The ascent of the hill of the citadel is very steep, and we proceeded rather slowly. But there were matters of interest about us. In one place, five hundred feet above the sea, the perpendicular bank on the upper side of the road was ten or fifteen feet high, and the cut exposed three veins of oyster shells, just as we have seen quartz veins exposed in the cutting of a road in Nevada or Montana. The veins were about eighteen inches thick and two or three feet apart, and they slanted along downward for a distance of thirty feet or more, and then disappeared where the cut joined the road. Heaven only knows how far a man might trace them by “stripping.” They were clean, nice oyster shells, large, and just like any other oyster shells. They were thickly massed together, and none were scattered above or below the veins. Each one was a well-defined lead by itself, and without a spur. My first instinct was to set up the usual—
NOTICE:
“We, the undersigned, claim five claims of two hundred feet each, (and one for discovery,) on this ledge or lode of oyster-shells, with all its dips, spurs, angles, variations and sinuosities, and fifty feet on each side of the same, to work it, etc., etc., according to the mining laws of Smyrna.”
They were such perfectly natural-looking leads that I could hardly keep from “taking them up.” Among the oyster-shells were mixed many fragments of ancient, broken crockery ware. Now how did those masses of oyster-shells get there? I can not determine. Broken crockery and oyster-shells are suggestive of restaurants—but then they could have had no such places away up there on that mountain side in our time, because nobody has lived up there. A restaurant would not pay in such a stony, forbidding, desolate place. And besides, there were no champagne corks among the shells. If there ever was a restaurant there, it must have been in Smyrna’s palmy days, when the hills were covered with palaces. I could believe in one restaurant, on those terms; but then how about the three? Did they have restaurants there at three different periods of the world?—because there are two or three feet of solid earth
