Page:Cape Cod (1865) Thoreau.djvu/46

between Orleans and Eastham, called Jeremiah's Gutter. The Atlantic is said sometimes to meet the Bay here, and isolate the northern part of the Cape. The streams of the Cape are necessarily formed on a minute scale, since there is no room for them to run, without tumbling immediately into the sea; and beside, we found it difficult to run ourselves in that sand, when there was no want of room. Hence, the least channel where water runs, or may run, is important, and is dignified with a name. We read that there is no running water in Chatham, which is the next town. The barren aspect of the land would hardly be believed if described. It was such soil, or rather land, as, to judge from appearances, no farmer in the interior would think of cultivating, or even fencing. Generally, the ploughed fields of the Cape look white and yellow, like a mixture of salt and Indian meal. This is called soil. All an inlander's notions of soil and fertility will be confounded by a visit to these parts, and he will not be able, for some time afterward, to distinguish soil from sand. The historian of Chatham says of a part of that town, which has been gained from the sea: "There is a doubtful appearance of a soil beginning to be formed. It is styled doubtful, because it would not be observed by every eye, and perhaps not acknowledged by many." We thought that this would not be a bad description of the greater part of the Cape. There is a "beach" on the west side of Eastham, which we crossed the next summer, half a mile wide, and stretching across the township, containing seventeen hundred acres, on which there is not now a particle of vegetable mould, though it formerly produced wheat. All sands are here called "beaches," whether they are waves of water or of air, that dash against