"By the way," said Gazen to me, "I've got a new theory for the rising and sinking of the sun behind the cliffs at Womla—a theory that will simply explode Professor Possil, and shake the Royal Astronomical Society to its foundations."

The astronomer and I were together in the observatory, where he was adjusting his telescope to look at the sun. After our misadventure with the flying ape, we had returned to our former station on the summit of the mountain, to pick up the drawing materials of Miss Carmichael; but as Gazen was anxious to get as near the sun as possible, and being disgusted with the infernal scenery as well as the foetid, malarial atmosphere of Mercury, we left as soon as we had replenished our cistern from the pools in the rock.

"Another theory?" I responded. "Thought you had settled that question."

"Alas, my friend, theories, like political treatises, are made to be broken."

"Well, what do you think of it now?"

"You remember how we came to the conclusion that Schiaparelli was right, and that the planet Venus, by rotating about her own axis in the same time as she takes to revolve around the sun, always keeps the same face turned to the sun, one hemisphere being in perpetual light and summer, whilst the other is in perpetual darkness and winter?"

"Yes."

"You remember, too, how we explained the growing altitude of the sun in the heavens which culminated on the great day of the Festival, by supposing that the axis of the planet swayed to and from the sun so as to tilt each pole towards the sun, and the other from it, alternately, thus producing what by courtesy we may call the seasons in Womla?"

"Yes."

"Well, judging from the observations I have made, we were probably right so far; but if you recollect, I accounted for the mysterious daily rise and set of the sun, if I may use the words, by changes in the density of the atmosphere bending the solar rays, and making the disk appear to rise and sink periodically, though in reality it does nothing of the kind. A similar effect is well-known on the earth. It produces the 'after glow' on the peaks of the Alps when the sun is far below the horizon; it sometimes makes the sun bob up and down again after sunset, and it has been known to make the sun show in the Arctic regions three weeks before the proper time. I had some difficulty in understanding how the effect could take place so regularly."