You've probably heard that an old Space X rocket will crash into the Moon on the forth of March. It's very likely and a good excuse to look at a few other things.
The object in question is the second stage of a Falcon 9 that was used to take the Deep Space Climate Observatory to L1, the first Lagrange point in the Earth-Sun system.1 The observatory monitors the Sun, specifically the solar wind, from a vantage point a million miles closer to the Sun. In addition to science, it it gives about an hour's warning for satellites in orbit as well as power stations who need to prepare for large solar storms.
The Falcon's second stage has been looping around the Earth and Moon in an unstable orbit making a few close approaches to both Earth and Moon. This type of orbit crashes into either the Earth or Moon or is perturbed into a solar orbit. Exactly where is difficult to predict, but almost certainly it will be on the far side of the Moon. Too bad as it might be visible through a telescope if it were to hit an area in the night side of the Moon's near side.
That brings up another point. The far side of Moon is the part away from us. We see the dark side, at least some of it, all the time except when the Moon is perfectly full.
The Moon's rotation is tidally locked with the time it takes to make an orbit. Initially the Moon wasn't and rotated at a faster rate. Over millions of years tidal forces slowed it down to the point where it became locked. Roughly speaking the Moon is slightly egg-shaped rather than a perfect sphere. If the long axis through the Moon isn't pointed at the Earth, a torque is exerted which moves it back into position. Once locked it would take a large force to unlock the rotation.
The Moon's far side is only the dark side when we see a full Moon from Earth. If you're interested in how bright the Moon's surface is, the far side tends to be much brighter than the side we see. And the elliptical orbit of the Moon permits us to observe a bit more than half of the Moon's surface over about a month, although only half at once.
A few other neat things about the Earth-Moon system. The two bodies orbit a common point, or barycenter, about 1,700 km below the Earth's surface. (the barycenter for our solar system is sometimes outside the Sun, currently it's on the inside).
And finally the average distance from the Earth to the Moon is increasing at about the rate your fingernail grows. Tidal forces are also slowing the Earth's rotation. There's a point where a day on the Earth will be the same as the lunar day - something like 46 days long. It's a bit in the future though.. long after the Sun becomes a red giant and incinerates the Earth and long after before the Sun explodes forming a planetary nebulae. The Earth and Moon will have vanished long before, but planetary nebulae are beautiful.
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1 In a two-body system like the Earth and Sun, there are five points where the gravitational force on an object exactly equals the centripetal force necessary for that object to move with the bodies. L1 is closer to the Sun and great for a solar observatory, L2 is behind the Moon and a great place for a telescope like the James Webb Space Telescope. (note the little orbit around L2 - it turns out the JWST orbits L2, rather than sitting there so the Earth doesn't shield it from the solar energy it needs to operate. L3 is where the anti-Earth of science fiction would live.. (except it's unstable, so not really), an L4 and L5 are useful points on our orbit to put solar observatories that look at the Sun from an angle other than head-on.