Craterra

Lunar Far Side

An Imbrian Impact with Crystalline Plagioclase

Spanning 84 kilometers south of the walled plain Hertzsprung, Ioffe displays terraced inner walls and an interior ridge bearing pure crystalline plagioclase.

Feature Profile & Selenographic Data

Feature type
crater
Coordinates
14.38° S · 129.16° W
Diameter
83.95 km
IAU approval
1970/01/01 00:00:00
LAC quadrangle
LAC-89 · Lucretius
Geological Period
Late Imbrian

Geological Chronicle

Located on the far side of the Moon south of the walled plain Hertzsprung, the impact crater Ioffe measures 83.95 kilometers across. The formation is attached directly to the southwestern outer rim of Fridman, with a short stretch of terrain separating its southeastern margin from neighboring Belopol'skiy.

Dating to the Late Imbrian period on the lunar geologic timescale, Ioffe is a relatively youthful crater with a well-defined outer rim and a terraced inner wall. Subsequent impacts have marked the perimeter, including a smaller crater along the edge joined to Fridman and a small craterlet along the northwestern rim.

The interior floor is relatively level and free of notable impacts, interrupted only by a low, uneven ridge extending from just east of the midpoint to the south-southwestern inner wall. Infrared spectroscopy identified the signature of pure crystalline plagioclase on this central ridge. The crater is named after Soviet physicist Abram Ioffe.

Chronology & Exploration

  1. Late Imbrian Crater Formation

    Ioffe forms during the Late Imbrian period on the lunar geologic timescale.

Scientific Sources & References

Name Origin

Joffe, Abram Feodorovich; Soviet physicist (1880-1960).

Interactive Lunar Surface

Explore Ioffe in 3D

Inspect lunar elevation data and the official selenographic position.