The beginning
of the fifteenth century was an era of great changes in all Europe. It
was the end of the darkness of the middle ages, the revival of learning
and science, and the birth of many useful arts, preeminent among which
was that of printing. The invention of the mariner's compass in the preceding
century had enabled sailors to go out of sight of land with impunity, and
a thirst for exploring unknown seas was awakened; long voyages were undertaken
and important discoveries made.
It was during this age of mental activity and growing knowledge
that Christopher Columbus undertook the most memorable enterprise that
human genius ever planned, and which renders his name immortal. On the
third of August, 1492, a little before sunrise, he set sail from Spain
for the discovery of the western world. A little before midnight, on the
thirteenth of October, he descried a light on the island of San Salvador.
From this moment properly dates the history of America. From this time
forward its progress bears date from a definite period, and is not shrouded
in darkness nor the mists of tradition.
Two years after the discoveries of Columbus became known in England,
Henry VII. engaged John Cabot, a Venetian merchant, to sail in quest of
discoveries in the West, and this navigator, in 1497, reached the coast
of Labrador, which he named Prima-Vista, thus making, probably,
the first visit to the coast by Europeans since the day of the Norsemen.
This voyage was succeeded by others under Sebastian Cabot, son of John,
in 1498, and by Gaspar Cortreal, from Portugal, to whom the discovery of
the St. Lawrence some authorities claim is due. This adventurer returned
to Lisbon in October of that year, laden with timber and slaves, seized
from among the natives of the coasts he had visited. On a second voyage
he perished at sea. In 1504 the French first attempted a voyage to the
New World; and in that year some Basque and Breton fishermen began to ply
their calling on the banks of Newfoundland and along its adjacent coasts.
From these the island of Cape Breton derived its name. In 1525 Stefano
Gomez sailed from Spain and is supposed to have entered the Gulf of St.
Lawrence and to have traded upon its shores. A Castilian tradition relates
that, finding neither gold nor silver upon the coasts, nor anything that
conveyed to these sordid adventurers an idea of wealth of any kind, they
frequently exclaimed "aca - nada," signifying "here is nothing,"
and that the natives caught up the sound, which was repeated by them when
other Europeans arrived, and thus gave origin to the designation of Canada.
In 1534 Francis I., king of France, listening to the urgent advice
of Philip Chabot, admiral of France, who portrayed to him in glowing colors
the riches and growing power of Spain, derived from her trans-Atlantic
colonies, dispatched Jacques Cartier, an able navigator of St. Malo, who
sailed April 20, 1534, with two ships of only sixty tons each and one hundred
and twenty men, reaching Newfoundland in May. After coasting along for
sometime, without knowing it was an island, he at length passed the straits
of Bellisle and traversed the Gulf of St. Lawrence. Having spent part of
the summer on these coasts, he sailed on the 25th of July, highly pleased
with the hospitable reception he had received from the natives, with whom
he traded for furs and provisions. His report induced the French king to
attempt a colony in the newly-discovered regions; and in May, 1535, Cartier
sailed with three small ships, with a numerous company of adventurers,
and arrived on the coast of Newfoundland much scattered and weakened by
a disastrous storm of July 26th. Here they took in wood and water, and
proceeded to explore the gulf, but were overtaken, August 1st, by a storm
which obliged them to seek a port, difficult of access, but with a safe
anchorage, near the mouth of the "Great River." They left this harbor
on the 7th, and on the 10th came to a "gulf filled with numerous islands."
Cartier gave to this gulf the name of St. Lawrence, having discovered it
on that saint's festival day. Proceeding on this voyage he explored both
shores of the St. Lawrence. Pleased with the friendly disposition of the
natives, and the comfortable prospects of a winter's sojourn, Cartier moved
his vessels where a little river flowed into a "goodly and pleasant
sound," which stream he named St. Croix, near the Indian village of
Stacona, the site of the present city of Quebec. Subsequently, October
2d, he ascended the river to a populous Indian village called Hochelaga,
on the site of which the city of Montreal now stands. Here Donnacona, an
Algonquin chief, conducted Cartier to the summit of a mountain about two
miles from the village, and to which he gave the name of Mount Royal, or
Montreal, and showed him, "in that bright October sun, the country for
many miles south and east, and told him of great rivers and inland seas,
and of smaller rivers and lakes penetrating a beautiful country belonging
to the war-like Iroquois. This beautiful country, which the chief called
Iroquoisia, included the present state of Vermont. Thus, to Jacques Cartier,
a French navigator and explorer, is due the honor of having been the first
European to gaze upon the Green Mountains of Vermont. In May Cartier returned
to France, taking with him the Indian chief Donnacona, and two other prominent
natives of the village, as prisoners; and they, who had treated the Frenchmen
with such uniform kindness, died in a strange land, exiled from their homes
and friends.
During each succeeding year, for sometime after, expeditions were
sent out to the newly-discovered river; but misfortunes attended them all,
and no efficient attempt at colonizing the country was made until 1608,
when DeMonts, a Calvinist, who had obtained from the king the freedom of
religious faith for himself and followers in America, though under the
engagement that the Catholic worship should be established among the natives,
after several perilous voyages and much opposition, dispatched Champlain
and Pontgrave, two experienced adventurers, to establish the fur trade
and begin a settlement. Samuel Champlain reached Quebec, where Cartier
had spent the winter nearly three-quarters of a century before, on the
third of July. On the 18th of the following April, 1609, in company with
two other Frenchmen and a number of the natives, he started up the St:
Lawrence, and, after a time, “turned southward up a tributary” and
soon entered upon the lake which perpetuates his name. Thus came the first
European upon the territory now included within the limits of Vermont.
The early explorations and discoveries we have mentioned led to
much litigation and controversy on the part of the several European countries
under whose auspices they had been conducted. The English, on the grounds
of the discoveries of the Cabots, claimed all the country from Labrador
to Florida, to which they gave the name Virginia; but their explorations
were confined principally to the coast between Maine and Albemarle Sound.
The French confined their explorations principally to the country bordering
on the St. Lawrence and its tributaries, which they named New France; while
the Dutch, by the discoveries of Henry Hudson, afterwards laid claim to
the country between Cape Cod and the Delaware river, which they called
New Netherlands.
Attempts at colonization were made by England during the reign of
Elizabeth, but they proved abortive, and it was not until the Tudor dynasty
had passed away and several years of the reign of James I., the first of
the Stuarts, had elapsed, before the Anglo-Saxon gained any permanent foothold.
Stimulated by the spirit of rivalry with France, England pushed her explorations
and discoveries, while France, from her first colony on the St. Lawrence,
explored the vast region from the great lakes to the Gulf of Mexico, and
established among the savages missions and trading posts, spreading from
Canada through the West, and finally through New York and Vermont.
The rivalries and jealousies that had made France and England so
long enemies in the Old World were transplanted to the New Continent. The
French made allies of the savages anti waged war against the English, and
years of bloodshed followed. The first of these hostilities, which are
now known as the old French and Indian wars, began with William's accession
to the throne of England, in 1690, and was terminated in the peace of Ryswic,
in 1697. Queen Anne's war, so-called, came next, commencing in 1702, and
terminating in the peace of Utrecht, in 1713. The third controversy was
declared by George II, in 1744, and continued until the preliminaries of
peace were signed at Aux-la-Chapelle, in 1748. The final great conflict
was declared by Great Britain, in 1756, and terminated in the capture of
Montreal, in September, 1760, when the whole of New France, or Canada,
was surrendered to Great Britain..
During the progress of these wars the territory of Vermont was often
crossed and recrossed by portions of both armies, and a few military settlements
sprang up. The first of these, however, was even before the wars, in 1665,
on Isle La Motte, where a fort was erected by Captain DE LA MOTTE, under
command of M. DE TRACY, governor of New France. In 1690 Capt. Jacobus DE
NARM, with a party from Albany, N. Y., established an outpost in the present
town of Addison, at Chimney Point, where he erected a small stone fort.
The first permanent settlement, however, and the first of any kind by Anglo-Saxons,
was begun within the limits of Windham county, in the town of Brattleboro,
in 1724, when Fort Dummer was built. For six or seven years the garrison
of this fort were the only white inhabitants. In 1730 the French built
a fort at Chimney Point, and a considerable population settled in the vicinity.
In 1739 a few persons settled in Westminster, and about the same time a
small French settlement was begun at Alburgh, on what is now called Windmill
Point, but was soon abandoned. The colony at Westminster increased but
slowly, and in 1754 the whole population, alarmed by the Indian attack
upon Charlestown, N. H., deserted their homes. Forts were erected and small
settlements were commenced in several other places, but fear of the Indians
prevented any large emigration till after the last French war, when, the
Province of Canada being then ceded to Great Britain, the fear of hostile
incursions subsided and the population rapidly increased.
During these wars, also, grants of land lying within the present
limits of the state had been made by the Dutch at Albany, by the French,
and by the colonies of Massachusetts, New Hampshire, and New York, and
each claimed jurisdiction over them. All of these claims, except that of
New York, however, were relinquished without much controversy, of which
more will be said on another page. But at the close of hostilities the
lands were sought so eagerly by adventurers, speculators, and settlers,
that in a single year, subsequent to 1760, Gov. WENTWORTH, of New Hampshire,
granted in the name of King George III. not less than sixty townships of
six miles square, and two years later the number of such grants amounted
to 138. The territory now began to be known by the name of the New Hampshire
Grants, and the number of actual settlers soon became quite large. The
affairs of these settlers were managed by committees in the several towns,
who met in general convention, when occasion required, to provide for their
common defense and welfare. The decrees of these conventions were regarded
as law, and violations of them were punished with extreme severity. While
the Revolutionary war was in progress the land title controversy was in
a degree suspended; but soon after the war broke out it became apparent
that the settlers of the grants needed some better organization than was
possible by means of committees and conventions. Accordingly, in 1776,
a convention was held at Dorset, and an address to Congress prepared, declaring
the unwillingness of the settlers to be regarded as subjects of New York.
This was not favorably received by Congress, whereupon the more resolute
of the people determined to assume the powers of an independent state,
"and risk the consequences." Another convention was held at Dorset, in
June, and met again by adjournment in September, when such measures were
taken that, at a convention held in Westminster, it was decided, on the
16th of January, 1777, that the following declaration should be adopted:
"This convention, whose members are duly chosen by
the free voice of their constituents, in the several towns on the New Hampshire
Grants, in public meeting assembled, in our names, and in behalf of our
constituents, do hereby proclaim and publicly declare, that the district
of territory comprehending and usually known by the name and description
of the New Hampshire Grants, of right ought to be, and is hereby declared
forever hereafter to be considered as a free and independent jurisdiction
or State, by the name and forever hereafter to be called, known and distinguished
by the name of New Connecticut, alias Vermont ; and that the inhabitants
that at present are or may hereafter become residents, by procreation or
emigration, within said territory, shall be entitled to the same privileges,
immunities and enfranchisements as are allowed ; and on such conditions,
and in the same manner, as the present inhabitants, in future, shall or
may enjoy; which are and forever shall be, such privileges and immunities
to the free citizens and denizens as are, or, at any time hereafter, may
be allowed, to any such inhabitants, or any of the free and independent
States of America; and that such privileges and immunities shall be regulated
in a bill of rights and by a form of government, to be established at the
next adjourned session of this convention." |
On the 4th of June the committee met at Windsor, there being present
seventy-two members, representing fifty towns. A committee was appointed
to prepare a draft of a constitution for the new state, and recommended
to the town to choose delegates on the 23d of June, to meet at Windsor,
July 2d, to discuss and adopt said constitution. The newly-elected convention
met July 2d, and continued in session six days. It received from the committee
appointed for that purpose a copy of a constitution very similar to that
of Pennsylvania, which was read and discussed. Before it was wholly adopted,
however, alarming news of the British army in the western part of the state
was received. It was proposed at first to adjourn and leave the work in
hand unfinished; but this was providentially prevented by the sudden occurrence
of a thunderstorm. Some who were less agitated by the news from the west
side of the state suggested the great importance of finishing the work
in hand. This advice was followed, the constitution adopted, an election
ordered, and a Council of Safety appointed to manage the affairs of the
state until the government should go into operation under the constitution.
This independence Vermont pursued, asking no favors, enjoying no
benefits of the Union, and sharing none of its burdens, until March 4,
1791, when she was admitted as one of the Federal states, with the full
rights and immunities belonging thereto. Thus Vermont exists to-day --
so may she always exist!
The constitution has remained without very material alterations,
the chief being the substitution of a Senate of thirty members, appointed
to the several counties, according to population, and chosen by a plurality
of the freemen of the several counties, in lieu of a council of twelve
members chosen by a plurality of the voters of the state at large; and
in 1870 a change from annual to biennial state elections and meetings of
the legislature. The frame of government now provides for, 1st, The executive,
the chief officers of which are the governor, lieutenant-governor, and
treasurer, all of whom are elected biennially, by the freemen of the state.
2d, A Senate of thirty members elected as before mentioned. 3d, A House
of Representatives, consisting of one member from each organized town,
elected by the freemen thereof. 4th, A judiciary, the officers of which
are elective, the Judges of the Supreme Court (who are also chancellors)
by the Senate and the House of Representatives, in joint assembly, the
assistant Judges of county courts (a Judge of the Supreme Court presides
in each County Court), Judges of the probate courts, sheriffs, state's
attorneys, and high bailiffs by the freemen of the respective counties;
and justices of the peace by the freemen of the several towns. The state
election is held in September, biennially, and a majority of all the votes
cast is required to elect every officer, except senators and other county
officers, including in the latter justices of the peace elected by the
several towns; but in March the freemen of each town meet for the transaction
of public business of the town, and the election of town officers. Every
term of town office is limited to one year, or until others are elected,
and all town elections are therefore annual. The governor's power of appointment
is very limited, embracing, ordinarily, his secretary and military staff
only; but he has power to fill any office created by law, where the appointment
is not fixed by the constitution or statute, a case which has rarely occurred;
and also to fill any vacancy occurring by death, or otherwise, until the
office can be filled in the manner required by constitution or laws. By
recent statutes the governor may nominate, subject to approval by the Senate,
various officers. The heads of the various state bureaus (except treasurer)
and generals of divisions and brigades are elected by the Senate and House
in joint assembly, -- the former officers biennially and generals when
vacancies occur. The General Assembly meets in the even years, on the first
Wednesday of October. The first officials elected, in 1788, were as follows:
Thomas CHITTENDEN, governor; Joseph MARSH, lieutenant-governor; Ira ALLEN,
treasurer; T. CHANDLER, secretary of state; Nathan CLARKE, speaker; and
Benjamin BALDWIN, clerk.
The division of the state into counties, and the formation of Washington
county, is described in the "Bench and Bar," following the roster
of officers in the civil war.
TOPOGRAPHY.
The surface of Washington county is varied by high mountains, gentle
hill slopes, and charming picturesque valleys. Camel's Hump lies on the
western border, and rears its rocky crest more than 4,000 feet above the
sea - the highest except Mt. Mansfield in the state. It is the best defined
and most conspicuous peak of the Green Mountains. It is conspicuous from
most parts of the county and the whole valley of Lake Champlain. It is
accessible from Huntington, but is usually ascended from Duxbury. The views
obtained at the summit in extent and "scenic beauty" are unsurpassed, and
amply reward the tourist for his labor in making the ascension.
Other heights from which magnificent views are obtained are Mt.
Hunger, 3,648 feet above "Old Ocean," on the line between Middlesex
and Worcester, and Bald Mountain in Northfield, 2,636 feet high. The Winooski,
or Onion, river and its numerous branches contribute their utility and
beauty to the territory, and the eastern part of the county is adorned
with numerous gems of lakes and ponds. The town of Woodbury alone has twenty-three.
The Winooski, the longest river in the state, rises in Cabot, receives
an important tributary in Marshfield, flows in a southwesterly direction
to Montpelier, and thence nearly northwest, which course it continues until
it discharges its waters into Lake Champlain about five miles north of
Burlington, and drains an area of about one thousand square miles. Its
principal tributaries in Washington county are Kingsbury Branch, Stevens
Branch, Dog river, Worcester or North Branch, Mad river, and Waterbury
river.
There is indubitable evidence that the valley of the Winooski, from
Montpelier to Bolton falls, was once the bed of a lake all along this valley
between the places named. The rapid mountain streams would deposit a sediment
in the still waters of this lake, which would settle and form terraces,
as at Waterbury village. Mr. C. N. ARMS informed the writer that in digging
his well in that village he encountered a birch tree about twenty inches
in diameter and well preserved, nineteen feet below the surface of the
ground. The question is, how came it there? The region of Bolton falls
"is an excavation through the back-bone of the Green Mountains," says Professor
HAGAR. In Zadoc THOMPSON's Gazetteer of Vermont, Part III., page
197, is the following description:
"The channels which have been worn in the rocks by
this river are a great curiosity. One of these between Middlesex and Moretown
is about eighty rods in length, sixty feet in width, and thirty feet deep;
the rock appearing like a wall on each side. Another of these channels
is between Waterbury and Duxbury, four miles below Waterbury village. Its
depth is about one hundred feet, and the rocks on the south side are perpendicular.
The rocks have here fallen into the chasm and form a natural bridge, which
is crossed by footmen at low water. Among the rocks here are also several
curious caverns. Holes also of cylindrical form are here worn into the
solid rocks several feet in depth. There is abundant evidence existing
that above this place a large pond formerly existed, whose waters were
drained off by the wearing down of the channel." |
GEOLOGICAL.
The science of geology is ever an interesting study, and as related
to this county it is exceedingly so; for here the record of the changes,
or "footprints," that time has left in the succeeding ages since
the earth was created, are numerous and well developed. Before mentioning
the several rocks that enter into the formation of the territory, however,
it may not be considered superfluous to briefly note the fundamental principles
of the science.
Among men of science it has become the common, if not prevailing,
opinion that in the beginning all the elements with which we meet were
in an ethereal or gaseous state-that they slowly condensed, existing for
ages as a heated fluid, by degrees becoming more consistent-that the whole
earth was once an immense ball of fiery matter-that, in the course of time,
it was rendered very compact, and at last became crusted over, as the process
of cooling gradually advanced, and that its interior is still in a molten
condition. Thus, if the view suggested be correct, the entire planet in
its earlier phases, as well as the larger part now beneath and within its
solid crust, was a mass of molten fire, and is known to geologists as elementary
or molten. Following this came another age, in which the molten mass began
to cool and a crust to form, called the igneous period. Contemporaneous
with the beginning of the igneous period came another epoch. The crust
thus formed would naturally become surrounded by an atmosphere heavily
charged with minerals in a gaseous or vaporous condition. As the cooling
advanced this etherealized matter would condense and seek a lower level,
thus coating the earth with another rock. This is named the vaporous period.
At last, however, another age was ushered in, one altogether different
from those that had preceded it. The moist vapor which must of necessity
have pervaded the atmosphere began to condense and settle, gathering into
the hollows and crevices of the rocks, until nearly the whole surface of
the earth was covered with water. This is called the aqueous period. As
these waters began to recede and the "firmament to appear," the
long winter that intervened, while the sun was obscured by the heavy clouds,
would cover the earth with mighty ice-floes and glaciers, forming a drift
or glacial period
A great difference also exists in the consolidation and structure
of the rocks thus formed. The very newest consist of unconsolidated gravel,
sand, and clay, forming alluvium. A little farther down we come to the
tertiary strata, where are same hardened rocks and others more or less
soft. Next below the tertiary is found thick deposits, mostly consolidated,
but showing a mechanical structure along with the crystalline arrangements
of the ingredients. These are called secondary and transition. Lowest of
all are found rocks having a decidedly crystalline structure, looking as
if the different minerals of which they are composed crowded hard upon
one another. These rocks are called metamorphic, hypozoic, and azoic.
The principal portion of the rocky of this territory is azoic, and
known as talcose schist and calciferous mica schist, though there are several
beds and veins of other formations. Talcose schist proper consists of quartz
and talc, though it has associated with it, as integral parts of its formation,
clay slate, gneiss, quartz rock, sandstones, and conglomerates, limestones
and dolomites: Talcose schist underlies a large portion of the towns of
Worcester, Middlesex, Montpelier, Duxbury, Waterbury, Moretown, Fayston,
Waitsfield, Northfield, Roxbury, Warren, and the west part of Berlin, Barre,
and East Montpelier. Calciferous mica schist underlies a large part of
the eastern portion of the county. Granite abounds in Berlin, Barre, Plainfield,
Marshfield, Cabot, and Woodbury. A broad belt of clay slate extends through
Roxbury, Northfield, Berlin, Montpelier, East Montpelier, Calais, and Woodbury.
Beds of serpentine and steatite exist in Roxbury, Warren, Waitsfield, Moretown,
Northfield, Duxbury, and Waterbury, also beds of copper and iron pyrites
in Waterbury.
Gazetteer
Of Washington County, Vt. 1783-1899,
Compiled
and Published by Hamilton Child,
Edited
By William Adams.
The Syracuse
Journal Company, Printers and Binders.
Syracuse,
N. Y.; April, 1889.
Pages 5
- 13
Transcribed
by Karima Allison 2003 |