show that Earth's axial tilt is stabilized by tidal interactions with the Moon.
Uranus' unique attribute, though, is that its axial tilt is 98° so that it orbits the Sun on its side every 84 years, presenting first one pole towards the Sun and then the other.
The angle of Earth's axial tilt is relatively stable over long periods of time.
Due to Earth's axial tilt, the amount of sunlight reaching any given point on the surface varies over the course of the year.

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