supposed, therefore, they must be fragments of millstones, or of pieces brought from a distance for some such use. Near Monte Allegro, the stone is all gypsum and selenite,—whole rocks of these occurring before and between the limestone. The wonderful strata of Bellota!
Girengti,
Tuesday, April 24, 1787.
Such a glorious spring view as we enjoyed at sunset to-day will most assuredly never meet our eyes again in one lifetime. Modern Girgenti stands on the lofty site of the ancient fortifications, an extent sufficient for the present population. From our window, we looked over the broad but gentle declivity on which stood the ancient town, which is now entirely covered with gardens and vineyards, beneath whose verdure it would be long before one thought of looking for the quarters of an ancient city. However, toward the southern end of this green and flourishing spot the Temple of Concord rears itself, while on the east are a few remains of the Temple of Juno. Other ruins of some ancient buildings, which, lying in a straight line with those already spoken of, are scarcely noticed by the eye from above, while it hurries over them southwards to the shore, or ranges over the level country, which reaches at least seven miles from the sea-mark. To-day we were obliged to deny ourselves the pleasure of a stroll among the trees and wild rockets, and over this expanse so green, so flourishing, and so full of promise for the husbandman, because our guide (a good-natured little parish priest) begged of us above all things to devote this day to the town.
He first showed us the well-built streets; then he took us to the higher points, from which the view, gaining both in extent and breadth, was still more glorious; and lastly, for an artistic treat, conducted us to the principal church. In it there is an ancient sar-
