SIR WALTER RALEIGH.
SIR WALTER RALEIGH.
SIR WALTER RALEIGH.
Though this map bears a date subsequent to Hudson’s voyage, the contents prove that the original could not have been drawn later than 1608. It was evidently one of the various maps of which Smith spoke and which he underrated. Its substance indicates that it was drawn from a source independent of the Dutch and French, showing that the English knew of the Bay of New York and its relation to Sandy Hook, and that they supposed the great river delineated was a broad stream which, in someway, communicated with the Pacific. On the original map of which Velasco’s example was a copy, the land west of the river was colored blue, and the legend says thatit is described by information drawn from the Indians. What we need now is the original map, which may still exist in some obscure collection in England or Holland, and quite as likely in the archives of Spain, sent thither by jealous Spanish spies, who lingered, like Velasco, at the court of James I., to learn what they could with respect to English enterprise in America. At all events we have in this English map the first seventeenth century delineation of this region, and one showing that the English knew the form and general character of the country which the crown conveyed to the colonists of North and South Virginia in 1606. So far as now known, it was clearly the English who first became acquainted with the name that the Aborigines applied to the island upon which our great metropolitan city stands. Whether or not this was an aboriginal word or a corruption of a Castilian term future investigators may decide. The unexpected finding of this old English map in the Spanish archives revives our hopes relating to the discovery of new sources of information concerning early voyages to this coast. English enterprise and adventure on the Virginia coast, extending from Raleigh’s expedition, 1584, to Gosnold’s fatal quest, 1603, must have brought Englishmen into the Bay of New York, unless miracle was balanced against curiosity and chance. There are archives yet to be opened that may give the origin of the delineations of this region found in the remarkable map from Samancas, and we need to be cautious in making claims even for the priority of the Dutch in 1598.
The period under consideration was a period of reconnoissance, one that offered some romantic incident, but more of disappointment and mortification. Here was a site for one of the noblest cities in the world, but the voyager was blind. The river offered no route to the gorgeous Indies, and Verrazano had little inclination to test its swift tide. Gomez, in the short January days of 1525, had no desire to ascend, for when his ship met the drift ice tossing on the cold, swirling stream, he thought of Anthony in his desolateretreat on the Red Sea, put the river under his charge, and sailed away in search of happier shores. Sailors of other nationalities, doubtless, ascended the river; but, finding it simply a river, they took what peltries they could get, and, like Gomez, turned the whole region over to the care of the solitary Saint, who for nearly a century stood connected with its neglect. Much remained to be done before steps could be taken with regard to colonization. The initial work, however, was inaugurated by the sturdy Englishman, Henry Hudson, and the proud Spanish caravel disappears, while the curtain rises upon the memorable voyage of the quaint Dutch fly-boat, the Half-Moon.
FOOTNOTES[2]Letter addressed to the writer in 1890.[3]The vignette on proceeding page is a faithful representation of the Florentine portrait.[4]The usual course was to sail southward and reach Florida coasting north, or to sail to Newfoundland and coast southward. It required especial boldness to take the direct course, and, in 1562, when Ribault followed this course, he was proud of the achievement. The fact that Verrazano sailed the direct course at that time proves the authenticity of his voyage, as a forger would not have invented the story.[5]On the Map of Verrazano, to which attention will be directed, this triangular island is delineated. The voyager approaching the island from the west comes to a point of the triangle where he can look away in the easterly direction, and at a glance take in two sides; while on reaching the eastern limit the third side plainly appears. In sailing past Block Island, as Verrazano did, from west to east, the navigator could not fail to discover its triangular shape. Indeed it is so marked that one is struck by the fact.[6]The story of this map is curious. The American contents were first given to the public by the writer in the “Magazine of American History,” and afterward reprinted in “Verrazano the Explorer.”[7]In “Cabo de Arenas,” the coast names taken from a large collection of maps are arranged in parallel columns, illustrating three main divisions of the coast, showing that Cabo de Baxos was the name applied to Cape Cod, and Cabo de Arenas to Sandy Hook. Capo Cod in the early times was not a sandy cape, but a beautiful and well-wooded cape. Sandy Hook ever since it was known has borne its present character.[8]Those who have fancied that Cape Arenas was Cape Cod, and that the bay behind it was Massachusetts Bay, have the same difficulty as regards dimensions. Students of American cartography understand perfectly well that latitudes in the old maps were often more than two degrees out of the way, the instruments of that period being so defective.[9]To convince himself of this fact the reader may compare the reconstructed Map of Chaves with the coast surveys, when the main difference will be found to consist in the exaggeration of Sandy Hook. The “Narrative and Critical History of America,” dealing with this point, suppresses all allusion to the fact that Kohl recognizes the cape on the Map of Chaves with the names “Santiago” and “Arenas” as Sandy Hook, which follows, as the river inside of the Hook he identifies with the Hudson. Dr. Kohl, though generally very acute, failed to see that Oviedo’s description of the Map of Chaves was, substantially, the description of Ribeiro, and that in identifying, as he chanced to, the “Arenas” of Ribeiro with Cape Cod, he stultified his own reasoning. Nor did he consider this, that if the great Cape “Arenas” was intended for Cape Cod, there is no representation whatever of Sandy Hook and the Hudson in the old cartography and that all the voyages to this region geographically went for nothing.Credat Judaeus Appellus!This exaggeration of Sandy Hook is conceded, yet the inlets along the New Jersey shore may have been viewed as connected by Gomez; and indeed, so great have been the changes along the coast that no one can well deny that they were connected in 1525, and formed a long bay running down behind Sandy Hook. It will prove more historic to follow the writer, who says, “that the coast of New York and the neighboring district were known to Europeans almost a century before Hudson ascended the ‘Great River of the North,’ and that this knowledge is proved by various maps made in the course of the sixteenth century. Nearly all of them place the mouth of a river between the fortieth and forty-first degrees of latitude, or what should be this latitude, but which imperfect instruments have placed farther north.”—Nar. and Crit. His. of Amer., 4: 432.
[2]Letter addressed to the writer in 1890.
[2]Letter addressed to the writer in 1890.
[3]The vignette on proceeding page is a faithful representation of the Florentine portrait.
[3]The vignette on proceeding page is a faithful representation of the Florentine portrait.
[4]The usual course was to sail southward and reach Florida coasting north, or to sail to Newfoundland and coast southward. It required especial boldness to take the direct course, and, in 1562, when Ribault followed this course, he was proud of the achievement. The fact that Verrazano sailed the direct course at that time proves the authenticity of his voyage, as a forger would not have invented the story.
[4]The usual course was to sail southward and reach Florida coasting north, or to sail to Newfoundland and coast southward. It required especial boldness to take the direct course, and, in 1562, when Ribault followed this course, he was proud of the achievement. The fact that Verrazano sailed the direct course at that time proves the authenticity of his voyage, as a forger would not have invented the story.
[5]On the Map of Verrazano, to which attention will be directed, this triangular island is delineated. The voyager approaching the island from the west comes to a point of the triangle where he can look away in the easterly direction, and at a glance take in two sides; while on reaching the eastern limit the third side plainly appears. In sailing past Block Island, as Verrazano did, from west to east, the navigator could not fail to discover its triangular shape. Indeed it is so marked that one is struck by the fact.
[5]On the Map of Verrazano, to which attention will be directed, this triangular island is delineated. The voyager approaching the island from the west comes to a point of the triangle where he can look away in the easterly direction, and at a glance take in two sides; while on reaching the eastern limit the third side plainly appears. In sailing past Block Island, as Verrazano did, from west to east, the navigator could not fail to discover its triangular shape. Indeed it is so marked that one is struck by the fact.
[6]The story of this map is curious. The American contents were first given to the public by the writer in the “Magazine of American History,” and afterward reprinted in “Verrazano the Explorer.”
[6]The story of this map is curious. The American contents were first given to the public by the writer in the “Magazine of American History,” and afterward reprinted in “Verrazano the Explorer.”
[7]In “Cabo de Arenas,” the coast names taken from a large collection of maps are arranged in parallel columns, illustrating three main divisions of the coast, showing that Cabo de Baxos was the name applied to Cape Cod, and Cabo de Arenas to Sandy Hook. Capo Cod in the early times was not a sandy cape, but a beautiful and well-wooded cape. Sandy Hook ever since it was known has borne its present character.
[7]In “Cabo de Arenas,” the coast names taken from a large collection of maps are arranged in parallel columns, illustrating three main divisions of the coast, showing that Cabo de Baxos was the name applied to Cape Cod, and Cabo de Arenas to Sandy Hook. Capo Cod in the early times was not a sandy cape, but a beautiful and well-wooded cape. Sandy Hook ever since it was known has borne its present character.
[8]Those who have fancied that Cape Arenas was Cape Cod, and that the bay behind it was Massachusetts Bay, have the same difficulty as regards dimensions. Students of American cartography understand perfectly well that latitudes in the old maps were often more than two degrees out of the way, the instruments of that period being so defective.
[8]Those who have fancied that Cape Arenas was Cape Cod, and that the bay behind it was Massachusetts Bay, have the same difficulty as regards dimensions. Students of American cartography understand perfectly well that latitudes in the old maps were often more than two degrees out of the way, the instruments of that period being so defective.
[9]To convince himself of this fact the reader may compare the reconstructed Map of Chaves with the coast surveys, when the main difference will be found to consist in the exaggeration of Sandy Hook. The “Narrative and Critical History of America,” dealing with this point, suppresses all allusion to the fact that Kohl recognizes the cape on the Map of Chaves with the names “Santiago” and “Arenas” as Sandy Hook, which follows, as the river inside of the Hook he identifies with the Hudson. Dr. Kohl, though generally very acute, failed to see that Oviedo’s description of the Map of Chaves was, substantially, the description of Ribeiro, and that in identifying, as he chanced to, the “Arenas” of Ribeiro with Cape Cod, he stultified his own reasoning. Nor did he consider this, that if the great Cape “Arenas” was intended for Cape Cod, there is no representation whatever of Sandy Hook and the Hudson in the old cartography and that all the voyages to this region geographically went for nothing.Credat Judaeus Appellus!This exaggeration of Sandy Hook is conceded, yet the inlets along the New Jersey shore may have been viewed as connected by Gomez; and indeed, so great have been the changes along the coast that no one can well deny that they were connected in 1525, and formed a long bay running down behind Sandy Hook. It will prove more historic to follow the writer, who says, “that the coast of New York and the neighboring district were known to Europeans almost a century before Hudson ascended the ‘Great River of the North,’ and that this knowledge is proved by various maps made in the course of the sixteenth century. Nearly all of them place the mouth of a river between the fortieth and forty-first degrees of latitude, or what should be this latitude, but which imperfect instruments have placed farther north.”—Nar. and Crit. His. of Amer., 4: 432.
[9]To convince himself of this fact the reader may compare the reconstructed Map of Chaves with the coast surveys, when the main difference will be found to consist in the exaggeration of Sandy Hook. The “Narrative and Critical History of America,” dealing with this point, suppresses all allusion to the fact that Kohl recognizes the cape on the Map of Chaves with the names “Santiago” and “Arenas” as Sandy Hook, which follows, as the river inside of the Hook he identifies with the Hudson. Dr. Kohl, though generally very acute, failed to see that Oviedo’s description of the Map of Chaves was, substantially, the description of Ribeiro, and that in identifying, as he chanced to, the “Arenas” of Ribeiro with Cape Cod, he stultified his own reasoning. Nor did he consider this, that if the great Cape “Arenas” was intended for Cape Cod, there is no representation whatever of Sandy Hook and the Hudson in the old cartography and that all the voyages to this region geographically went for nothing.Credat Judaeus Appellus!This exaggeration of Sandy Hook is conceded, yet the inlets along the New Jersey shore may have been viewed as connected by Gomez; and indeed, so great have been the changes along the coast that no one can well deny that they were connected in 1525, and formed a long bay running down behind Sandy Hook. It will prove more historic to follow the writer, who says, “that the coast of New York and the neighboring district were known to Europeans almost a century before Hudson ascended the ‘Great River of the North,’ and that this knowledge is proved by various maps made in the course of the sixteenth century. Nearly all of them place the mouth of a river between the fortieth and forty-first degrees of latitude, or what should be this latitude, but which imperfect instruments have placed farther north.”—Nar. and Crit. His. of Amer., 4: 432.