Craterra

Montes Cordillera / Western Limb

A Floor-Fractured Late Imbrian Crater on the Cordillera Rim

Sitting along the outer ring of Mare Orientale, Schlüter preserves terraced walls, dark floor deposits, and a plagioclase-rich central ridge.

Feature Profile & Selenographic Data

Feature type
crater
Coordinates
5.93° S · 83.39° W
Diameter
87.55 km
IAU approval
1964/01/01 00:00:00
LAC quadrangle
LAC-73 · Riccioli
Geological Period
Late Imbrian

Geological Chronicle

Schlüter is an 87.55-kilometer impact crater located near the western limb of the Moon's near side. The structure lies along the northwestern flank of the Montes Cordillera, the outer mountain ring that encircles Mare Orientale, nearly attached to the damaged crater Hartwig on its eastern rim.

Formed during the Late Imbrian epoch, the crater displays a roughly circular outer rim with bulges toward the north and southeast. Its inner perimeter contains systems of terraces alongside a slumped northern inner wall and a small double-crater set into the southern inner slope.

Schlüter is a floor-fractured crater with a slender rille near the northwestern wall and a patch of low-albedo material along the northern margin. In the midpoint of the floor, an elongated central ridge extends in a northerly direction, where infrared observations have identified pure crystalline plagioclase.

Chronology & Exploration

  1. Late Imbrian Crater Formation

    Schlüter forms along the northwestern face of the Montes Cordillera.

Scientific Sources & References

Name Origin

Heinrich; German astronomer (1815-1844).

Interactive Lunar Surface

Explore Schlüter in 3D

Inspect lunar elevation data and the official selenographic position.