interior lamps so they glowed green, yellow and blue; it was a relief to be immersed once more in bright Earth light.
We set off in our gondola-truck for the next part of our expedition. We were making, I was told, for an impact crater believed to hold liquid water, which itself was not far from a cryovolcano, another feature of interest for the expedition. This site was perhaps a hundred kilometres from where we had come down.
Miriam transferred her lake samples to cold stores, and ran some of them through a small onboard science package. She jabbered about what she had discovered. Poole encouraged her more than Dzik did, but even that wasn’t much. Dzik and Poole were more interested at that moment in playing with the gondola. They sat at an improvised driver’s console and fussed over gear ratios and the performance of the big tyres. Poole even insisted on driving the bus himself, though Titan was so flat and dull for the most part he could easily have left the chore to the onboard systems. That proved to me the fallacy of not bringing along specialist biologists on a jaunt like this. It was only Miriam who seemed to have a genuine passion for the life systems we were supposed to be here to study; Dzik and Poole were too easily distracted by the technology, which was, after all, only a means to an end.
They had, however, rearranged the interior to make it feel a little less cramped. The couches had been separated and set up around the cabin, so you could sit upright with a bit of elbow room. The cabin was pressurised so we could remove our helmets, and though the expandable walls didn’t work any more there was room for one at a time to shuck off his or her exosuit. Poole ordered us to do so; we had already been inside the suits for a few hours, and the suits, and ourselves, needed some down time. Poole had set up a curtained-off area where we could let our discarded suits perform their self-maintenance functions while we had showers – of water recycled from our urine and sweat, which was deemed a lot safer than melt from the ice moon. Poole himself used the shower first, and then Miriam. She was hasty, eager to get back to her work, and kept talking even while she cleaned up.
After Miriam was out of the shower I took my turn. It was a miserable drizzle and lukewarm at that, but it was a relief to let my skin drink in the water. I was quick, though; with the unknown dangers of Titan only centimetres away beyond the gondola’s fragile metal walls, I didn’t want to spend long outside the security of the suit.
It was scarcely a comfortable ride, even discounting the calculating face of Harry Poole glaring from wall-mounted slates. I was relieved when, after a couple of hours, we reached our destination.
At that point Bill Dzik was in the shower. Safely suited up, with Dzik’s offensive presence absent, I was able to sit forward in my couch and peer over Miriam’s and Poole’s shoulders at the landscape outside. That cryovolcano was a mound that pushed out of the landscape some kilometres to the west of us. It had the look of a shield volcano, like Hawaii or Mons Olympus, a flat-profiled dome with a caldera on the top. It wasn’t erupting while we sat there, but I could see how successive sheets of ‘lava’ had plated its sides. That lava was water ice, heavily laced with ammonia, which had come gushing up from this world’s strange mantle, a sea of liquid water locked under the ice, kilometres below our tyres.
As for the crater lake, I saw nothing but a plain, flatter and even more featureless than the average, covered with a thin scattering of ice sand. But the lake was there, hidden. Poole extracted radar images which showed the unmistakable profile of an impact crater, directly ahead of us, kilometres wide. Such is the vast energy pulse delivered by an infalling asteroid or comet – or, in Saturn’s system, perhaps a ring fragment or a bit of a tide-shattered moon – that the water locally can