Linné (crater)

From Wikipedia, the free encyclopedia

Crater characteristics

Linné crater from orbit. NASA photo.
Coordinates 27.7° N, 11.8° E
Diameter 2.4 km
Depth 0.6 km
Colongitude   348° at sunrise
Eponym Carl von Linné

Linné is a small lunar impact crater located in the western Mare Serenitatis. The maria around this feature is virtually devoid of other features of interest. The nearest named crater is Banting to the east-southeast.

The estimated age of this crater is only a few tens of millions of years. It has a bowl shape, and is surrounded by a blanket of ejecta formed during the original impact. But it lacks a ray system. This ejecta has a relatively high albedo, making the feature appear "bright".

In 1866, the experienced lunar observer and mapmaker Johann Friedrich Julius Schmidt made the surprising claim that Linné had changed its appearance. Instead of a normal, somewhat deep crater it had become a mere white patch. A controversy arose that continued for many decades. However, this crater size tests the limit of visual perception of Earth-based telescopes. In conditions of poor seeing this feature can appear to vanish from sight[1] (see also transient lunar phenomenon).

[edit] Satellite craters

By convention these features are identified on lunar maps by placing the letter on the side of the crater mid-point that is closest to Linné crater.

Linné Latitude Longitude Diameter
A 28.9° N 14.4° E 4 km
B 30.5° N 14.2° E 5 km
D 28.7° N 17.1° E 5 km
F 32.3° N 13.9° E 5 km
G 35.9° N 13.3° E 5 km
H 33.7° N 13.8° E 3 km

The following craters have been renamed by the IAU.

[edit] References

  • See the reference table for the general listing of literature and web sites that were used in the compilation of this page.

[edit] External links