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Eratosthenes (crater)

Coordinates:14°28′N11°19′W / 14.47°N 11.32°W /14.47; -11.32
From Wikipedia, the free encyclopedia
Crater on the Moon
Feature on the moon
Eratosthenes
Coordinates14°28′N11°19′W / 14.47°N 11.32°W /14.47; -11.32
Diameter59 km
Depth3.6 km
Colongitude12° at sunrise
EponymEratosthenes
Eratosthenes-centered area in selenochromatic Image (Si) with some landmarks (yellow/normal, red/pyroclastic).
Eratosthenes (lower left of center) and surroundings from Apollo 17.NASA image.
Eratosthenes crater. Photo taken from Earth. Author: Georgi Georgiev, Stara Zagora, Bulgaria.

Eratosthenes crater is a relatively deeplunarimpact crater that lies on the boundary between theMare Imbrium andSinus Aestuummare regions. It forms the western terminus of theMontes Apenninus mountain range. It is named after ancient Greek astronomerEratosthenes ofCyrene,[1] who estimated thecircumference of the Earth, and thedistance from the Earth to the Sun.

Description

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The crater has a well-defined circular rim,terraced inner wall, central mountain peaks, an irregular floor, and an outerrampart of ejecta. It lacks aray system of its own, but is overlain by rays from the prominent craterCopernicus to the south-west.

TheEratosthenian period in thelunar geological timescale is named after this crater, though it does not define the start of this time period.[2] The crater is believed to have been formed about 3.2billion years ago.

At low Sun-angles, this crater is prominent due to the shadow cast by the rim. When the Sun is directly overhead, however, Eratosthenes visually blends into the surroundings, and it becomes more difficult for an observer to locate it. The rays from Copernicus lie across this area, and their higheralbedo serves as a form ofcamouflage.

In 1851 Shropshire AstronomerHenry Blunt constructed a model of the Moon's surface showing Eratosthenes. The model is based on observations made by Blunt with a reflecting telescope from his home in Shrewsbury and was displayed in the same year at the Great Exhibition, London.

From 1910 to the 1920s,William H. Pickering noted dark patches in the crater that varied in a regular manner over each lunar day. He first put forward the speculative idea that these patches appeared to migrate across the surface, suggestive of vegetation. Pickering believed that the Moon had a thicker atmosphere and reported seeing climatic variations such as frost and snow, leading him to refer to the crater as the "Gardens of Eratosthenes".[3] Later his views would change, and he would come to believe that the vegetation was instead "swarms of animal life",[4][5] which he often referred to as swarms of insects, or "lunar insects". The scientific community did not share his enthusiasm for these ideas,[6] but they received a degree of attention in the popular press of the time primarily due to Pickering's reputation.

Detail map of Mare Imbrium's features. Eratosthenes is marked "L".

Satellite craters

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Eratosthenes and its 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 Eratosthenes.

EratosthenesCoordinatesDiameter, km
A18°20′N8°20′W / 18.34°N 8.33°W /18.34; -8.33 (Eratosthenes A)5.7
B18°42′N8°42′W / 18.70°N 8.70°W /18.70; -8.70 (Eratosthenes B)5.3
C16°53′N12°23′W / 16.89°N 12.39°W /16.89; -12.39 (Eratosthenes C)5.2
D17°26′N10°54′W / 17.44°N 10.90°W /17.44; -10.90 (Eratosthenes D)3.8
E17°56′N10°53′W / 17.93°N 10.89°W /17.93; -10.89 (Eratosthenes E)3.8
F17°41′N9°55′W / 17.69°N 9.91°W /17.69; -9.91 (Eratosthenes F)4.0
H13°19′N12°15′W / 13.31°N 12.25°W /13.31; -12.25 (Eratosthenes H)3.5
K12°51′N9°16′W / 12.85°N 9.26°W /12.85; -9.26 (Eratosthenes K)4.3
M14°01′N13°35′W / 14.02°N 13.59°W /14.02; -13.59 (Eratosthenes M)3.5
Z13°45′N14°06′W / 13.75°N 14.10°W /13.75; -14.10 (Eratosthenes Z)0.6

References

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  1. ^"Eratosthenes".usgs.gov. Gazetteer of Planetary Nomenclature. International Astronomical Union. RetrievedSeptember 21, 2017.
  2. ^Wilhelms D. (1987)."Chapter 12. Eratosthenian System"(PDF).Geologic History of the Moon. United States Geological Survey Professional Paper 1348. pp. 249–250. Archived fromthe original(PDF) on 2013-05-14.
  3. ^Sheehan, William; Dobbins, Thomas A. (2001).Epic Moon: A History of Lunar Exploration in the Age of the Telescope. Vol. 410. Willmann-Bell. pp. 250, 251.ISBN 0943396700.
  4. ^Pickering, W. H. (1919)."Eratosthenes I, a study for the amateur".Popular Astronomy.27:579–583.Bibcode:1919PA.....27..579P.
  5. ^Pickering, W. H. (1924)."Eratosthenes".Popular Astronomy.32 (6):392–404.Bibcode:1924PA.....32..393P.
  6. ^Westfall, John; Sheehan, William (2014).Celestial Shadows: Eclipses, Transits, and Occultations. Vol. 410. Springer. p. 73.ISBN 9781493915354.

Further reading

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External links

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American projects
Soviet and
Russian projects
Chinese and
Russian project
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Proposed sites
Related
Craters on theMoon: C–F
C
D
E
F
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