Fishing Grounds of the Gulf of Maine | Page 4

by a numerous and hardy race of fisher folk.
The tides within the Gulf of Maine have a very great rise and fall as compared with other waters in this region. At the south of Cape Cod tides are seldom over 4 feet in their range, but beginning at once at the north of Cape Cod with a rise of from 7 to 10 feet these increase quite constantly as they go eastward reaching about 28 feet in the neighborhood of Passamaquoddy Bay, to touch their highest point in the Bay of Fundy, where in many places is a rise and fall of 50 feet, and in some few places tides of 70 feet are reported. These Fundy tides probably are the greatest in the world.
This great ebb and flow of water serves to aid shipbuilding and the launching of vessels as well as to carry the deep water far up into the inlets of the coast and into the mouths of the rivers, making these navigable for crafts of considerable size well into the land or up to the lowest falls of the streams.
The climate here is one of extremes, and, lying as it does between 42�� and 45�� north latitude, the region may be said to be cold. Apparently the waters of the Gulf of Maine are not affected by any stray current from the Gulf Stream, which passes at a considerable distance from its mouth, thus doing little to temper the cold of this area either on land or at sea. Whether these waters are cooled further by any flow from the Labrador Current may be questioned.
The winters are long, usually bringing heavy snowfalls; and strong gales are frequent during much of the fall and winter season. Perhaps the most dangerous of these "blows" come out of the mountain to the north and northwest of the gulf. Thus, in addition to the uncertainty of an opportunity to set gear when once upon the fishing grounds, the winter fishing here is not without its element of serious danger. While the ice crop in northern New England never fails, yet, perhaps because of the strong tidal currents of these waters, the principal harbors rarely are closed by ice, or, if closed, for but a few days only.
While the summers are fairly mild and in certain parts of them even extremely hot, fogs are heavy and virtually continuous during the "dog days" (July 20 to September 1). when southerly and south-westerly breezes bring the warm moist air from the Gulf Stream into the cooler currents from the land. The fogs of Fundy are especially noted, even in these waters. During the summer seasons winds from the east and north bring the only clear weather experienced in the outer chain of fishing grounds.
The main body of the gulf lies approximately between 42�� and 45�� north latitude. It is in form like a deep bowl whose outer rim is made by Georges Bank and Browns Bank, with a narrow, deep-water spillway between: its area is half encircled in the arms of the mainland, two conspicuous headlands reaching bodily seaward to mark its wide entrance at the opposite sides--Cape Cod, Mass. [7] on the western side, and Cape Sable, [8] Nova Scotia, on the eastern flank, distant from each other about 230 miles. These two capes range with each other about ENE. and WSW, thus matching alike the general trend of the coast line, of the island chains and of the offshore ledges within this area.
From a base line connecting these outposts of the gulf the distance to the Maine coast opposite averages about 120 miles. From Cape Sable, at its eastern end, the coast trends for some distance to the northwest, whence a continuation of this course strikes the coast of Maine near West Quoddy Head at a distance of rather more than 110 miles. From West Quoddy head to Cape Elizabeth (in a direct line about 160 miles) the coast, in general rough, rocky, and with many lofty headlands is extremely irregular and deeply indented and follows a general course of WSW. Thence, the coast, lower and becoming more and more sandy, begins to trend more decidedly south-west until it reaches Boston, when it turns to the southeast, and to the east toward Cape Cod.
But this is not the entire story. There remain outside of these stated limits the Bay of Fundy in the north, with a possible area of 3,000 square miles; and at the south Cape Cod Bay, whose area, with that of the waters west of a perpendicular drawn from the western end of the base line that strikes the land in the vicinity of Portsmouth, N. H. makes an additional section containing close to 1,500 square miles. Within the limits thus inclosed there are, roughly, 30,000 square miles