CHAPTER III.

Bradford’s Account of the Wreck.—His Visit to the Scene of the Disaster.—The Passengers and Crew received at Plymouth.—Tradition of the Name “Sparrow-Hawk.”—Extracts from the Work of Amos Otis, Esq.—Recovery and Saving of the Wreck.

E now proceed to give the history of the ancient ship according to the chronological order of events. The reader’s attention is invited to the following interesting and important extract from “Bradford’s History of Plymouth Plantations, A. D. 1626–7,” MS. p. 146:⁠—

“Ther is one thing that fell out in y^e begining of y^e winter before, which I have refferred to this place, that I may handle y^e whole matter togeither. Ther was a ship, with many passengers in her and sundrie goods, bound for Virginia. They had lost them selves at sea, either by y^e insufficiencie of y^e maister, or his ilnes; for he was sick & lame of y^e scurvie, so that he could but lye in y^e cabin dore & give direction; and it should seeme was badly assisted either w^th mate or mariners; or else y^e fear and unrulines of y^e passengers were such, as they made them stear a course betweene y^e southwest & y^e norwest, that they might fall with some land, what soever it was they cared not. For they had been 6. weeks at sea, and had no water, nor beere, nor any woode left, but had burnt up all their emptie caske; only one of y^e company had a hogshead of wine or 2. which was allso allmost spente, so as they feared they should be starved at sea, or consumed with diseases, which made them rune this desperate course. But it plased God that though they came so neare y^e shoulds of Cap-Codd [147] or else ran stumbling over them in y^e night, they knew not how, they came right before a small blind harbore that lyes aboute y^e midle of Manamoyake Bay to y^e Southward of Cap-Codd, with a small gale of wind; and about highwater toucht upon a barr of sand that lyes before it, but had no hurte, y^e sea being smoth; so they laid out an anchore. But towards the evēing, the winde sprunge up at sea, and was so rough, as broake their cable, & beat them over the barr into y^e harbor, wher they saved their lives & goods, though much were hurte with salt water; for w^th beating they had sprung y^e but end of a planke or too, & beat out their occome; but they were soone over, and ran on a drie slate within the harbor, close by a beach; so at low water they gatt out their goods on drie shore, and dried those that were wette, and saved most of their things without any great loss; neither was y^e ship much hurt, but shee might be mended, and made servisable againe. But though they were not a litle glad that they had thus saved their lives, yet when they had a litle refreshed them selves, and begane to thinke on their condition, not knowing wher they were, nor what they should doe, they begane to be strucken with sadnes. But shortly after they saw some Indians come to them in canows, which made them stand upon their gard. But when they heard some of y^e Indeans speake English unto them, they were not a litle revived, especially when they heard them demand if they were the Gove^r of Plimoths men, or freinds; and y^t they would bring them to y^e English houses, or carry their letters.

“They feasted these Indeans, and gave them many giftes; and sente 2. men and a letter with them to y^e Gove^r, and did intreat him to send a boat unto them, with some pitch, & occume, and spiks, w^th divers other necessaries for y^e mending of ther ship (which was recoverable). Allso they besought him to help them with some corne and sundrie other things they wanted, to enable them to make their viage to Virginia; and they should be much bound to him, and would make satisfaction for any thing they had, in any comodities they had abord. After y^e Gov^r was well informed by y^e messengers of their condition, he caused a boate to be made ready, and such things to be provided as they write for; and because others were abroad upon trading, and such other affairs, as had been fitte to send unto them, he went him selfe, & allso carried some trading comodities, to buy them corne of y^e Indeans. “It was no season of y^e year to goe withoute y^e Cape, but understanding wher y^e ship lay, he went into y^e bottom of y^e bay, on y^e inside, and put into a crick called Naumskachett,[4] wher it is not much above 2. mile over [148] land to y^e bay wher they were, wher he had y^e Indeans ready to cary over any thing to them. Of his arrivall they were very glad, and received the things to mend ther ship, & other necessaries. Allso he bought them as much corne as they would have; and wheras some of their sea-men were rune away among y^e Indeans, he procured their returne to y^e ship, and so left them well furnished and contented, being very thankfull for y^e curtesies they receaved. But after the Gove^r thus left them, he went into some other harbors ther aboute, and loaded his boate with corne, which he traded, and so went home. But he had not been at home many days, but he had notice from them, that by the violence of a great storme, and y^e bad morring of their ship (after she was mended) she was put a shore, and so beatten and shaken as she was now wholy unfitte to goe to sea.[5] And so their request was that they might have leave to repaire to them, and soujourne with them, till they could have means to convey them selves to Virginia; and that they might have means to trāsport their goods, and they would pay for y^e fame, or any thing els wher with y^e plantation should releeve them. Considering their distres, their requests were granted, and all helpfullnes done unto them; their goods transported, and them selves & goods sheltered in their houses as well as they could.

“The cheefe amongst these people was one M^r. Fells and M^r. Sibsie which had many servants belonging unto them, many of them being Irish. Some others ther were y^t had a servante or 2. a peece; but y^e most were servants, and such as were ingaged to the former persons, who allso had y^e most goods. Affter they were hither come, and some thing setled, the maisters desired some ground to imploye ther servants upon; seing it was like to be y^e latter end of y^e year before they could have passage for Virginia, and they had now y^e winter before them; they might clear some ground and plant a crope, (seeing they had tools & necessaries for y^e same) to help to bear their charge, and keep their servants in imployment; and if they had oppertunitie to departe before the same was ripe, they would sell it on y^e ground. So they had ground appointed them in convenient places, and Fells & some other of them raised a great deall of corne, which they sould at their departure.”

The historian here details some domestic infelicities of Mr. Fells in consequence of which the Plymouth Pilgrims

“pact him away & those that belonged unto him by the first oppertunitie, and dismiste all the rest as soone as could, being many untoward people amongst them; though ther were allso some that caried them selves very orderly all y^e time they stayed. And the plantation [149] had some benefite by them, in selling them corne & other provisions of food for cloathing; for they had of diverse kinds, as cloath, perpetuanes, & other stuffs, besids hose, & shoes, and such like comodities as y^e planters stood in need of. So they both did good, and received good one from another; and a cuple of barks caried them away at y^e later end of somer. And sundrie of them have acknowledged their thankfullnes since from Virginia.”

To the account of the loss of the ship, Freeman’s “History of Cape Cod; Annals,” &c., appends the following note:

“The beach where this ship was wrecked was thenceforward called “The Old Ship.” The remains of the wreck were visible many years.”

The January number of the N. E. Historical and Genealogical Register for 1864 (p. 37) contains an able article by Amos Otis, Esq., in which allusion is made to the tradition that the name of the old ship was “Sparrow-Hawk.” Mr. Otis speaks of this tradition as uncertain. We will give the tradition as it is, and leave it to make its own impression on our readers. A family by the name of Sparrow has long resided in the close vicinity of the Old Ship Harbor. The first settler of the name, Mr. Jonathan Sparrow, bought the land, where the family now live, in 1675. The present proprietor, Mr. James L. Sparrow, states that it had been “handed down” from father to son that there was an old ship buried in the sand in Potanumaquut Harbor in the early days of the colony, and that its name was “Sparahawk,” or “Sparrow-Hawk.”

Mr. Otis remarks, that “the evidence which seems to prove beyond a reasonable doubt that those remains belong to the ship which Gov. Bradford informs us was lost in Potanumaquut harbor in the winter of 1626–7 ... is principally based on the geological changes that have occurred on the coast, since its discovery. Archer’s account of Gosnold’s voyage around the Cape, in 1602, and of the appearance of the coast, is so unlike anything seen by the modern mariner, that his relation has been considered a myth or traveller’s tale, unreliable and unworthy of credence. Geological inquiries may seem out of place in a historical and genealogical journal; but if they do nothing more, they will verify the accuracy of Archer’s descriptions, and thus aid us in our investigations of the truths of history.

“The accounts of the wrecked ship in Morton and Prince, are copied from Bradford. Morton is not careful in his dates, but he informs us that the master was a Scotchman, named Johnston, a fact not stated by Bradford. Mr. Prince with his accustomed accuracy, states that a ship was lost in the beginning of the winter [December], 1626. Gov. Bradford’s description of the place where the ship was lost, would be perfectly clear and distinct if the configuration of the coast was the same now as it was when he wrote. Namaskachet Creek remains, but Isle Nauset, Points Care and Gilbert, have been swept away by the waves and currents of the ocean. Where Monamoick Bay was, there is a straight line of sea-coast; where an open sea then was, now long beaches meet the eye; and where were navigable waters, now we see sandy wastes and salt meadows.

“Such remarkable changes having been made in the configuration of this coast since its discovery by Gosnold, and its examination by Smith, in 1614, is it surprising that the knowledge of the location of “Old Ship Harbor” should have been lost, or that the readers of Bradford should have been unable to determine where Monamoick Bay was?

“Prof. Agassiz, of Cambridge, in company with the writer and others, has recently made a careful geological examination of the eastern coast of the towns of Eastham, Orleans, and Chatham.... The result was a verification of the accuracy of Archer’s description of the coast.

“This examination enables me to draw an outline map of the coast as it was in 1602, and in 1626. I have also a map of the harbors, beaches, and salt meadows as they were, and as they now are.” [V. map, p. 14.]

In Gov. Bradford’s account, which we have already quoted, he says that “he landed on Naumskachett creek” on the inside of the bay. From the fact that the distance from this creek, which now forms a part of the boundary line between Brewster and Orleans, to the navigable waters of Potanumaquut is about two miles,—as stated by Bradford,—while to Nauset harbor, the distance is greater, Mr. Otis considers it proved “beyond controversy that Potanumaquut was the harbor into which the ship ‘stumbled.’”

We quote from Mr. Otis, the facts in relation to the discovery:

“On the 6th of May, 1863, Messrs. Solomon Linnell, 2d, and Alfred Rogers, of Orleans, were on Nauset Beach, and discovered portions of a wreck. Mr. Linnell was at the same place on the 4th, when no part of the wreck was visible. This proves that it was uncovered between the 4th and 6th of May, 1863. When first discovered, it was partially covered with the marsh mud in which the wreck had been embedded. On removing some of the mud, they found a quantity of charcoal, and the appearance of the timbers and planks indicated that the vessel of which these were the remains had been burnt.[6] On Saturday, May 9, Leander Crosby, Esq., visited the wreck, and collected a quantity of beef and mutton bones; several soles of shoes, probably made for sandals; a smoking pipe of the kind used by smokers of opium; and a metallic box.”

Dr. Benj. F. Seabury and John Doane, Jr., afterwards visited the wreck, and found the rudder lying a few feet distant; this they removed, and it is now deposited in the hall of the Pilgrim society, at Plymouth. Messrs. Seabury and Doane took measurements of the ship, and public attention was now drawn to a consideration of the subject.

“The peculiar model of the wreck excited the curiosity of the people, and although four miles from the village, it was visited by hundreds, and each one took a fragment as a memento of his visit. At the time the writer was there the current had swept out a basin in the sand around the wreck, and it being low tide, every part excepting the keel could be examined. One striking part was immediately noticed by everyone,—the long, tail-like projection at the stern. The oldest sailor never saw a vessel built on that model, she must have had, to use a nautical expression, “a clean run,” and have been a good sea-boat.... She had been most carefully built. The frames were placed side by side.... There were twenty-three regular frames remaining, or forty-six timbers, not counting the six at the stern. At the bow several frames were missing. The planks were fastened with spikes and treenails, in the same manner as at the present time. Some of the treenails had been wedged after they were first driven, showing that some repairs had been made.

“The timbers and planks of the old ship are very sound, there is no appearance of rot. There are no barnacles upon them, they are not eaten by worms, and there is no indication that they have been for any considerable length of time exposed to the action of the elements. The spikes, bolts and other fastenings of iron have entirely disappeared, ... rust had gradually consumed them, and discolored sand indicated the places where the iron once was. The wreck was embedded in marsh mud and covered deeply in sand. Under such circumstances air was almost wholly excluded, and oxidation must have been slow.

“Though called a ship, she had only one mast, and that as shown by the mortise in the keelson, was nearly midship.”

“In August last, the wreck was again covered with sand, and is now buried several feet below the surface, where it may remain undiscovered for ages. Centuries hence some plodding antiquarian may labor to prove it to be the same I have described in this article.[7]

“One point remains to be considered. Is the wreck recently discovered a part of Capt. Johnston’s ship, lost in 1626? The reader will look at his map. ‘Ile Nawset’ was of the drift formation, hilly, and in some parts rocky. No part of it now remains. About fifty years ago, a small portion of it, called Slut’s Bush, had not washed away. The sand on its shores, and most of which has been washed by the currents from the north, has blown inward by the winds, covering the meadows within, and in some places filling the navigable channels and harbors on the west. In some places the waves of the ocean have swept across the beach, and transported immense quantities of sand to the meadows in a single tide.”

“The wreck of the Old Ship is on the second lot of the Potanumaquut meadows.[8] This was always known as the Old Ship lot, but why it was so called no one could explain. Now the reason is apparent. The position of the wreck has not probably changed since it sunk in the place where it now lies. At low tide there are about two feet of water around it, showing that at high water there was a sufficient depth to have floated a vessel of seventy tons burthen. Every portion of the wreck is below the surface of the meadows. These two facts prove that this vessel was not cast away upon a beach nor on the meadows.

“At the present time a wreck sunk in such a situation would be covered with sand and mud in the course of a month. Similar causes existed then, and it is safe to assume that Capt. Johnston’s vessel was covered up very soon after she was lost.

“Salt meadows do not form on a shore where a surf beats, or where a strong current exists. While the ancient entrance to the harbor was open, there was such a current on the west or inside of Isle Nauset, which prevented the formation of salt meadow near the wreck. After the closing of the old entrance, the current turned west of Pochett and Sampson’s islands, and found an outlet through Pleasant bay, to Chatham harbor, thus leaving a body of still water favorable to the rapid formation of salt meadows. This view is confirmed by the Eastham records. That town was settled in 1646, and in the early division of meadows, the Potanumaquut are not named. As salt meadows were considered more valuable then, than at the present time, it is surprising that they are not named till 1750, if they had then existed.

“Records cannot be quoted to prove the antiquity of this wreck, neither can it be proved by living witnesses; we necessarily have to rely on other testimony. That the rust had entirely consumed all the iron used in its construction is evidence of its antiquity. The position of the wreck in reference to navigable waters, to the salt meadows, and to the beaches is reliable testimony.

“Now it is perfectly certain that this wreck must have been in its present position since the year 1750, or 113 years, for since that date there have been no navigable waters within a quarter of a mile of the spot where it lies. It is also certain that it must have been in its present position during all that period, prior to 1750, while the meadows were forming around it, and on the west. If it is admitted that those meadows are of recent formation, one hundred years would be a low estimate, making the whole time 213 years.

“If it be said that the Potanumaquut meadows belong to the older and not to the recent formation, it proves too much; it proves that the wreck has been in its present position many centuries—that it is the remains of an old ship in which the Northmen, or other ancient navigators sailed.

“The position of this wreck in reference to the salt meadows and to the beach, is the best possible evidence of its antiquity. If driven there it must have been by a westerly wind, which would cause a low tide. Admitting that the vessel of which this wreck is the remains, was, by some unknown cause, forced on the meadows, how was the wreck buried below the line of the surface?

“To suppose that she was so buried on hard meadows by natural causes is an impossibility. That the wreck was there first, and the meadows formed over it, seems a self-evident truth, and judging from the rate at which similar meadows have formed, two hundred and thirty-seven years is not an unreasonable length of time to assign for the formation of the Potanumaquut meadows, and consequently the length of time that the wreck of the Old Ship, at Orleans, has remained in its present position.

“Those who are not aware of the remarkable geological changes that have occurred on the eastern coast of Cape Cod since its discovery, doubt the truthfulness of Archer, who was the historian of Gosnold’s voyages. I have in this article assumed that he was a careful and an accurate observer, and faithfully recorded what he saw. Great geological changes make their own records; they leave in the strata and in the various deposits, the footprints which the scientific student of nature can trace and follow.

“Cape Cod was discovered by Bartholomew Gosnold, May 15th, 1602, O. S. He anchored at first near the end of the Cape, which he called Shoal Hope, but afterwards changed to the name it has since retained. Afterwards he anchored in the harbor, in latitude 42°. On the 16th he sailed round the Cape. After proceeding twelve leagues in this circuitous course, he descried a point of land ‘a good distance off’ with shoals near it. He ‘kept his luff’ to double it, and after passing it ‘bore up again with the land’ and at night anchored, where he remained that night and the following day, May 17.

“He saw many shoals in that vicinity, and ‘another point that lay in his course.’ On the 18th he sent a boat to sound around the point, and on the 19th passed around it in four or five fathoms and anchored a league or somewhat more beyond it, in latitude 41° 40′.

“Nothing is named in this account that the most careless observer would not have seen and noted. When he discovered the first point he was off Eastham, a little north of the beach where the ‘Three Lights’ are now located. He saw the danger, and like a prudent mariner kept his luff to avoid it. The shoal he called Tucker’s Terror, the headland, Point Care. After passing Point Care he bore up again to the mainland. This description of the coast is simple and truthful. To determine the exact position of Point Care, is attended with some difficulty. That it was the north end headland of the island named by Capt John Smith ‘Ile Nawset,’ there appears to be no reason to doubt. The only difficulty is in determining precisely where the north end of that island was in 1602. The northern end of it, which persons living remember, was opposite the present entrance to Nauset Harbor. In 1602 it probably extended half a mile further north, that is, as far north as the low beach extended, that persons now living remember. John Doane, Esq., now seventy years of age, was born in the immediate vicinity of Point Care, his father and grandfather, in fact all his ancestors from the first settlement, owned the land and meadows between Ile Nawset and the main. He says that within his recollection Point Care has worn away about half a mile. When his grandfather was a boy, Point Care extended much further into the ocean than it did when he was young.”

These are not vague and uncertain recollections. Mr. Doane points to monuments, and the exact distance that the ocean encroached on the land within his recollection can be ascertained. He states that fifty years ago a beach extended from the present entrance of Nauset harbor half a mile north, where the entrance then was. Within this beach his father owned ten acres of salt meadows, on which he for several years assisted him in cutting and raking the hay. Now where that beach was there are three or four fathoms of water, and where the meadows were is a sand bar on which the waves continually break, and make Nauset harbor difficult of access. Within his memory the north beach, connected with Eastham shore, has extended south one mile, and the whole beach has moved inward about its width, say one fourth of a mile. Formerly there were navigable waters between Nauset and Potanumaquut harbors. It is about a century since vessels have passed through, and about fifty years since the passage was entirely closed. This is caused by the moving of Nauset beach inward. Dunes always travel inward, never outward, let the direction be what it may.

“Mr. Doane says that his grandfather informed him, that when he was young, a rocky, swampy piece of land, known as Slut’s Bush, was about in the middle of Isle Nauset; that many berries grew there, and that he had repeatedly been there to pick them. When the present John Doane was a lad, only the western edge of this swamp remained. The roots of the trees and bushes that grew there ran under and between the rocks and stones, and when the waves undermined the rocks, the whole, rocks, stumps and roots, settled together. Slut’s Bush is now some distance from the shore, in deep water; vessels pass over it, and on a calm day the stumps and roots may be seen at the bottom. The fisherman sometimes gets his line entangled with them and pulls them up. During violent gales of wind they are sometimes loosened and driven to the shore.

“Beyond Slut’s Bush, about three miles from the shore, there is a similar ledge called Beriah’s Ledge, probably formed in precisely the same manner as Slut’s Bush ledge is known to have been formed. Six nautical miles south of Point Care, Gosnold discovered another headland, which he named Point Gilbert. Archer furnishes us with all the particulars respecting the soundings, the straits, his passing round it, and anchoring a league or more beyond, in latitude 41° 40′. We have historical and circumstantial evidence that Point Gilbert existed in 1602; it united with the main land at James Head, near Chatham lights. From James Head on its south shore, it extended nine miles on an east-by-south course, to its eastern terminus, afterwards known as Webb’s Island, situate where Crabb’s Ledge now is. Cape Care was worn away by the gradual abrasion of the waves; over Point Gilbert the sea, during a violent gale, swept, carrying away long sections in a single day. The inner ledge on the line of Point Gilbert is known as Island Ledge, and the name indicates that the sea broke over the point at two places about the same time. Rev. Dr. Morse states that Webb’s island at one time contained fifteen acres of rocky land covered with wood from which the early inhabitants of Nantucket procured fuel.[9] The process which has been described as having occurred at Slut’s Bush ledge also occurred at Crabb and Island ledges; the stumps and roots of the trees were carried down by the superincumbent rocks. Mr. Joshua Y. Bearse, who resided many years at Monamoit point, and has all his life been familiar with the shoals and ledges near Chatham, informs me that it is very difficult to obtain an anchor lost near either of these ledges; the sweeps used catch against the rocks and stumps at the bottom where the water is four fathoms deep. He also states that after the violent gale in 1851, during which the sea broke over Nauset Beach where the ancient entrance to Potanumaquut harbor was, and where the entrance to Chatham harbor was in 1775, with a force which seems almost incredible, sweeping away banks of earth twenty feet high, cutting channels therein five fathoms deep, moving the sea around to its very bottom, and tearing up the old stumps which had been there more than a century,—Mr. Bearse states that more than one hundred of these drifted during that gale to the shore at Monamoit beach, and that he picked them up for fuel. A part of these were stumps that bore the marks of the axe, but the greater part were broken or rotted off.

“These old stumps did not grow under the water; they did not float to the positions from which they were dragged up; they grew in a compact rocky soil overlying a loose sand. The waves and the currents removed the loose substratum, and the rocks and the stumps went down together into the deep water where they are now found. From the place where Gosnold anchored, a league or more from Point Gilbert, there was an open sea to the southwest. Monamoit beach, which projects out eight miles south from Morris island, did not then exist; there was nothing there to impede navigation.”

[“Prof. Agassiz who is the author of the geological theory which the accompanying map delineates, furnishes us with the following note, dated Cambridge, December 17, 1863.

“Surprising and perhaps incredible as the statements of Mr. Amos Otis may appear, they are nevertheless the direct and natural inference of observations which may easily be made along the eastern coast of Cape Cod. Having of late felt a special interest in the geological structure of that remarkable region, I have repeatedly visited it during the last summer, and in company with Mr. Otis examined on one occasion with the most minute care, the evidence of the former existence of Isle Nauset and Point Gilbert. I found it as satisfactory as any geological evidence can be. Besides its scientific interest, this result has some historical importance. At all events it fully vindicates Archer’s account of the aspect of Cape Cod, at the time of its discovery in 1602, and shows him to have been a truthful and accurate observer.—Editor.”]

It only remains to state the facts in regard to the final recovery and saving of the wreck. Messrs. Leander Crosby and John Doane, Jr., assisted by Solomon Linnell, 2d, Alfred Rogers, and others, conveyed the planks and timbers, at various times, to the upland. One mass, including the keel and thirteen timbers, was thrown out by the sea, and was at once secured. The whole was collected together, on the premises of Mr. Crosby, whence it was conveyed to Boston, and the pieces restored to their original position, as already related, by Messrs. Dolliver and Sleeper.