Fishing Grounds of the Gulf of Maine Part 1

Fis.h.i.+ng Grounds of the Gulf of Maine.

by Walter H. Rich.

PREFACE TO THE 1994 EDITION

Fis.h.i.+ng Grounds of the Gulf of Maine by Walter H. Rich first appeared in the U.S. Department of Commerce, Bureau of Fisheries, Report of the United States Commissioner of Fisheries, for the fiscal year 1929.

When Captain Robert McLellan of Boothbay Harbor died in 1981, the employees of the Maine Department of Marine Resources contributed money to be used to purchase books in his memory, for the Department's Fishermen's Library. Captain McLellan's family was asked what purchases they would recommend, and a top priority was to somehow reprint this work on the fis.h.i.+ng grounds. This was a book that had been helpful to Captain McLellan in his career, and one which his son, Captain Richard McLellan, found still valid and useful.

Contributions from the employees of the Department of Marine Resources paid to get this project started; film to reproduce the pages of the original text was donated by the Bigelow Laboratory for Ocean Sciences; printing costs were paid by the Department.

It is the hope of the Department and its employees that the fishermen of today will benefit from the detailed information in this publication, and that they will remember Captain Robert McLellan, a man who knew how to use books to enhance his career as a fisherman, who knew how to share his knowledge with the scientific community, and who was widely respected by fishermen and scientists alike.

INTRODUCTION

Paralleling the northeastern coast line of North America lies a long chain of fis.h.i.+ng banks--a series of plateaus and ridges rising from the ocean bed to make comparatively shallow soundings. From very early times these grounds have been known to and visited by the adventurers of the nations of western Europe--Northman, Breton, Basque, Portuguese, Spaniard, Frenchman, and Englishman. For centuries these fis.h.i.+ng areas have played a large part in feeding the nations bordering upon the Western Ocean, and the development of their resources has been a great factor in the exploration of the New World.

According to statistics collected by the Bureau of Fisheries.[2] these banks annually produce over 400,000,000 pounds of fishery products, which are landed in the United States; and, according to O. E. Sette,[3]

annually about 1,000,000,000 pounds of cod are taken on these banks and landed in the United States, Canada, Newfoundland, France, and Portugal.

Apparently the earliest known and certainly the most extensive of these is the Great Bank of Newfoundland, so named from time immemorial. From the Flemish Cap, in 44 06' west longitude and 47 north lat.i.tude, marking the easternmost point of this great area, extends the Grand Bank westward and southwestward over about 600 miles of length. Thence, other grounds continue the chain, pa.s.sing along through the Green Bank, St.

Peters Bank, Western Bank (made up of several more or less connected grounds, such as Misaine Bank, Banquereau, The Gully, and Sable Island Bank); thence southwest through Emerald Bank, Sambro, Roseway, La Have, Seal Island Ground, Browns Bank, and Georges Bank with its southwestern extension of Nantucket Shoals.

To all these is added the long shelving area extending from the coast out to the edge of the continental plateau and stretching from the South Shoal off Nantucket to New York, making in all, from the eastern part of the Grand Bank to New York Bay, a distance of about 2,000 miles, an almost continuous extent of most productive fis.h.i.+ng ground.

Within the bowl that is the Gulf of Maine, the outer margin of which is made by the shoaling of the water over the Seal Island Grounds, Browns Bank, and Georges Bank, this chain is further extended by another series of smaller grounds, as Grand Manan Bank, the German Bank, Jeffreys Bank, Cashes Bank, Platts Bank, Jeffreys Ledge, Fippenies Bank, Stellwagen or Middle Bank; and again, lying inside these, this fis.h.i.+ng area is increased by a very large number of smaller grounds and fis.h.i.+ng spots located within a very short distance of the mainland.

All these banks are breeding places of the most valued of our food fishes--the cod, haddock, cusk, hake, pollock, and halibut--and each in its proper season furnishes fis.h.i.+ng ground where are taken many other important species of migratory and pelagic food fishes as well as those named here. It is probable that no other fis.h.i.+ng area equaling this in size or in productivity exists anywhere else in the world, and the figures of the total catch taken from it must show an enormous poundage and a most imposing sum representing the value of its fishery.

With the most distant of these grounds we shall not deal here, leaving them for later consideration when noting certain of the fishery operations most characteristic of them. Thus, we may treat of those well-defined areas that lie within or are adjacent to the Gulf of Maine, such as the Bay of Fundy, the Inner Grounds (those close to the mainland), the Outer Grounds (those within the gulf), the Georges area, Seal Island Grounds, and Browns Bank, these forming the outer margin of the gulf; and also make mention of certain others of those nearer offsh.o.r.e banks that are most closely connected with the market fishery of the three princ.i.p.al fis.h.i.+ng ports within the Gulf of Maine.

[Footnote 1: First published as Appendix III to the Report of the US Commissioner of Fisheries for 1929. Bureau of Fisheries Doc# 1059.

Submitted for publication Jan 18,1929.]

[Footnote 2: U.S. Bureau of Fisheries Statistical Bulletin No. 703]

[Footnote 3: U.S. Bureau of Fisheries Doc.u.ment No. 1034]

ACKNOWLEDGMENTS

As to the charts, it has been the writer's endeavor, by consulting a large number of fis.h.i.+ng captains of long experience upon these grounds, to reduce the margin of inaccuracy as much as possible. In case of conflict of their opinion, the greatest agreement as to the facts has been accepted.

The grounds as drawn are not meant to include any definite depth curve but are meant to show certain fis.h.i.+ng areas. It is known of course, that most species frequent the shallows and the deep water at the various seasons: also, that certain other species are found on the deeper soundings during virtually all the year. Thus, if a given area appears as a larger ground than is shown upon other charts made for navigating purposes, often this is because we have included in it a cusk ground or a hake bottom lying adjacent to the shoal as charted.

A large number of these grounds have been described before by G. Browne Goode and others, and where possible their work has been used as a basis for the present paper, with any further information or the noting of any changed condition of the grounds or difference in fis.h.i.+ng methods employed upon them that was obtainable.

Grateful acknowledgment is hereby made to the many captains who furnished information that, made the drawing of the charts possible and for the facts used in the descriptions of the fis.h.i.+ng grounds.

With the offsh.o.r.e banks, particularly with the Georges area and Browns Bank and to a certain extent, also, the western portion of the Inner Grounds, the writer has had a considerable personal acquaintance from which to draw.

For the geographical and historical data the writer has quoted freely from various modern authors, who, in their turn, have drawn their facts from older records. Among those quoted are Holmes's American Annals; Parkman's Pioneers of France in the New World; Southgates History of Scarburo; Abbott and Elwell's History of Maine; Willis's History of Maine; Sabine's Report on the Princ.i.p.al Fisheries of the American Seas; A History of the Discovery of the East Coast of North America, by Dr.

John G. Kohl, of Bremen, Germany; various chapters of Hakluyt's Voyages; the Journal of John Jocelyn, Gent.; and New England Trials of the famous Captain John Smith.

GULF OF MAINE--GEOGRAPHICAL & HISTORICAL NAME

What is apparently the earliest mention of this body of water appears on some old Icelandic charts that show, roughly, Cape Cod Bay in their southern areas and the Bay of Fundy in the northern. On these maps the cape itself was shown on the "Promontory of Vinland" and was given the name Kialarnes, or the s.h.i.+p's Nose, from its resemblance in form to the high upturned prow of the old Norse s.h.i.+ps. To the entire area of the gulf was given the t.i.tle Vinland's Haf.

Oviedo (Historia General de las Indias) sometimes names this gulf the Arcipelago de La Tramontana, or the Arcipelago Septentrional--the northern archipelago. He gives us to understand that he, himself, or Chaves, had this information from the Report and Survey of Gomez, who, in his search for a northwest pa.s.sage to Asia in 1525, "discovered all these coasts lying between 41 and 41 30' north". As a matter of fact, his careful explorations certainly covered all the territory between 40 and 45 degrees.

The Spanish navigators who followed Gomez, in describing these coasts, when indicating this gulf, usually named it in honor of Gomez, the first of their nation to make a careful survey of its sh.o.r.es. Thus it became known as the Arcipelago de Estevan Gomez, and the mainland behind it as La Tierra de Gomez. It was so named on the map of Ribero in 1529 who thus acknowledged the source of his information.

The Biscayans followed Gomez but later gave way to the French fishermen, who followed down the chain of banks extending southward from the Grand Bank and entered these waters by way of Cape Sable. These gave to it the name Gulf of Norumbega or Sea of Norumbega. The name Norumbega was for a time applied to the coast lands and to the inland country stretching away indefinitely westward and northwestward from the waters of the gulf.

Later, with the coming of the English and the establishment of their colony in Ma.s.sachusetts, the t.i.tle Ma.s.sachusetts Bay came into general use, although this name was afterwards restricted to the smaller section of the gulf at present so termed.

The charter of Gorges (in April, 1639) designated the territory deeded to him as the Province or County of Maine,[4] whence, perhaps, the modern custom of referring to these waters as the Gulf of Maine may have arisen. This latest name seems especially appropriate, in view of the fact that the present State of Maine lying directly opposite its entrance capes, stretches along the inner borders of the gulf and with its deeply indented sh.o.r.e line occupies by far the greatest section of its coasts. Thus the t.i.tle has finally come into general use and acceptance in modern times. Apparently it was first officially proposed and used by the Edinburgh Encyclopedia in 1832 [5] and later was adopted by the United States Coast Survey.

[Footnote 4: "All that parte, purport and porcion of the Mayne Land of New England, we doe name, ordeyne and appoynt shall forever hereafter bee called and named The Province and Countie of Mayne."]

[Footnote 5: Edinburgh Encyclopedia, Philadelphia edition, by Thomas Parker, Vol. XVIII, p. 263.]

DESCRIPTION

A very striking and peculiar body of water is this Gulf of Maine, markedly different in character from any other of the bays on the coast line of the eastern United States. Especially does it differ in the depth of its coastal waters, where in all the others, except the much smaller New York Bay, the shoal water is found extending far out from the land.

In the Gulf of Maine, however, with the single exception of the vicinity of Ammens Rock on the eastern part of Cashes Bank, the entire central area presents navigable deep water having a mean depth of 100 fathoms, out of which rise the various underwater plateaus, whose depths average about 50 fathoms and which const.i.tute the larger of the fis.h.i.+ng grounds.

In addition to these, many smaller banks and "fis.h.i.+ng spots" are found nearer the land where they lie a along the 50-fathom curve.

In general this curve lies at a distance of about 16 miles from the coast line, but in many instances it approaches much neared to the mainland. From this 50-fathom depth the soundings decrease very gradually to the 20 and 10 fathom marks.

These latter soundings are often held far in toward the coast line, even carrying the deep water well into the river mouths, so that in deeply indented hays, in long inlets running far into land, in the river mouths, the deep water behind the rocky headlands, or in the lee of the thousands of surf-washed islands that line the coast, are found innumerable safe anchorages within easy run of the fis.h.i.+ng grounds, where the fleets may take shelter from a sudden blow or await the arrival of a "fish day," when conditions may permit "making a set" under the hards.h.i.+ps of winter fis.h.i.+ng.

If the marine features of this region are radically different from those of other coastal bodies of the eastern United States, so, too, the sh.o.r.e land, battered as it has been by sea and storm or worn by glacial action or Arctic currents, is no less remarkable.