According to C. E. Potter of Manchester, New Hampshire, the very word schooner is of New England origin, being from the Indian schoon or scoot, meaning to rush, as Schoodic, from scoot and anke, a place where water rushes. N. B. Somebody of Gloucester was to read a paper on this matter before a genealogical society, in Boston, March 3, 1859, according to the Boston Journal, q. v.
Nearly all who come out must walk on the four planks which I have mentioned, so that you are pretty sure to meet all the inhabitants of Provincetown who come out in the course of a day, provided you keep out yourself. This evening the planks were crowded with mackerel fishers, to whom we gave and from whom we took the wall, as we returned to our hotel. This hotel was kept by a tailor, his shop on the one side of the door, his hotel on the other, and his day seemed to be divided between carving meat and carving broadcloth.
The next morning, though it was still more cold and blustering than the day before, we took to the Deserts again, for we spent our days wholly out of doors, in the sun when there was any, and in the wind which never failed. After threading the shrubby hill country at the southwest end of the town, west of the Shank-Painter Swamp, whose expressive name—for we understood it at first as a landsman naturally would—gave it importance in our eyes, we crossed the sands to the shore south of Race Point and three miles distant, and thence roamed round eastward through the desert to where we had left the sea the evening before. We travelled five or six miles after we got out there, on a curving line, and might have gone nine or ten, over vast platters of pure sand, from the midst of which we could not see a particle of vegetation, excepting the distant thin fields of Beach-grass, which crowned and made the ridges toward which the sand sloped upward on each side;—all the while in the face of a cutting wind as cold as January; indeed, we experienced no weather so cold as this for nearly two months afterward. This desert extends from the extremity of the Cape, through Provincetown into Truro, and many a time as we were traversing it we were reminded of “Riley’s Narrative” of his captivity in the sands of Arabia, notwithstanding the cold. Our eyes magnified the patches of Beach-grass into cornfields in the horizon, and we probably exaggerated the height of the ridges on account of the mirage. I was pleased to learn afterward, from Kalm’s Travels in North America, that the inhabitants of the Lower St. Lawrence call this grass (Calamagrostis arenaria), and also Sea-lyme grass (Elymus arenarius), seigle de me; and he adds, “I have been assured that these plants grow in great plenty in Newfoundland, and on other North American shores; the places covered with them looking, at a distance, like cornfields; which might explain the passage in our northern accounts [he wrote in 1749] of the excellent wine land [Vinland det goda, Translator], which mentions that they had found whole fields of wheat growing wild.”
The Beach-grass is “two to four feet high, of a seagreen color,” and it is said to be widely diffused over the world. In the Hebrides it is used for mats, pack-saddles, bags, hats, etc.; paper has been made of it at Dorchester in this State, and cattle eat it when tender. It has heads somewhat like rye, from six inches to a foot in length, and it is propagated both by roots and seeds. To express its love for sand, some botanists have called it Psamma arenaria, which is the Greek for sand, qualified by the Latin for sandy,—or sandy sand. As it is blown about by the wind, while it is held fast by its roots, it describes myriad circles in the sand as accurately as if they were made by compasses.
It was the dreariest scenery imaginable. The only animals which we saw on the sand at that time were spiders, which are to be found almost everywhere whether on snow or ice-water or sand,—and a venomous-looking, long, narrow worm, one of the myriapods, or thousand-legs. We were surprised to see spider-holes in that flowing sand with an edge as firm as that of a stoned well.
In June this sand was scored with the tracks of turtles both large and small, which had been out in the night, leading to and from the swamps. I was told by a terræ filius who has a “farm” on the edge of the desert, and is familiar with the fame of Provincetown, that one man had caught twenty-five snapping-turtles there the previous spring. His own method of catching them was to put a toad on a mackerel-hook and cast it into a pond, tying the line to a stump or stake on shore. Invariably the turtle when hooked crawled up the line to the stump, and was found waiting there by his captor, however long afterward. He also said that minks, muskrats, foxes, coons, and wild mice were found there, but no squirrels. We heard of sea-turtle as large as a barrel being found on the beach and on East Harbor marsh, but whether they were native there, or had been lost out of some vessel, did not appear. Perhaps they were the Salt-water Terrapin, or else the Smooth Terrapin, found thus far north. Many toads were met with where there was nothing but sand and beach-grass. In Truro I had been surprised at the number of large light-colored toads everywhere hopping over the dry and sandy fields, their color corresponding to that of the sand. Snakes also are common on these pure sand beaches, and I have never been so much troubled by mosquitoes as in such localities. At the same season strawberries grew there abundantly in the little hollows on the edge of the desert standing amid the beach-grass in the sand, and the fruit of the shadbush or Amelanchier, which the inhabitants call Josh-pears (some think from juicy?), is very abundant on the hills. I fell in with an obliging man who conducted me to the best locality for strawberries. He said that he would not have shown me the place if he had not seen that I was a stranger, and could not anticipate him another year; I therefore feel bound in honor not to reveal it. When we came to a pond, he being the native did the honors and carried me over on his shoulders, like Sindbad. One good turn deserves another, and if he ever comes our way I will do as much for him.
In one place we saw numerous dead tops of trees projecting through the otherwise uninterrupted desert, where, as we afterward learned, thirty or forty years before a flourishing forest had stood, and now, as the trees were laid bare from year to year, the inhabitants cut off their tops for fuel.
We saw nobody that day outside of the town; it was too wintry for such as had seen the Back-side before, or for the greater number who never desire to see it, to venture out; and we saw hardly a track to show that any had ever crossed this desert. Yet I was told that some are always out on the Back-side night and day in severe weather, looking for wrecks, in order that they may get the job of discharging the cargo, or the like,—and thus shipwrecked men are succored. But, generally speaking, the inhabitants rarely visit these sands. One who had lived in Provincetown thirty years told me that he had not been through to the north side within that time. Sometimes the natives themselves come near perishing by losing their way in snow-storms behind the town.
The wind was not a Sirocco or Simoon, such as we associate with the desert, but a New England northeaster,—and we sought shelter in vain under the sand-hills, for it blew all about them, rounding them into cones, and was sure to find us out on whichever side we sat. From time to time we lay down and drank at little pools in the sand, filled with pure fresh water, all that was left, probably, of a pond or swamp. The air was filled with dust like snow, and cutting sand which made the face tingle, and we saw what it must be to face it when the weather was drier, and, if possible, windier still,—to face a migrating sand-bar in the air, which has picked up its duds and is off,—to be whipped with a cat, not o’ nine-tails, but of a myriad of tails, and each one a sting to it. A Mr. Whitman, a former minister of Wellfleet, used to write to his inland friends that the blowing sand scratched the windows so that he was obliged to have one new pane set every week, that he might see out.
On the edge of the shrubby woods the sand had the appearance of an inundation which was overwhelming them, terminating in an abrupt bank many feet higher than the surface on which they stood, and having partially buried the outside trees. The moving sand-hills of England, called Dunes or Downs, to which these have been likened, are either formed of sand cast up by the sea, or of sand taken from the land itself in the first place by the wind, and driven still farther inward. It is here a tide of sand impelled by waves and wind, slowly flowing from the sea toward the town. The northeast winds are said to be the strongest, but the northwest to move most sand, because they are the driest. On the shore of the Bay of Biscay many villages were formerly destroyed in this way. Some of the ridges of beach-grass which we saw were planted by government many years ago, to preserve the harbor of Provincetown and the extremity of the Cape. I talked with some who had been employed in the planting. In the “Description of the Eastern Coast,” which I have already referred to, it is said: “Beach-grass during the spring and summer grows about two feet and a half. If surrounded by naked beach, the storms of autumn and winter heap up the sand on all sides, and cause it to rise nearly to the top of the plant. In the ensuing spring the grass mounts anew; is again covered with sand in the winter; and thus a hill or ridge continues to ascend as long as there is a sufficient base to support it, or till the circumscribing sand, being also covered with beach-grass, will no longer yield to the force of the winds.” Sand-hills formed in this way are sometimes one hundred feet high and of every variety of form, like snow-drifts, or Arab tents, and are continually shifting. The grass roots itself very firmly. When I endeavored to pull it up, it usually broke off ten inches or a foot below the surface, at what had been the surface the year before, as appeared by the numerous offshoots there, it being a straight, hard, round shoot, showing by its length how much the sand had accumulated the last year; and sometimes the dead stubs of a previous season were pulled up with it from still deeper in the sand, with their own more decayed shoot attached,—so that the age of a sand-hill, and its rate of increase for several years, is pretty accurately recorded in this way.