rises to the height of two hundred, and sometimes perhaps three hundred feet above the level of the sea. According to Hitchcock, the geologist of the State, it is composed almost entirely of sand, even to the depth of three hundred feet in some places, though there is probably a concealed core of rock a little beneath the surface, and it is of diluvian origin, excepting a small portion at the extremity and elsewhere along the shores, which is alluvial. For the first half of the Cape large blocks of stone are found, here and there, mixed with the sand, but for the last thirty miles boulders, or even gravel, are rarely met with. Hitchcock conjectures that the ocean has, in course of time, eaten out Boston Harbor and other bays in the mainland, and that the minute fragments have been deposited by the currents at a distance from the shore, and formed this sand-bank. Above the sand, if the surface is subjected to agricultural tests, there is found to be a thin layer of soil gradually diminishing from Barnstable to Truro, where it ceases; but there are many holes and rents in this weather-beaten garment not likely to be stitched in time, which reveal the naked flesh of the Cape, and its extremity is completely bare.
I at once got out my book, the eighth volume of the Collections of the Massachusetts Historical Society, printed in 1802, which contains some short notices of the Cape towns, and began to read up to where I was, for in the cars I could not read as fast as I travelled. To those who came from the side of Plymouth, it said: "After riding through a body of woods, twelve miles in extent, interspersed with but few houses, the settlement of Sandwich appears, with a more agreeable effect, to the eye of the traveller." Another writer speaks of this
