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SPOONEH uu liy llic editor several years ai;ti aloiii;- tlie lines of i-eseaicii and of tlie collection and systematizing; of nialerials. Tlie identification of .Mr. Sjiooner with the enterprise dates from a later period, hnt in its relative imjiortance is not to be esti- mati'd by its dnration. To him the credit of the antlioi'ship of the History is uudividedly dne. The editor's personal shai-e in the joint iindertakinji' — apart from the selection of the ])lan of the work and the procnrement and arrangement of materials — has been mostly that of sn])ervision; or, more ]iro](erly expressed, of such co-oiieration with ^Ir. Spooner as personal knowledge of the snbject and zealous interest in the project have enabled him to render in the ])arlicnlars specially of recommendation, contribution, and criticism. This His- tory is therefore not a work of collaboration, e.vcept in the s(^nse here ]irecisely indicated. As a literary work it is the exclusive pi'o- ihictidii (if .Ml-. Sjiooner; and whatever satisfaction the editor may icasonably — without an excess of comjilacency — take io himself in view of his own association in the entei'pi-ise, rests in a peculiar mannei- u])on his appreciation i>{ the conscieutious deNotinn and ai-- cnm]dished ability with which .Mr. Sjiooner has biouyht it lo its jirac- lical issue. Althouiih the ])revioiis histories of W'eslidiester Counlw liolton's and Scharfs, ai-e works (d' i;reat \dlume and information, they are \\orks of riderence strictly, and as sue h b(doiii; rather to I lie dejtart- nieiit i>\' histoiical miscellany than to that of bo(dcs adapted foi- i)o]»- ular i'ea'xliiiiistiv('l_y and cxccllcnl 1 v wiittcn, (]ii not ((Piistitutc a liis- tory eo]ile, and (luite incapalde of Ixdni^' taujiht to the youn,ii because of tlie unsuitability for tliat jiurpose of all books heretofort" imblished that lieai' on the subject. In foiniulatinji' the plan for the ])resent work the editor had funda- menlaily in view a lucid continuous narrative, thoroujih in its treat- ment of the outlines of the subject and reasonably attenti\'e to local details without extendini;' to minuteness. These lines have been bd- lowed Ihi'ouiihout. All exist inii materials, so far as accessible, have In en utilized, ])ro]ier credit beini; ;Lil\-en to the sources from whicli borrowinjis have been made. The work conipi-ehends a variety of new materials, whiidi have been interwoven in the text. Porticms of the manuscript have been reAisi'd or criticised by jiersons jiarticiilaily W(dl informed on certain jihases id' the subject; and to all of tjiese critics the editor extends his thankful aidvnowlediiinents. Special credit is due to Mr. James L. \Vells for his editoi-ia! super- vision of the entire work so far as concerns the sections of the oriijinal county now constituting the Borough of the Bronx, New York City; and thanks must also be expressed to Mr. Wells for the crest of Jonas Broiudc (the first settler of Westchester County), intioduced by his kind permission in the title-])age. It is probably not generally known that from the Broncdc crest have been derived some of the essential features of the arms of the State of New York. " Shon.vaud IIojii:sT]:.\r)." AUCiTTST, 11)00. /vfez^J^ CONTENTS Editor's rrefjuH' iii ("llAl'TKIt I I'liysiciil Description ot I lie ('(niiity 1 ClIAl'lKK II Tlif Aboriyiual luhabitauls 17 ("llAI'TKR III DiscoVk-ry and rreliiuinary \'icw .")! ("iiAi-i'in;. I\' The Earliest Settlers — I>rnn(d<, Anne Ilutrldnsim, 'riirockninr.Dn, Tornell T."> ("IIAI'I'KK \' Tlie Kedenbtable Caplain dolin rnderliill Dr. Adrian \'an der Dimek !>•; ("iiAi'i'i:i; \'l Iteuininniis ot Sei-ious Sel I lenienl \\'est( iiesler Town. Kye in ("hai'ti:!; \'1I "The Portion of the North Kidinti on the Main" — l'n)j>Tess of Settlement and Bejiinniniis (d' I lie .Mamii'ial Estates \'.V2 CiiAriDii \lll Tlie riiiliiises and tlie \'an Corthindls l.").") CiiArrKi: IX Telliani .Manor and New Korlielle Caleb JleatlH-ote and Sears dale .Manoi'— -( ieneral ( ?bser\al ions on ; he .Manors \'i-'> ( 'llAI'TKI; X (ieneral Ilistorieal Hex lew lo llie l!et;innin,i:' of the Eii;lile(-ni li Cenlnry — ('(inii)letion of ilie Work ef Original Sel 'lenient ... . I'.i-"! ('iiAi'ri:u XI A (I lance a I tlie Hoi-onuh Tow n of Westtdiester 22(> Vl ajXTENTS Chapter XII The Election on the (Jreen ;it Kiistcliester, 17;« 235 CllAl'TlOIl XIII The Aristocratic I'aiiiilies and Their Intlueuces 25r) ("IIAI'TEH XIV From the Stainji Act to I he Last Session of the Colonial Assembly 277 <'11A1'TEII XV Westchester County in i.iiie for Indcjicudence — Events to .Inly 0, 1 77(1 2;t(i ClIAI'TEU X\'I The State of New Voik liorn at \Vhite IMains — Events to October 12, 177(i 335 ClIAI'TEU XVII The Campaign and Battle id' White IMains 357 Chapter XVIII Fort ^^'ashin}^■ton■s I-'nll — The l)(din(iuencv of (leneral Lee 397 Chai'TER XIX The Strategic Situation — TIh' Xentral (Jrouud 412 ClIAl'TER XX Events of 1777 and 177S 425 ClIAl'TER XXI I'roni .lannai-y. 1779, to September, 17S(1 44t) Chatter XXII The Captnre of Andre 4()4 ClIAl'TER XXIII The West(diester Ojiei-ations of the Allied Armies, 17S1 — End of the War 4!l7 Chapter XXIV General Ilislor\ (d t lie Count \('(Hi(lndesented a mere problem of territorial rectification upon the basis of reciprocal concessions by the two provinces and subsequently the two common- wealths concerned; and. accordingly, while leaving a jiortion of the eastern border line of Westchester County somewhat indeterminable for two centuries, the issues at stake never affected the integrity of its aggregate area as allotted at the beginning. On the other hand, the southern boundary of the old county lias undergone extremely radical nuiditicatioiis. which are still in progress. Since 1873, by various legislative acts, large sections of it have been cut away and transferred to the City of New York, comprising what until r<'cent Aears were known as the • annexed districts " of the metropolis, now HISTORY OF WESTCHESTER COUNTY officially si,\h-(l t\w •• Itoiouiili ol' the Jtroiix "" ot the Greater City. Altlionjiii tile ci.uiity still n-tains its two most populous muuicipali- ties, Youkois aud .Alouut \'eruou, the New York City liue lias been pushed ri.L;ht up to their borders, and there is uo i-easonable doubt that within a few more yeai-s they, too, Mill be absorbed. Already forty- one and one-half square miles, or 20,500 acres, have been annexed to the city. In these pages the story of old Westchester County is to be told; and whenever the county as a whole is mentioned without specific indicatidii of the present limits, the reader will uuderstanate wave. Avliile tlic latter is llic result <\i ilie cuiiracl of tlie Sound and Sandy Uook tides. The tides in the Hudson Itiver and Spnylen Duyvil are ]»rodiu-ed by the pntpagation of the sea li(h' tiirougli the Upi)er and i.ower hays." Tlie mean rise of tlie li(h' in the Harlem is from tive and one-half to six feet; in the S])iiyten Duyvil ("i-eek it is iJu'ee and eij;'bt-teuths feet. The mean iiiiih water level in the Hudson liiver at Spuyteii Duyvil t'reeU is nearly a foot lower and an hour and forty minutes earlier than in the Harlem, and the mean duration of the rise of tide in the former is thirty-six minutes shorter than in the latter. The westei-ly current, from Ilellgarc, is swifter than the east- erly, from the Hudson. The jdacc of "divide" between the Harlem I\iver and the S] my ten Duyvil ( 'reck is usually located at Kin<;sbridge. In early times the Harlem was naviiiable for most (d' its leiiiith. but owing to artihcial obstructions (notably that of ^lacomb's Daiui. which were begun in the first part of the present cent iiry. i he ( haniiel above the present Central Bridge became both shallow ami con- tracted. The mean natural depth of Si)nyte]i Dnyvil Creidc lias always been com]iaralively slight. Owing to the importance of this water- way as a means of short transit for craft plying between the Hudson Kiver and ports on the Sound and in New England, the United Stales Government has in our own time dredged a channel, whi( h. from the Hudson to Hellgate. has a de])th of from twelve to fifteen feet. This impro\ement, knov\n as tlie Harlem Shi]) ("anal, was ojuMied to com inerce on the 17th of June, lS9o. The Harlem Kiver and S|iiiyien Duyvil Creek are crossed at iiresent by thirteen bridges. Along the Spuyten Dnyvil and Harlem Kiver [loiiion of its water line, as along the Sound, the ddd i (oiinty of Westchester loses the comparatively lofty feature whicli ( haraclerizes its Hudson shore, anil the land is generally Ioav. sinking into marshy tracts in some localities near the Sarreto Pr)int. Hunt's Point, Coi-nell's Neck (Clason's Point). Throgg's Neck (with Fort Schuyler at its ex- tremity), Kodman's (I'elham) Xeck, Davenport's Neck, De Lancey Point, and Kye Neck. S(une of these localities are famous in the his- tory of the county, ihein-ovince, and the State. The coast indentations imliide the outlets (d the TSronx Tliver, Westchester Creek, and tlu' Hut( hinson liiver; Eastchester l?ay, Pelham Bay, De I.ancey Cove and 6 HISTORY OF WESTCHESTER COUNTY J.aicliiuuiit lliubur, MaiuaruiU'ck Harbor, aud B^raui Harbor. Mucli of the contraband trade of colonial times was supposed to have found L-over in the unobserved retreats which the deep inlets of this toast afforded; and of some of the earlier settlements along the t^ound it is supposed that they were undertaken quite as much to provide secure places of rendezvous for commerce ;iiore or less outside the pale of the law as to iH'oniote the development of the country. In close prox- imitv to the shore are manv islands, of which the more notable are THE H.\HI,KM KIVEK I.Ml'KOVK.MK.Nl S (^HVCKMAN S .MLA IX.IWSJ. those between Pelham Bay and Xew IJochelle, including' City, Hart's, Hunter's, David's, and Glen Islands. The New York City limits on the Hudson now reach to the northern bounds of the hamlet of Mount Saint Vincent, and on the Sound to a ]>oinl about ojiixisite, taking in also Hunter's, Hart, and City Islands. Of the more than one hundred miles of coast line originally and until 1873 possessed by Westchester County, about thirty have passed to the city — thi*ee miles on the Hudson, eight on Spuyten Duyvil Creek and the Harlem Uiver, and the I'emaindtu' on the Sound. The eastern boundarv of the couutA' is an entireh* arbitrarA- one. PHYSICAL DKSCIMI'TIOX OF THE COUNTY 7 ill iiu rcsiK'cl lullnwiii-i ualmal liiics df division, (if whicii, indeed, tJiere are none of a eoutinuous cliavai-ter at this portion of liie eastern confines of New York Stale. To t lie reader iiiifaniiliar witii I lie jiistory of the New York and Connecticut honndary dispute, this /.ij^zaj;- line will appear to liave been traced (|uiie without reference to any sym- metrical division of territory, hut tor the accoininodation of special ol)jects ill territ(u-ial adjustment. This is largely true, although the line, as finally drawn, was rednced as nearly to a simple construction as could he done consistently with the very dillicnlt circumstances of the boundary dispnti'. On the iKU'th the limit fixed for the couiily at the lime of its erec- tion was the ttoint where the Tlighlands of the Hudson begin. Pur- suant to this provision the line between \Yestciiester and I'utnam Counties starts on the Hudson at Anthony's Nose and follows an east- erly course to the Connecticut boundary. The surface of the county consists of several ranges of hills, with valleys stretching between, in wliicli are numerous streams and an abundance of lakes. None of the jihysical features of Westchester County (if we except its lovely i)ros|>('ct of the Hudson) are in any wise r{' the c(ninty), passes from the town of Blount Pleasant on the Hudson eastward tiirougli the towns of New Castle, Bedford, Poundridge, and Salem into Con- necticut. In spite of this exce])(ioii. however, the general trend of the hills is north and south, a fact illustrated by the almost uniformly southerly course of the more considerable streams, and by the usually level character of the roails running north and south, as contrasted with the c(ms]»icuous uneveiiuess of those which extend east and west. Famous in our county's history are the North Castle or Chaiijiaciua Hills, above White Plains, into which Washington retired with the <'ontinental army after the engagement near the latter place (October 2S, 177(1 1, and. mi account of the .strength of the new position thus gained, ciuupelled tieneral Howe, with his greatly su]teri(u- forc<'. to return to New 'S'ork. The highest point in Westchester County ( ac- 8 HISTORY OF WESTCHESTER COTXTY cording to the figures of till- i'liitci] States ('o;ist Survey l is Antiionv's Nose, !)no feet above half tide h-vei. rilYSICAL DESCKIPTIOX OF TIIK COINIV 9 Of tlio streams of AVestcliestor County the iiaiiics of two, the Croloii and tlio lironx, have become widely familiar. Tlie former riv<'r is ilie chief source of tlie water su])ii]y of New Yorlc City; I he latter — wliicii, by the way, also furnishes water to New York — has nmny historic and romantic associations, tU^ar to New Yorkers as well as West- chester people, and its name has been adopted for one of the beautiful new ])arks of the city, and also for one of the five grand divisions which constitute the Greater New York. t^ome half dozen streams of noticeable size find their outlets in the Hudson. Peekskill Creek gathers its waters from the hills of the northwestern corner of the county, and flows into the Hudson just above the village of Peekskill. Furnace ISrook is a small rivulet which empties into the river several miles farther south. Then comes the Croton, having its outlet in Croton Buy, as the northeastern por- tion of the Tappau Sea is called. The Croton has its sources in Dutchess County — these sources com- prising three " branches " (the East, Middle, and West), which unite in the southern \n\vt of Putnam County. In its course through ^Yest- ciiester County to its mouth, the Croton receives as tributaries the Mnscoot, Titicns, Cross, and Kisco Rivers. The Muscoot is the outlet of the celebrated Lake Mahopac in I'utnam County, and the Cross (also called the Peppenegheck ) of Lake Waccabuc, one of the largest of the Westchester lakes. The Croton watershed lies almost wholly in the State of New York, although draining a small ar<'a in Connec- ticut. It extends abcmt thirty-three miles north and soiiili and eleven miles east and west, and has an area of 339 square miles above the present Croton Dam. to Avhich about twenty square miles will be a former is thirty-eight ami the latter thirty-three miles long, the distance in each case beiuii measured to the receiving reservoir. It is the old a(pieduct 10 HISTORY OF WESTCHESTER COUNTY which crosses the Havh-m River over High Bridge; the uew is carried underneath the stream. South of tlie ("roton iliver the next Hudson tributary of interest is the Sing Sing Kill, which finds its nioutli tlirough a romantic ravine crossed by the notable Aqueduct Bridge. Next comes the Pocantico River, entering the Hudson at Tarrytown. The last feeder of the PHYSICAL DESCUIPTION OF THE CorNTY 11 Hudson lioiii WestL-lu'stt'i- Cimiity, and the last received by il bcfm-e discliargiug- its waters into the sea, is the Sawmill (or Xepperhaiii Eiver, at Youlcers. To tliis stream is due the credil for the creation of a very considerable i»ortion of the manufacturini; imlustries of the county, and consequently, also, to a i^reat extent, thai for ihc building up of the City of Yonkers. Into the Spuyten Duyvil Creek empties Tibbel's I'.rook, a small runlet which rises in the Town of Youlcers and Hows south, passing throujih Van Cortlandt Lake (artificial). The most noteworthy of the streams emptying into the Sound is the Bronx Kiver, whose outlet is between Hunt's I'oint and Cornell's Neck. The Bronx lies wholly within Westchester County, having its headwaters in the hills of the toAvns of Mount IMeasant and New Castle. It traverses and partially drains the middle section of the county. This river, with other Avaters which have been artificially connected with it, afl'ords to New York City a water sui)ply of its own, quite independent of the Croton s3-stem--a fact, perhaps, not generally understood. It is dammed at Kensico Station, making a storage reservoir of 250 acres. A similar dam has been thrown across the Byram River, and another across the outlet of Little Bye Bond. By the damming of Little Kye Pond that body of water, witli Bye Bond, has been converted into a single lake, having an area of 2S(> acres. The three parts of this system — the Bronx, Byram, and Bye Bond reservoirs — are, as already stated, connected aiMiticially, ami the water is delivered into a receiving reservoir at \\'illiams's Bridge through the so-called Bronx Biver pipe line, a conduit of forty-eight- iuch cast-iron pipe. The portion of the Bronx watershed draiuerl for this jmrpose has an area of thirteen and one-third scpiare miles. Bast of the mouth of the Bronx Biver on the Sound are the outlets of Westchester and Eastchester Creeks — tidal streams — em])tying, respectively, into Westchester and Ea.stchester Bays. The Hutciiinson Biver rises in Scarsdale and tloAVs into Eastchester Bay. The Mania- roneck Biver has its source near White I'lains aiul Harrison, tinding its outlet in Mamaroneck Harbor. The B.yram Biver, which enters the Sound above Bortchester, and at its mouth separates our county from Connecticut, drains parts of North Castle and Bye. Blind BrooU empties at Milton, after draining portions of Harrison and Bye. Most of tlie streams flowing into the Sound afford, by the reflux of the tidi', an intermitting hydraiilic power. The MiaTius Biver, rising in North Castle, and Stamford .Mill Kiver, rising in Boundridge, find their way to the Sound through Connecticut. Some minor streams in the northern section of the county How into Putnam Countv. 12 HISTOUV OF WESTCHESTKK COUNTY The lakes of AYestclioster, like the hills and streams, boast no fea- tures of exceptional interest, but are strictly in keeping with the quiet beauty of the general landscape. The largest, as already men- tioned, is Crolon Lake, entirely artiticial; and we hav(^ also seen that several of the natural lakes have been utilized for purposes of water supph'. Lake Waccabuc, in the Town of Lewisboro, has, since 1S70, been connected with the Croton system. It covers over two hundred acres, and is very deep and ])ure. In the Town of Poundridge several PHYSICAL DKSCKll-llOX VF TlIK CUCNTY 13 poii»ls< have beeu artiliciallv joined tu vnv unullier, loriiiiiii; a hand- some body of water, called Trinity Lake, a mile aud a (luarter long, which supplies the City of Staiiifofd, Conn. A dam twenty feet high has been erected across its outlet. Other lakes of local importance and intei'est are Peach Lake, on the Putnam County border; Mohegan and ^lohansic lakes, in Yorktown; Valhalla Lake (through which the Bron.\ Ikiver flows j, between Mount Pk-asant and North Caslle; Kye Lake, near the Connecticut line; Byram Lake, in Bedford and North Castle, the feeder of the Byram River, and Cross Pond (100 acres i in I'oundridge. The rocks of Westchester County consist mainly of gneiss aud mica- schist of many dissimilar varieties, and white crystalline limestone with thin interlying beds of serpentine, all of ancient origin and entirely devoid of fossils. Professor Ealph S. Tarr, of Cornell Univer- sity, in a recent sei'i<^s of jiajiers' on the geology of New York State, embodying the latest investigations aud conclusions on the subject, assigns to the southern angle of the State, including Westchester County, the name of the " (Jneissic PTighbind Pi-ovince." This ]»rov- ince, he says, is of complex structure, and one in which, in its main and most typical part, the rocks are very much folded and disturbed metamorphic strata of ancient date. " These rocks," he continues, " are reallj' an extension of the highlands of New Jersey, which reach across the southern angle of New Y'ork, extend northeastward, and enter Connecticut. Besides thes(^ Archean gneisses theT'c is some sandstone and a black diabese or trap, which form the Palisades, besides extensive la.vers of limestone, gneiss, and schist, which extend across the region occupied by th<* City of New Yoi-k. This whole series of strata is intricately associated. Except at the very seashore line, the province is a moderate highland, with rather rough topog- raphy and with hills rising in some ])laces to an elevation of 1.000 or 1,200 feet above the sea level. Wliei'e there is limestone or sand- stone in this area, there is usually a lowland, while highlan