she ventured. âAre you worried about meteors hitting us?â
âYes, but not the way youâre thinking.â He waved toward her window. âTeardrop Lake over by Ceres. If you look at it on satellite photos you can see that itâs a circular depression thatâs been eroded by the rivers entering and leaving. The Dead Sea southeast of Olympus is the same thing plus what appear to be fault-line appendages. Even Splayfoot Bay shows a deep area in the center thatâs basically circular. This planet has been literally pelted with rocks over maybe the last half million yearsânot surprising when you consider how close we are to the asteroid belt here. So whereâs all the metal those meteorites brought down with them?â
Watching her, he noted with approval the furrowing of her forehead. At least she recognized the paradox there; some heâd talked to hadnât even made it that far. âWell ⦠could the Rooshrike survey data be wrong?â
âThatâs the most likely explanation,â Hafner nodded. âThe problem is that weâve done our own spot checks since then. Our equipment doesnât have their half-kilometer range, but the chunk of rock that dug out Splayfoot Bay ought to have left some of itself scattered through the topsoil.â
âThen maybe the asteroids that hit were just as metal-poor as Astra,â she suggested. âIf the whole system formed from the same cloud of dust ⦠no. Doesnât work, does it?â
âNot when we know the Rooshrike are mining metals on the first planet,â Hafner agreed. âBesides which, some of the smaller asteroids were analyzed by the original survey team and turned out to have a reasonable metal content. No, whatever happened here happened only to Astra.â
They rode in silence for the next few minutes. Ahead, the hazy cone of Mt. Olympus gradually became sharper, the low angle of sunlight showing first the gross and finally the fine structure of its surface. Hafner watched with undivided interest, eyes probing for clues as to the type of lava that had formed it. The steepness of the cone suggested viscous lava flows, which on Earth would mean a predominance of andesitic rock. On the other hand, he could see little evidence of the surface characteristics that usually accompanied that type of lava. Still, if the volcano had been dormant for a long time, erosion would have altered many of the visual reference points. As with everything else in geology, there was ultimately no substitute for physically digging out the rocks and analyzing them.
âWhat about some weird process that breaks the metal down?â Carmen spoke up abruptly. âA nuclear fission sort of thing. Maybe itâs some organismâs way of producing energy.â
âChemical energy is a lot safer to work with,â Hafner grunted. An interesting idea ⦠but the flaw was easy to find. âBesides, that would only get rid of elements in the bottom half of the periodic table. Sodium is far too light a metal to fizz, but Astra hasnât got any of it, either.â
âOh. Wait a minute.â She threw him a puzzled look. âNo sodium either? But I thought Astraâs ocean was salty.â
âNot really. Thereâs a fair assortment of stuff dissolved in it, but none of it strictly qualifies as salt. A salt, you see, is formed by replacing the hydrogen atom in an acid by a metal, as in hydrochloric acid to sodium chloride. Without metals, the acids remain as is or make bonds with oxygen or silicon.â He shook his head. âWeâre sitting on a genuine treasure trove of strange chemistry here. Compounds that wouldnât last five seconds on Earth are just lying around waiting to be examined. I think weâre up to eighteen brand-new carbon compounds alone since weâve landed.â
âAnything valuable?â
âYou mean in terms of sending to Earth? So far, no. But