Jeffreys Bank, Cashes Bank, Platts Bank, Jeffreys Ledge, Fippenies Bank, Stellwagen or Middle Bank; and again, lying inside these, this fishing area is increased by a very large number of smaller grounds and fishing 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 fishing 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 fishing 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 offshore banks that are most closely connected with the market fishery of the three principal fishing ports within the Gulf of Maine.

As to the charts, it has been the writer's endeavor, by consulting a large number of fishing 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 fishing 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 fishing 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 fishing grounds.

With the offshore 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 Principal 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.

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 Ship's Nose, from its resemblance in form to the high upturned prow of the old Norse ships. To the entire area of the gulf was given the title 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 passage 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 shores. 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 Massachusetts, the title Massachusetts 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 shore line occupies by far the greatest section of its coasts. Thus the title 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.

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 constitute the larger of the fishing grounds. In addition to these, many