How Mars is made. The outer shell is a 20,000-face sphere whose every vertex is moved by the real MOLA elevation at that point (NASA's public-domain MEGDR grid, 2 pixels per degree), exaggerated about three times so a 100 mm globe carries Olympus Mons as a 0.9 mm rise and Hellas as a 0.3 mm dip you can feel. Faces are colored by the elevation dichotomy that splits Mars — below −2.5 km is lowland — with the residual polar caps in a third color. Two hemisphere shells meet at the equator on a rabbet (lap) joint that Anoor bonds during assembly; the southern shell carries a small flat cut so the globe leans at Mars' real 25.19° obliquity. Made in PETG.
How the Moon is made. The outer shell is a 20,000-face sphere whose every vertex is moved by the real LOLA elevation at that point (NASA's public-domain Lunar Orbiter Laser Altimeter grid, 2 pixels per degree), exaggerated about twice so a 100 mm globe carries the farside highlands as a 0.6 mm rise and the deep basins as dips you can feel. The dark color goes where the Moon is dark — the maria, drawn from NASA's own LROC brightness map — and the highlands take the light one; the Moon has no polar caps, so there are two colors and the name. Two hemisphere shells meet at the equator on a rabbet (lap) joint that Anoor bonds during assembly; the southern shell carries a small flat cut so the globe leans at the Moon's 6.68° tilt to its orbit, the nearside facing you. Made in PETG.
How Earth goes together. The globe is two hemisphere shells that meet at the equator on a rabbet (lap) joint — a lip on the northern shell nests into a matching groove on the southern shell, keeping the land/ocean seam aligned all the way around. This joint is registration only, not a snap-fit: Anoor bonds it permanently during assembly, so it's never meant to be reopened. Both pole tips seat into a half-meridian arc stand that's tilted to Earth's real 23.44° axial tilt — the same obliquity that actually gives Earth its seasons, not a decorative angle.