Craterra

Western Mare Imbrium

A Well-Preserved Impact Crater in the Lava Plains of Mare Imbrium

Excavated during the Eratosthenian period, Delisle retains a polygonal rim and hummocky ejecta skirt amid a network of lunar rilles.

Feature Profile & Selenographic Data

Feature type
crater
Coordinates
29.98° N · 34.68° W
Diameter
24.83 km
IAU approval
1935/01/01 00:00:00
LAC quadrangle
LAC-39 · Aristarchus
Geological Period
Eratosthenian

Geological Chronicle

Delisle sits in the western part of Mare Imbrium, spanning 24.83 kilometers in diameter north of the crater Diophantus and northwest of the ridge Mons Delisle. Excavated into basaltic lava flows during the Eratosthenian period, the crater has not been significantly modified by subsequent processes, leaving its structure relatively fresh.

The rim displays a somewhat polygonal outline surrounded by a rampart and a skirt of hummocky terrain formed from impact ejecta. A low central rise rests on the floor, accompanied by slight slumping along the inner wall.

The surrounding plains are marked by sinuous channels, including the 150-kilometer Rima Diophantus to the south and Rima Delisle to the northeast. Johann H. Schröter included the feature in lunar nomenclature as "de l'Isle" in 1791, honoring French astronomer Joseph-Nicolas Delisle, before the International Astronomical Union officially adopted its modern designation in 1935.

Chronology & Exploration

  1. Eratosthenian Impact Formation

    Delisle forms in the basaltic lava flows of western Mare Imbrium.

  2. 1791 Lunar Nomenclature Entry

    Johann H. Schröter records the crater in lunar nomenclature as "de l'Isle".

  3. 1935 IAU Name Adoption

    The International Astronomical Union officially adopts the modern designation Delisle.

Scientific Sources & References

Name Origin

Joseph Nicolas; French astronomer (1688-1768).

Interactive Lunar Surface

Explore Delisle in 3D

Inspect lunar elevation data and the official selenographic position.