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In contrast, the Lunar distance (LD or ), or Earth–Moon characteristic distance, is a unit of measure in astronomy. More technically, it is the semi-major axis of the geocentric lunar orbit . The lunar distance is on average approximately 385,000 km (239,000 mi), or 1.28 light-seconds ; this is roughly 30 times Earth's diameter or 9.5 times ...
The Moon is Earth's only natural satellite. It orbits at an average distance of 384,400 km (238,900 mi), about 30 times the diameter of Earth. Tidal forces between Earth and the Moon have synchronized the Moon's orbital period (lunar month) with its rotation period at 29.5 Earth days, causing the same side of the Moon to always face Earth.
The Sun's gravitational effect on the Moon is more than twice that of Earth's on the Moon; consequently, the Moon's trajectory is always convex [25] [26] (as seen when looking Sunward at the entire Sun–Earth–Moon system from a great distance outside Earth–Moon solar orbit), and is nowhere concave (from the same perspective) or looped.
The first correction to the lunar distance is the distance between the limb of the Moon and its center. Since the Moon's apparent size varies with its varying distance from the Earth, almanacs give the Moon's and Sun's semidiameter for each day. [12] Additionally the observed altitudes are cleared of semidiameter.
Earth is about to pluck a second moon from an asteroid belt — but we only get this mini ... 2025, according to NASA, it will skim past Earth at a distance of about 1.1 million miles (1.8 million ...
But we have had them in the past, as in the case of 2022 NX1 – which joined Earth as a mini-Moon in 1981 and then came back in 2022. Other planets also have their own mini-moons, with Jupiter ...
Earth's moon is roughly 2,000 times more massive than Mimas. ... Mimas follows an elliptical orbit around Saturn at an average distance of about 115,000 miles (186,000 km). As its distance from ...
The distance to the Moon can be measured with millimeter precision. [27] The Moon is spiraling away from Earth at a rate of 3.8 cm/year. [24] [42] This rate has been described as anomalously high. [43] The fluid core of the Moon was detected from the effects of core/mantle boundary dissipation. [44]