Module 1 ended on a promise: this module covers how missions actually learn anything. Every mission ahead in this course — to the Moon, Mars, the outer planets, or a small body — is one of five basic methods. What each one can tell you matters less on its own than what it can't, since that's what decides why a later mission gets built at all.
Each method generally costs more and takes longer than the one before it — and generally tells you more in return.
Gets you: A first look — often the very first images or data of a target ever obtained — for relatively low cost and travel time. Can't: Show how the target changes over time, or guarantee the brief pass caught a representative moment rather than an unusual one.
Gets you: Sustained observation over months or years — comprehensive mapping, and the ability to watch seasons, weather, or geology change over time. Can't: Examine surface material directly, and entering orbit around some targets costs far more delta-v (Module 1) than a flyby ever would.
Gets you: Direct surface contact — close-up imaging and instruments that need to physically touch the ground, like seismometers or weather stations. Can't: Move. A lander characterizes exactly one spot, permanently, no matter how much diversity exists elsewhere on the surface.
Gets you: Everything a lander gets, plus mobility — the ability to investigate multiple locations across a single mission's lifetime, dramatically expanding geologic diversity sampled. Can't: Match the precision of an Earth-based laboratory — onboard instruments are capable, but still a compromise built for mass and power limits (Module 1's mass budget), and travel is slow, often just meters to kilometers over years.
Gets you: The genuine article, back on Earth — full laboratory-grade analysis with equipment no spacecraft could ever carry, at a level of precision nothing remote can match. Can't: Happen often. It's the most technically demanding and expensive method by far — a round trip, not a one-way delta-v budget — which is exactly why only a handful of missions, including JAXA's Hayabusa and Hayabusa2, have ever pulled it off.
Missions don't have to climb these five steps in order for every destination. Some targets get repeated flybys before anyone ever attempts orbit; some well-understood targets have gone straight to a lander once the risk was judged acceptable. What's consistent isn't the sequence — it's the trade-off: more commitment generally buys more depth of knowledge, at a real cost in time, money, and risk. Every destination module ahead — the Moon, Mars, the outer planets, small bodies — will describe its missions in exactly these five terms, so this is the vocabulary the rest of the course runs on.
NASA JPL mission design overview materials, and NASA/ESA public educational materials distinguishing flyby, orbiter, lander, rover, and sample-return mission classes.
Module 3 puts this methodology to work on the Moon — Apollo through Artemis, and why it matters again strategically and scientifically.