Keeler (lunar crater)

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Keeler
Keeler crater 2075 med.jpg
Coordinates 10°12′S161°54′E / 10.2°S 161.9°E / -10.2; 161.9
Diameter 160 km
Depth 3.0 km [1]
Colongitude 200° at sunrise
Eponym James E. Keeler

Keeler is a large lunar impact crater that lies on the Moon's far side. It is connected along the eastern edge to Heaviside, a walled plain of similar dimensions. Keeler, however, is the younger of the two formations, with more clearly delineated features. To the northeast of Keeler is the smaller crater Stratton, and to the northwest lies Ventris.

Contents

Oblique photo of Keeler from Apollo 10 Keeler crater AS10-32-4823.jpg
Oblique photo of Keeler from Apollo 10

The outer rim of Keeler is roughly circular, with a straight segment where it is joined to Heaviside. The northern portion of the rim is more irregular, with an outward protuberance to the north-northwest. Portions of the inner wall have a terrace structure, especially along the southern half. Note the terraced walls of the crater. Within the crater interior, Planté lies on the eastern floor, adjacent to the inner wall. There is an interior ridge that runs from about the midpoint toward the west-southwest. The floor is generally level, with some areas of irregularity to the south. A few small craters mark the interior plain.

Measurements with the electron reflectometer instrument on board the Lunar Prospector showed that this crater is one of a number of impact sites that show demagnetization. The low magnetic reading lies at the center of this crater, and the reduced field extends outward to about one and a half crater diameters. Scientists believe that shock demagnetization is the cause. [2]

Keeler is one of the largest craters of Lower (Early) Imbrian age. [3]

The crater was named after American astronomer James Edward Keeler by the IAU in 1970. [4] Keeler was known as Crater 302 prior to naming. [5] [6] A highly eroded crater that is west of Keeler and somewhat larger than it was designated Crater 300, but it is currently unnamed.

Satellite craters

Oblique photo of Keeler from Apollo 13, with low sun angle (at the terminator) Keeler crater AS13-60-8635.jpg
Oblique photo of Keeler from Apollo 13, with low sun angle (at the terminator)
The central peak from Apollo 11. The highest peak is approximately 3.5 km above the crater floor. Keeler crater central peak AS11-38-5571.jpg
The central peak from Apollo 11. The highest peak is approximately 3.5 km above the crater floor.

By convention these features are identified on lunar maps by placing the letter on the side of the crater midpoint that is closest to Keeler.

KeelerLatitudeLongitudeDiameter
L13.3° S163.2° E71 km
S11.4° S158.0° E30 km
U9.1° S156.9° E29 km
V8.9° S158.3° E53 km

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References

  1. LTO-85C1 Plante L&PI topographic orthophotomap
  2. Halekas, J. S.; Mitchell, D. L.; Lin, R. P.; Frey, S.; Hood, L. L.; Acuna, M. H.; Binder, A. B. (May 2001). "Demagnetization Signatures of Lunar Impact Craters" (PDF). American Geophysical Union, Spring Meeting 2001, abstract #GP22A-11. Bibcode:2001AGUSM..GP22A11H . Retrieved 2010-01-28.
  3. The geologic history of the Moon. USGS Professional Paper 1348. By Don E. Wilhelms, John F. McCauley, and Newell J. Trask. U.S. Government Printing Office, Washington: 1987. Table 10.2.
  4. Keeler, Gazetteer of Planetary Nomenclature, International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN)
  5. Lunar Farside Chart (LFC-1A)
  6. Lunar Landmark Locations - Apollo 8, 10, 11, and 12 Missions. NASA technical note D-6082. Manned Spacecraft Center, Houston, Texas. November 1970. Figure 4.

Other sources