Einstein (crater)

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Einstein
Einstein crater 4188 h2 4188 h3.jpg
Lunar Orbiter 4 image. Einstein is the larger, eroded crater. The smaller central crater is Einstein A.
Coordinates 16°36′N88°39′W / 16.60°N 88.65°W / 16.60; -88.65 Coordinates: 16°36′N88°39′W / 16.60°N 88.65°W / 16.60; -88.65
Diameter 181 km
Depth Unknown
Colongitude 91° at sunrise
Eponym Albert Einstein
Topographic map. Red means highlands and blue means lowlands. Einstein and Einstein A.jpg
Topographic map. Red means highlands and blue means lowlands.

Einstein is a large lunar impact crater that lies along the western limb of the Moon, which makes it difficult to observe from the Earth. The visibility of this formation is subject to libration effects, but even under the best conditions not much detail can be observed except from lunar orbit. Nearby craters of note include Moseley just to the north, Dalton along the eastern rim, Vasco da Gama just to the southeast, and Bohr to the south-southeast. The formation Vallis Bohr is visible to the south.

Contents

The outer rim of this walled plain has been strongly obliterated by many smaller impacts. Occupying the center of the interior floor is Einstein A, an impact crater with terraced inner walls and a central peak. The outer rampart of this concentric crater spreads across the interior floor, covering over half the diameter of Einstein. Several smaller craters also lie scattered across the floor, but there are sections of relatively flat surface in the southwest part of the floor. Two small craters on the west side have fissured floors. These are believed to be secondary craters from the Orientale impact to the south. [1]

The widespread notion that this crater was discovered by Patrick Moore in 1939 [2] [3] [4] is probably erroneous. [5] In the middle of the 20th century Hugh Percy Wilkins designated the crater Caramuel to honor Juan Caramuel y Lobkowitz. [6] [7] The crater was known under this unofficial name for some time, [4] [8] but neither this name, nor almost all of Wilkins' other nomenclature, were adopted by the International Astronomical Union. [9] In 1963 E. Whitaker and D.W.G. Arthur named thie crater Einstein after Albert Einstein, [8] and in 1964 this name was adopted by the IAU. [10] Wilkins' map also contained a crater called Einstein, but it is a less prominent one [8] Simpelius D. [2]

Satellite craters

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

Einstein [10] CoordinatesDiameter, km
A 16°41′N88°15′W / 16.69°N 88.25°W / 16.69; -88.25 (Einstein A) 50
R 13°50′N91°53′W / 13.83°N 91.88°W / 13.83; -91.88 (Einstein R) 20
S 15°06′N91°40′W / 15.10°N 91.67°W / 15.10; -91.67 (Einstein S) 20

See also

Related Research Articles

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Euler (crater)

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Bohnenberger (crater)

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Artamonov (crater)

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Beals (crater) Lunar impact crater

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Bohr (crater) Lunar surface depression

Bohr is a lunar impact crater that is located near the western lunar limb, in the area that is affected by librations. It is attached to the southwestern rim of the larger, eroded Vasco da Gama formation, and to the southeast of the crater Einstein. The crater was observed for the first time in 1963, by Arthus and Ewen Whitaker in the book Rectified Lunar Atlas.

Fechner (crater) Lunar surface depression

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Becquerel (lunar crater) Lunar impact crater

Becquerel is a lunar impact crater that lies in the northern hemisphere on the far side of the Moon. This is an ancient and heavily worn formation that is now little more than an irregular buri in the surface. The outer rim has been worn and reshaped until it forms a rugged, mountainous region around the flatter interior.

Barkla (crater) Lunar impact crater

Barkla is a lunar impact crater that lies near the eastern limb of the Moon. It is located to the east of the prominent crater Langrenus, and was formerly designated Langrenus A before being renamed by the IAU in 1979. Due east of Barkla is Kapteyn, a formation only slightly larger with a similar size. Southwest of Barkla is the crater Lamé.

Cusanus (crater) Lunar crater

Cusanus is a lunar impact crater that is located near the northeastern limb of the Moon. In this location the crater appears very foreshortened when observed from the Earth, and its visibility is affected by libration. The northern rim of Cusanus is nearly joined to the south-southeastern rim of the larger crater Petermann. To the west is Baillaud and to the southeast is Hayn.

Damoiseau (crater) Lunar impact crater

Damoiseau is a lunar impact crater that is located just to the west of the Oceanus Procellarum, in the western part of the Moon's near side. It lies due east of the prominent crater Grimaldi, a walled plain with a distinctive dark floor. Due south of Damoiseau is the crater Sirsalis.

Dollond (crater)

Dollond is a small lunar impact crater that is located in the central region of the Moon, to the north of the crater Abulfeda. It was named after British optician John Dollond. Due west of Dollond is Anděl. Dollond is circular and cone shaped, with a tiny floor at the midpoint of the sloping interior walls.

Bliss (crater) Lunar impact crater

Bliss is small lunar impact crater that is located just to the west of the dark-floored crater Plato. It lies in a region of continental terrain between Mare Imbrium to the south and Mare Frigoris to the north. This crater is bowl-shaped, with a small interior floor at the midpoint and a somewhat eroded outer rim.

Bondarenko (crater) Lunar impact crater

Bondarenko is a lunar impact crater on the far side of the Moon. It is located to the northeast of the large, dark-floored crater Tsiolkovskiy, and south of the crater Chauvenet. This is a worn crater formation with an irregular floor, similar to other craters in the area, which are covered by ejecta from Tsiolkovskiy.

Einthoven (crater)

Einthoven is a lunar impact crater that is located on the far side of the Moon. It is located beyond the region of the surface that is sometimes brought into view due to libration, and so can not be viewed from the Earth. Einthoven is located to the northeast of the huge walled plain Pasteur.

FitzGerald (crater)

FitzGerald is a large lunar impact crater on the far side of the Moon. It lies to the west-southwest of the crater Cockcroft, and about two crater diameters to the northeast of Morse.

Fleming (crater) Lunar impact crater

Fleming is a large lunar impact crater that is located on the Moon's far side, and cannot be seen from the Earth. It lies about a crater diameter to the east-northeast of Hertz, and to the northwest of Lobachevskiy.

References

  1. The geologic history of the Moon, 1987, Wilhelms, Don E.; with sections by McCauley, John F.; Trask, Newell J. USGS Professional Paper: 1348. Figure 3.9 A (online)
  2. 1 2 Moore P.; Cattermole P. J. (1967). The Craters of the Moon. New York: W. W. Norton and Company Inc. pp. 124 (image on p.63).
  3. Allen D. A. (June 1966). "The Lunar Crater Caramuel". Journal of the British Astronomical Association. 76: 248–255. Bibcode:1966JBAA...76..248A.
  4. 1 2 Allen D. A.; Andrews C. J. (May 1969). "The last word on Einstein Crater (Caramuel)". Journal of the British Astronomical Association. 79: 288–290. Bibcode:1969JBAA...79..288A.
  5. Mobberley M. (2013). It Came From Outer Space Wearing an RAF Blazer!: A Fan's Biography of Sir Patrick Moore. Springer Science & Business Media. pp. 15, 22–23, 102, 171, 581. doi:10.1007/978-3-319-00609-3. ISBN   978-3-319-00609-3.
  6. "Wilkins 300-inch Map Names (from Wilkins and Moore, 1961)". the-moon.wikispaces.com. Retrieved 2014-12-11.
  7. "Unofficial Names of Hugh Percy Wilkins (from Wilkins and Moore, 1961)". the-moon.wikispaces.com. Retrieved 2014-12-11.
  8. 1 2 3 Longshaw N. (June 2014). P. Grego (ed.). "Einstein surprise" (PDF). The British Astronomical Association Lunar Section Circular. 51 (6): 10–12. Archived from the original (PDF) on December 14, 2014.
  9. Whitaker E. A. (2003). Mapping and Naming the Moon: A History of Lunar Cartography and Nomenclature. Cambridge University Press. pp. 230, 235. ISBN   9780521544146.
  10. 1 2 "Einstein". Gazetteer of Planetary Nomenclature. International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN). 2010-10-18. Retrieved 2014-12-13.

Sources