Moon
Natural satellite orbiting the Earth / From Wikipedia, the free encyclopedia
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The Moon is Earth's only natural satellite. It orbits around Earth at an average distance of 384400 km (238900 mi; 1.28 ls), or about 30 times Earth's diameter. The Moon faces Earth always with its near side by having a rotation period that equals its orbital period, resulting from being tidally locked to Earth. This period is in relation to the Sun 29.5 days long and visible as the cycle of the lunar phases. For Earth, the Moon has been aside from the Sun the most influential celestial object, particularly with its gravitational influence it has been the main driver of Earth's tides.
Designations | |||||||||||||
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Designation | Earth I | ||||||||||||
Adjectives | |||||||||||||
Symbol | or | ||||||||||||
Orbital characteristics | |||||||||||||
Epoch J2000 | |||||||||||||
Perigee | 362600 km (356400–370400 km) | ||||||||||||
Apogee | 405400 km (404000–406700 km) | ||||||||||||
384399 km (1.28 ls, 0.00257 AU)[1] | |||||||||||||
Eccentricity | 0.0549[1] | ||||||||||||
29.530589 d (29 d 12 h 44 min 2.9 s) | |||||||||||||
Average orbital speed | 1.022 km/s | ||||||||||||
Inclination | 5.145° to the ecliptic[2][lower-alpha 1] | ||||||||||||
Regressing by one revolution in 18.61 years | |||||||||||||
Progressing by one revolution in 8.85 years | |||||||||||||
Satellite of | Earth[lower-alpha 2][3] | ||||||||||||
Physical characteristics | |||||||||||||
Mean radius | 1737.4 km (0.2727 of Earth's)[1][4][5] | ||||||||||||
Equatorial radius | 1738.1 km (0.2725 of Earth's)[4] | ||||||||||||
Polar radius | 1736.0 km (0.2731 of Earth's)[4] | ||||||||||||
Flattening | 0.0012[4] | ||||||||||||
Circumference | 10921 km (equatorial) | ||||||||||||
3.793×107 km2 (0.074 of Earth's) | |||||||||||||
Volume | 2.1958×1010 km3 (0.02 of Earth's)[4] | ||||||||||||
Mass | 7.342×1022 kg (0.0123 of Earth's)[1][4][6] | ||||||||||||
Mean density | 3.344 g/cm3[1][4] 0.606 × Earth | ||||||||||||
1.622 m/s2 (0.1654 g; 5.318 ft/s2)[4] | |||||||||||||
0.3929±0.0009[7] | |||||||||||||
2.38 km/s (8600 km/h; 5300 mph) | |||||||||||||
27.321661 d (spin-orbit locked) | |||||||||||||
Equatorial rotation velocity | 4.627 m/s | ||||||||||||
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North pole right ascension |
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North pole declination | 65.64°[10] | ||||||||||||
Albedo | 0.136[11] | ||||||||||||
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Surface absorbed dose rate | 13.2 μGy/h (during lunar daytime)[14] | ||||||||||||
Surface equivalent dose rate | 57.0 μSv/h (during lunar daytime)[14] | ||||||||||||
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0.2[15] | |||||||||||||
29.3 to 34.1 arcminutes[4][lower-alpha 4] | |||||||||||||
Atmosphere[16] | |||||||||||||
Surface pressure |
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Composition by volume | |||||||||||||
The Moon's mass, density and surface gravity of about one-sixth of Earth's (at 0.1654 g), are rivaled among Solar System satellites only by Jupiter's moon Io. It is a satellite planet in geophysical terms and among all planetary-mass objects of the Solar System larger and more massive than all of its known dwarf planets.[17] Its diameter is 3,474 km (2,159 mi), which is roughly one-quarter that of Earth or about the width of Australia,[18] making it by far the largest and most massive satellite in the Solar System in relation to its parent planet and the fifth-largest Solar System satellite overall. The body of the Moon is differentiated and terrestrial, with no significant hydrosphere, atmosphere, or magnetic field. It formed 4.51 billion years ago, not long after Earth's formation, out of the debris from a giant impact between Earth and a hypothesized Mars-sized body called Theia.
The lunar surface is covered in impact craters and is marked, mostly on the near side of the Moon, by dark maria ("seas"), which are plains of cooled magma. These maria formed when large impacts on the far side of the Moon heated up low lying layers of its crust on the near side. The Moon is, beside when passing through Earth's shadow during a lunar eclipse, always illuminated by the Sun, but from Earth the visible illumination shifts during its orbit, producing the lunar phases.[19] The Moon is the brightest celestial object in Earth's night sky. This is mainly due to its large angular diameter, while the reflectance of the lunar surface is comparable to that of asphalt. The apparent size is nearly the same as that of the Sun, allowing it to cover the Sun almost completely during a total solar eclipse. From Earth about 59% of the lunar surface is visible over time due to cyclical shifts in perspective (libration), making parts of the far side of the Moon visible.
For humans the Moon has been an important source of inspiration and knowledge, having been crucial to cosmography, mythology, religion, art, time keeping, natural science, and spaceflight. On September 13, 1959 the Soviet Union's Luna 2 was the first human-made object to reach the Moon and any extraterrestrial body, and the first soft landing was achieved in 1966 by Luna 9. On July 20, 1969 the United States' Apollo 11 mission landed humans for the first time on the Moon, and any extraterrestrial body, at Mare Tranquillitatis with the lander Eagle. Five more crews were sent between then and 1972, each with two men landing on the surface. The longest stay was 75 hours by the Apollo 17 crew. Thereafter exploration of the Moon has continued robotically, with crewed missions being planned to return starting in the late 2020s.