The following is the first chapter of my culminating study on Vermont Independence. It covers the geological formation of the Vermont landscape through the boarder disputes that predated the American Revolution ending which the Westminster Massacre in 1775. Because the program I attended focused on original content, much of my writing on the Green Mountain boys is omitted as it was covered by studies in earlier semesters.
Chapter
1
A
Pre-Vermont History
In
June of 1770, Ethan Allen rode to Albany, New York, to represent John
Carpenter, an evicted settler from Bennington in the so-called New
Hampshire grants, the disputed land that lay north of the
Massachusetts Colony west of the Connecticut River across the Green
Mountains to Lake Champlain. Through, poor cartography, unclear
charters, as well as opportunism and outright land snatching, the
territory that was to become Vermont was parceled with conflicting
deeds issued by both New Hampshire and New YorkJohn Tabor Kempe, the
former attorney general of the colony of New York, represented
fellow attorney and real estate operator John Duane. Duane had
considerable interest in the grants and had what were called “writs
of ejectment” issued to New Hampshire deed holders. The Albany
courts sided with the New York deed holders based on a 1764 ruling of
the Orders in Council. The following day Kempe and Duane caught up
with Allen at Stephen Fay's Catamount Inn in Bennington to offer him
a substantial plot of prime real estate under New York patent if he
were to drop the grant's cause. When he refused, Kempe threatened,
“Be advised, the people of the grants would do well to make the
best terms with the rightful New York land lords.” Allen replied
with words that have echoed through Vermont's history and have become
its rallying cry “The gods of the hills are not the gods of the
valleys” (Jellison 38). Allen's intent was to let these “Yorkers”
know that the people of the grants were not to easily bought. Having
worked hard to build and obtain what little they were able, they were
not quick to relinquish it. This was a direct threat as Ethan Allen
continued by saying “If you accompany me to the hills of
Bennington, the sense will be made clear.” From there they could
see that a group of armed settlers, later known as the “Bennington
Mob” and the predecessor to the Green Mountain Boys, was assembling
in the streets of Bennington, ready to defend the western front. With
these statements Ethan Allen showed a not-so subtle disregard for
popular and standard religious sentiment by implying that there may
be more than one almighty God with a capital “G,” effectively
denouncing
the monotheistic notions held by most Puritan people of colonial New
England. Allen was known for his disregard for popular and
contemporary religious views having himself been evicted by special
town meeting from Northampton, Massachusetts, for such “insolence.”
By
invoking the “gods of the hills” he implied that the geography
and physical landscape of the Green Mountains are at the core of the
people's resolve, that the hills shape and carve people's character.
The terrain is a little bit harder to traverse and the soil even
harder to work. The winters are a bit more severe and last longer
than in the lowlands. Survival was a daily concern for early settlers
of the grants. These are among the core reasons Vermonters are
diligent and durable.
The
gods that formed and raised the Green Mountains to a maximum height
of over 12,000 feet did so through a series of major tectonic events.
The first, over a billion years ago, the Greenville Orogeny, was a
collision of the North American and Eurasian plates creating the
Adirondack Mountains and the bedrock on which the Green Mountains
would rest. When the plates receded 575 million years ago, the
Iapetus Ocean opened up and covered what would be Vermont. Evidence
of this ancient ocean can be found on Isle le Motte in Lake
Champlain, which is among the world's oldest coral reefs and has
fossils dating to this period. As the plates receded, taking several
million years, the seam between the plates ruptured causing volcanic
activity that created a massive chain of islands called the Taconic
Island Arc which divided the ocean. Soon after in geological terms
(50 million years), the Taconic Island Arc collided and fused with
the North American Continent and pushed the Green Mountains to
heights the East Coast hasn't seen since. With this event the gods
had something special in store for the land that was to become
Vermont. When the Taconic plate collided with early Green Mountains
the heat and pressure turned shale into slate and limestone into
marble. This is evidenced by the large veins of slate from Fair
Haven, Vermont, that continue through New York and Pennsylvania as
well as Vermont’s famed “Marble Valley”.
The
force of the collision between the Taconic Island Arc and the
proto-North American plate was so great that the eastern edge of the
Taconic Islands snapped from the oceanic crust. As the proto-North
American plate continued to move eastward the ocean's plate began to
subduct, and volcanic activity began once again, this time creating a
series of granite domes in Vermont and New Hampshire. About 400
million years ago a small continent in the east called “Avalon,”
thought to be part of the African plate collided with the proto-North
American plate, which began the massive mountain-building cycle known
as the Acadian Orogeny. After the Acadian Orogeny the plates
continued to subduct and tighten to form the well-known
supercontinent of Pangaea. During the Allegheny Orogeny, the
Appalachian Mountains from Alabama to Pennsylvania were formed. The
instability of Pangaea caused major rifting and eventually the
massive continent began to break apart, and over a period of 180
million years the plates drifted into their present place (Sherman et
al. 3). After the gods of the hills were done building their massive
peaks it was time for the ice to do its part. No fewer than four
glacial periods have occurred since the last mountain-building cycle.
These mile-thick sheets of ice repeatedly scraped, gouged, and
blunted the landscape and ground the once giant mountains down to the
relatively small peaks they are today. As these glaciers began to
melt, rivers formed under the sheets of ice and deposited boulders
and fragments. These fragments can still be seen in the many stone
walls lining dirt roads. Hikers may happen upon these walls in new
forests, the Around 13,000 years ago glacial-melting created Lake
Vermont where present-day Lake Champlain is. The glacier to the north
dammed water draining into the lake and caused it to swell over 700
feet higher than the present lake. It engulfed all of Lake George and
the northern Hudson Valley. The lake also entirely covered the Otter
Creek region up to Rutland, and the Missisquoi region as far as
Memphremagog. It also extend deep into the river valleys of the
Winooski to Montpelier and the through the Waterbury reservoir to
Stowe, and the Lamoille as far as Hyde Park (Klyza 38).
When
the glacier began to melt, Lake Vermont drained out through the St
Lawrence River and left a body of water that was lower than the
present lake. When the glacier melted completely the ocean levels
rose while the plate, crushed by glacial ice, was hundreds of feet
lower than at present and the Atlantic reached Champlain through the
St. Lawrence gulf mixing saltwater and creating what would become
known as the Champlain Sea. Although not as big as Lake Vermont, the
Champlain Sea left its own distinct marks. Relics of the Champlain
Sea are found in several places throughout the Champlain Valley in
countless fossils, most notably that of a whale, found while laying a
railroad bed near Charlotte in 1848.
Over
time the plate recovered, rose above sea level, These events of
tectonics, glacial drifts, and receding seas have shaped Vermont into
its six distinct physiographic regions. The Green Mountains run north
to south for the length of the state and split into three separate
ranges. They include hundreds of peaks up to the tallest at the north
peak of Mount Mansfield at 4,392 feet. The Taconic Mountains in the
southwest of the state are a source of limestone and slate and
provide a seemingly impregnable barrier between the Green Mountains
and the Hudson Valley. The Valley of Vermont is nestled between the
Taconic and Green Mountains, and apart from being a great source of
limestone and marble, it also supports many plants that are not
commonly found in New England. The Champlain Valley gives Vermont its
only real fertile plain as well as a variety of New England fish. The
Piedmonts are just what they translate into, foothills. This region
covers most of the eastern side of the state as part of the
Connecticut River watershed. The last region is the Northeast
Highlands, 600 square miles of primarily spruce and some of the
foothills of the White Mountains
The
gods stayed quiet in the region for a while after the glacier
retreated, tending only to the flow of rivers and the return of life.
The glacier had washed clean the surface of the mountains awaiting
the bacteria and angiosperms that would inhabit them and start life
anew. Elk, caribou, mammoth, and mastodons used to roam these hills,
but as the temperatures rose and the waters receded they moved on.
When the waters dropped to nearly their current depths the forest
diversified, bringing in the type of landscape we see today.
Vermont
has four primary watersheds. The Connecticut River runs nearly the
entire length of the state along its eastern border with New
Hampshire. The river originates from lakes in northern New Hampshire
but swells as it carries the drainage from the eastern slopes of the
Green Mountains and the foothills in New Hampshire, divides
Massachusetts and Connecticut, and empties into the Long Island
Sound. The Champlain Valley receives most of the drainage from the
western slopes of the Green Mountains and the eastern Adirondacks,
and drains northward through the Richelieu River and into the St.
Lawrence River. In the southwest Taconic Mountains, the waters of the
Battenkill and the Willomac Rivers drain into the Hudson River and
make their way to the Atlantic through New York's Lower Bay. The
fourth, and sometimes forgotten, watershed carries a few small rivers
north through Lake Mempremagog into the St. Francis River and to the
St. Lawrence River. These rivers and lakes would not only determine
the flow of people and commerce in and out of the region, they would
inevitably shape the future of Vermont in its relationships with
neighboring states and Canada.
By
the time of colonial exploration Vermont was inhabited by the Eastern
Algonquin Indians, primarily Abenaki, who used the Green Mountains as
a hunting ground, and took fish from Lake Champlain. A number of
other tribes, including Mahican, some of the southern Algonquian
tribes of Massachusetts, and the Iroquois tribes of upstate New York,
knew these hills and used them for hunting, fishing, and as a
crossing route from the St. Lawrence River to the Atlantic Ocean,
with very few permanent native settlements, mostly in the Champlain
Valley.
Early
Paleoindians likely arrived in Vermont about 11,000 years ago after
the last glacier receded. Paleoindian sites are consistent with the
eastern reaches of the Champlain Sea, suggesting that they were
present on the banks of the sea around 6,900 years ago. Evidence of
villages in Vermont can be found as far back as the Woodland The
Abenaki's woodland ancestors were pre-agrarian, hunting and gathering
tribes. Agriculture didn't appear in Vermont until 1100-1400 C.E.
Owing to Vermont's late spring, the Abenaki had limited agricultural
produce. The advent of the bow made the Native Americans heavily
reliant on hunting. In the winter they would gather in large villages
and live off of prepared food, while men went hunting on snowshoe.
By
the time Samuel de Champlain arrived in 1609, few native boundaries
were clear, but the lake that now bears his name was a natural
boundary between the Iroquois and Abenaki people when
sixteenth-century European explorers arrived (Klyza 31). European
exploration altered native life considerably. The natives traded furs
for manufactured cloth from Europe. When the furs became scarce the
natives were convinced to sell land in order to continue receiving
the goods to which they had grown accustomed. The Europeans also
brought disease, which nearly eradicated the native population in New
England, killing them by the thousands. Apart from the depletion of
the fur trade and new diseases, Europeans brought with them a new
kind of warfare, far more devastating than the tribal warfare the
natives were accustomed to. European trade turned into European
military alliance and the natives became entangled in a thousand year
old grudge match that migrated across the Atlantic Ocean and was now
being played out on the North American Continent.
During
the early period of American exploration the Spanish covered most of
the Caribbean, Central American and the Gulf Coast, while the English
were penetrating the Atlantic coast from Virginia to Maine. The
French, in pursuit of the Northwest Passage to India, were in control
the St. Lawrence Seaway allowing them access further inland by In
1535 Jean Cartier had explored the St. Lawrence as far up-river as
Hochelaga, present-day Montreal, but Samuel de Champlain was the
first to explore Vermont's coast. The Dutch would reach Vermont by
way of the Hudson River, while the English
explored
both the Hudson and Connecticut rivers to reach Vermont.
The
French built forts along Lake Champlain in efforts to control the fur
trade with the Abenaki. In 1666 the French built Fort Ste. Anne on
Isle le Motte, the first white settlement in Vermont. Although the
French worked their way through the lake with forts at Chimney Point
and Fort Carillon (Ticonderoga), they did not aggressively attempt to
settle Lake Champlain. The first permanent settlement of colonists
in Vermont was Fort Dummer, built in 1724 along the Connecticut River
near present-day Brattleboro. It was one of four forts the
Massachusetts Bay Company had been given royal charter to build along
the Connecticut River. The others were Hinsdale on the eastern bank
across from Dummer, Fort Hill, over looking the Great Meadow in
present-day Putney, Vermont, and Fort No. 4 in Charlestown, New
Hampshire, at which were stationed Phineas Stevens and Robert
Rogers
during the French and Indian Wars, and later General John Stark, the
hero of the Battle of Bennington.
An
important point to remember is that Vermont was never in the plans
for the American Colonies. It wasn't granted as an individual region
by any nobility. There was only a lake, a mountain range, and a river
that may have belonged to New York, New Hampshire, Massachusetts, or
even Canada. Land disputes in New England arose from simple boundary
errors that were neatly exploited. The first lands chartered in
present-day Vermont were issued by Massachusetts in 1713. These towns
lay just north of Massachusetts' current northern border, on the west
bank of the Connecticut River. The “equivalent lands” were
granted to Connecticut as compensate for land lost on a boarder
dispute near Agwam.
In
1741 Benning Wentworth became royal governor of New Hampshire at the
time that new boundary lines were established in surrounding
colonies. A 1664 grant placed the Connecticut River as the eastern
border of New York. This disputed earlier charters that placed the
border at a line twenty miles east and parallel to the Hudson River,
roughly where it is today. Massachusetts and Connecticut had
contested the Connecticut River line, but it was not resolved until
around 1725 when Massachusetts and Connecticut were given the
twenty-mile line as their western border, and the lines on the maps
began to look similar to today (Meeks 53). In 1740 the northern
boundary of Massachusetts was determined to be “a similar curve
line pursuing the course of the Merrimack River at three miles
distance on the north side thereof, beginning at the Atlantic Ocean
and ending at a point due north of a
place
called Pentucket Falls, and by a straight line drawn from thence due
west 'till it meets with his Majesty’s other governments” (Meeks
50). This put Massachusetts' northern border seven miles lower than
their Fort Dummer. At this Massachusetts gave control of the fort
over to New Hampshire. This was enough to give Wentworth an argument
that the land west of the Connecticut River to “his Majesty’s
other Governments” twenty miles from the Hudson would fall under
the jurisdiction of New Hampshire. It is assumed that Wentworth had
intended on granting land west of the Connecticut River immediately
upon ascending to his position as governor but the outbreak of King
George’s War in 1744 delayed granting and settlement in the Green
Mountain Wilderness. In November 1749, Benning Wentworth wrote to New
York Governor Tryon stating his intentions of selling New Hampshire
Grants in the Green Mountains claiming a royal commission.
I have it in command from his Majesty to make Grants of the
unimproved Lands within my Government, to such of the inhabitants and
others, as shall apply for grants for the same [. . .] The [French &
Indian]War hitherto has prevented me from making so great a progress
as [. . .] it will be necessary for me to be informed how far North
of Albany the Government of New York extends [. . .] and how many
miles to the east of the Hudson river to the northward of the
Massachusetts line, that I might govern myself accordingly. (qtd. in
Graffanino et al. 20, hereafter
referred to as Vermont Voices)
Wentworth
had chartered the first town in honor of himself long before the
letter was composed. Bennington is located between the northwest
corner of Massachusetts and the southern tip of Lake Champlain. It
seems that Benning wasn't merely crossing the line a bit but outright
reaching to his furthest extent, the twenty-mile line, in order to
grab as For the next five years grants were given and settlements
began to grow. Many of the grantees secured their grants at no money
down with the understanding that they were to build mills and pay off
the deed. Others paid for their grants in installments of pelts and
furs, all of it payable to Benning Wentworth himself. In 1754 during
the onset of the French and Indian Wars, granting ceased. Vermont was
primarily used as a military crossing. In 1761 after the war had
stopped, New Hampshire resumed granting and New York began surveying
land it thought to be its own.
In
1764 it was ruled that the Connecticut River would be the border
between New York and New Hampshire. However, this ruling gave no
decision on the validity of New Hampshire Grant holders who had
already settled and were living in the grants. New York began to
issue writs of ejectment to overlaying lands in the Grants. By the
time conflict started Wentworth became quite wealthy and had no
intention of taking responsibility for his settlements in the grants.
By 1766, after granting over 100 questionable grants, Benning
Wentworth resigned his post as governor but was replaced by his
nephew John Wentworth. During the rest of the decade conflicts arose
on the grants, mainly due to surveyors drawing lines on land already
inhabited by settlers. A number of those settlers were forcibly
evicted
from
their land. When grievances were presented to England, both provinces
were ordered to stop granting, an order both governors chose to
ignore. New York immediately established Cumberland County along the
Connecticut River and continued granting disputed land, while New
Hampshire pressed their grants north toward the Champlain
While
many people were removed from their homes, some began to take a
stand. James Breckenridge was among the first to resist eviction by
the New York authority. In October of 1769 New York surveyors,
drawing lines on his farm in Bennington, were driven off with
threats. On July 11, 1771, Sheriff Henry Ten Eyck arrived from Albany
with about 300 men to serve Breckenridge a writ of ejectment. They
were greeted by seven armed men and a couple dozen farmers inside the
main house, also armed. After a brief parley, two of his posse were
allowed on to the farm to meet with Breckenridge. By the time they
reached Breckenridge's house, as many as forty men made their
presence known along a nearby ridge overlooking the meeting. After a
brief exchange Breckenridge ordered the posse off his land and
returned to his house.Ten Eyck reconvened with the rest of the posse
and ordered a charge on the house. The charge began but quickly
collapsed. Most of the men retreated while twenty men made it to the
door and demanded entrance. The sheriff read the writ out loud and
movement
began along the ridge. He threatened to batter the door down. At
this, the forty men along the ridge took “casual bead along the
sites.” The twenty men on the sheriff’s lead retreated and
returned to Albany (source). It was at this standoff that the Green
Mountain Boys were born. They were a militia free from any
continental or royal authority, who, between 1771 and 1775, were
the
guardians of the ordinary farmers and homesteaders. Although they
would fight along side the United States during the American
Revolution, their enemy wasn’t the Crown as much as it was one cell
of authority in the royal government of New York. When the settlers
in the Grants first looked to the Royal authorities in New Hampshire
to come to their aid in the land dispute; “The people [were] heard
with patience by British authorities. . . .
The
Grants had no legitimate grievance against Great Britain before the
Revolution. The governors of New York, the land speculators of New
York, were the oppressors, not King George III” (Van DeWater 55).
As the first winds of revolution began to blow all over the colonies,
Britain became a common enemy. The next four years would see a period
of relatively nonviolent rebellion in many parts on the western side
of the state. In most cases the armed militia was used to drive off
New York surveyors. The punishment for Yorkers disputing land was the
application of the “beech seal” in which the accused would have
his pants removed and whipped with a switch from a beech tree, and be
banished from Vermont. In another case at the Catamount Tavern in
Bennington, Dr. Samuel Adams was speaking out against the actions of
the Green Mountain Boys. He was tied to a chair and hoisted above the
entrance to the tavern for more than two hours. These acts were
carried out for purposes of propaganda rather than physical harm.
With
few exceptions the eastern side of the state was safe from the
oppressive arm of the royal New York government in Albany. Most
people along the Connecticut River owned New York land. Of those who
bought New Hampshire deeds, many simply forfeited their deeds and
repurchased their land under New York patent. This worked for those
with just a few acres, but for those with much larger tracts, often
acquired on credit, the cost was unmanageable. As rebellious tones
grew louder, royal governments acted more harshly toward dissent. In
October, 1774, Lieutenant Leonard Spaulding was charged with high
treason and jailed for saying that the king had broken his coronation
oath by signing the Quebec bill, which deprived the people of the
province the right to assemble, the right to a jury trial, and in
civil cases replaced British law with French law. Spaulding was
later freed from jail by a group of sympathetic local citizens (Hall
202).
The
royal authorities of New York in Cumberland County were set to hold a
session of court in Westminster on March 13, 1775, to settle
unresolved land claims. A warning was sent to Colonel Thomas Chandler
in Chester to suspend the court session for fear that an armed posse
would cause uneasiness among the people. Chandler assured the group
that there would be no arms present and agreed to do no further
business than one case, which involved a murder that had to be tried.
By the time the court officials, accompanied by and armed posse,
arrived at Westminster, a mob of nearly 150 militia men, led by
Lieutenant Leonard Spaulding, had assembled to block entrance to the
court and prevent any proceedings from going on. After a being
refused entrance to the court, the posse retreated to a local pub.
After a few hours they returned to the courthouse. The mob occupying
the courthouse dwindled as night had fallen. The posse demanded
entrance and fired shots above the door. The mob inside returned fire
over the heads of the posse. At that the posse unloaded a steady
volley of fire into the courthouse instantly killing William French,
a nineteen year-old militia member from Brattleboro, and wounding
several others, including Daniel Houghton from Dummerston, who would
die
Upon
realizing that a man had been killed in the melee the posse fled from
the scene. They were pursued by the militia and rounded up within the
night, brought back to the courthouse (when they were finally let in)
to stand trial for the murder of William French. A mock trial was
conducted and the offenders were convicted to banishment from
Vermont. The death of William French would remain a symbol of New
York and British oppression. His grave in the cemetery in
Westminster, just across from where the courthouse once stood bears
this epitaph:
In memory of William French,
Son of Mr. Nathaniel French,
who was shot at Westminster, March ye 13, 1775,
by the hands of cruel Ministerial Tools of George ye 3rd
in the Court house, at a 11 a'clock at night,
in the 22d year of his age.
Here William French his Body lies,
For Murder, his Blood for Vengenance cries,
King George the Third his Tory Crew,
Tha wich a bawl his head Shot threw,
For Liberty and his Country's Good
Lost his Life, his Dearest blood.
On
April 11, at a convention in Westminster, it was voted “that it is
the duty of the inhabitants to wholly renounce the resist the
administration of the government of New York 'till such a time as the
lives and property of these inhabitants may be sucured by it”
(Robinson 99). In less than ten days the battle of Lexington began
and the American colonies were engaged in war. Vermont would spend
the next few years sorting out where its allegiance would lie while
there was only a clear enemy and no clear allies.