Fishing Grounds of the Gulf of Maine | Page 4

thousands of safe harbors and havens for the navigator. All along shore
are strewn hundreds of islands, a characteristic feature of the region and
one noted with wonder by every early explorer. [6] These islands, if
near the land, are beautiful and smiling; if in the open sea, of rugged
grandeur; and mainland and island alike are inhabited 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