Note 74 — PETER KALM’s TRAVELS. (continued 2)

This country being low, and situated upon a bay of the river, it may be conjectured, that this flat ground was formerly part of the bottom of the river, and formed itself, either by a decrease of water in the river, or by an encrease of earth, which was carried upon it from the continent by the brooks, or thrown on it by storms. A great part of the plants, which are to be met with here, are likewise marine; such as glass-wort, sea milk-wort, and sea-side pease74. But when I have asked the inhabitants, whether they find shells in the ground by digging for wells, they always answered in the negative. I received the same answer from those who live in the low fields directly north of Quebec, and all agreed, that they never found any thing by digging, but different kinds of earth and sand.