Tebbutt (crater)
Encyclopedia
Tebbutt is a lunar
Moon
The Moon is Earth's only known natural satellite,There are a number of near-Earth asteroids including 3753 Cruithne that are co-orbital with Earth: their orbits bring them close to Earth for periods of time but then alter in the long term . These are quasi-satellites and not true moons. For more...

 crater
Impact crater
In the broadest sense, the term impact crater can be applied to any depression, natural or manmade, resulting from the high velocity impact of a projectile with a larger body...

 that is located near the southwestern edge of Mare Crisium
Mare Crisium
Mare Crisium is a lunar mare located in the Moon's Crisium basin, just northeast of Mare Tranquillitatis. This basin is of the Pre-Imbrian period, 4.55 to 3.85 billion years ago. This mare is in diameter, and 176,000 km2 in area. It has a very flat floor, with a ring of wrinkled ridges...

. It was formerly designated Picard G before being named by the IAU
International Astronomical Union
The International Astronomical Union IAU is a collection of professional astronomers, at the Ph.D. level and beyond, active in professional research and education in astronomy...

, and lies south of the crater Picard
Picard (crater)
Picard is a lunar impact crater that lies in Mare Crisium. To the west is the almost completely flooded crater Yerkes. Due east of Picard is the tiny Curtis. being slightly larger than Peirce to the north-northwest...

. To the north of Tebbutt, but farther east than Picard, is the flooded Lick
Lick (crater)
Lick is a lunar crater that has been flooded with basaltic lava. The north rim is attached to the smaller, bowl-shaped crater Greaves. Lick lies on the southwest edge of Mare Crisium. Its rim is broken at the north and south ends, and the southwest rim is attached to the crater remnant Lick A...

.

This crater has a worn and damaged outer rim along its eastern half, but the rim is all but nonexistent on the western face, being little more than a pair of curved ridges beneath the surface. Lava flows have overflowed this western rim and submerged the interior, leaving a relatively level and featureless interior. A small craterlet marks the southern end of the interior floor, and several tiny craters mark the surviving rim.
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