GAZETTEER
OF
CHITTENDEN
COUNTY, VT
Very aptly and truthfully has it been said that, "history is a bridge
connecting the now with the past." It is indeed a bridge, over which we
may pass to the hallowed days of which we all love to hear, -- a passage
whose every plank is the record of some noble life or deed, urging us to
emulate their virtues, or, at other points, warning us from the errors
and vices into which many have fallen. It is our purpose, then, to pass
with the reader over this bridge, connecting the prosperous present with
the toil laden past of Chittenden County, involving also a cursory glance
at the history of its parent, the State. A hasty journey it must necessarily
be, however, -- a mere superficial glance at the principal points of interest
on the way, in which it shall be our endeavor to present the truth, and
to preserve many, or at least some, facts which would otherwise soon become
enshrouded in the oblivion that surrounds but too many of the heroic deeds
and sacrifices attending the conception and birth of the old democratic
State of Vermont, a territory that has no parallel in its peculiar beauties,
revealed in the variety, the majesty and exquisite loveliness of its scenery,
and whose history establishes a just claim to its title of “The Classic
Ground of America."
There are good reasons for believing that the first civilized people
who visited New England, were a colony of Norwegians, or Northmen, who
emigrated thither, according to the original Icelandic accounts of their
voyages of discovery, as follows:
"In the
spring of A. D. 986, Eric the Red, so named from the fact of his having
red hair, emigrated from Iceland to Greenland, and formed a settlement
there. In 994, Biarne, the son of Heriulf Bardson, one of the settlers
who accompanied Eric, returned to Norway, and gave an account of discoveries
he had made to the south of Greenland. On his return to Greenland, Leif,
the son of Eric, bought Biarne's ship, and, with a crew of thirty five
men, embarked on a voyage of discovery, A. D. 1000. After sailing some
time to the southwest, they fell in with a country covered with a slaty
rock, and destitute of good qualities, and which, therefore, they called
Helluland (slate-land). They then continued southerly until they found
a low flat coast, with white sand cliffs, and immediately back, covered
with wood, whence they called the country Markland (wood land). From here
they sailed south and west, until they arrived at a promontory which stretched
to the east and north, and sailing round it turned to the west, and sailing
to the westward, passed between an island and the mainland, and entering
a bay through which flowed a river, they concluded to winter there. Having
landed, they built a house to winter in, and called the place Leifsbuthir
(Leifs booths). Soon after this, they discovered an abundance of vines,
whence they named the country Vinland, or Wineland, which corresponds with
the present country at the head of Narragansett Bay, in Rhode Island." |
Subsequent to this came the discoveries of Columbus, in 1492; the
English discoveries in 1497, followed, during the same year, by the Portuguese;
the Spanish, in 1506, and finally came the French, in 1524, who subsequently
discovered the Gulf and River St. Lawrence, and first began a colony upon
it, whence they soon spread to the heart of the country, to which they
had an easy means of access by way of the great lakes, whose waters head
within a few miles of the tributaries of the Mississippi, which flows across
half the continent to the Gulf of Mexico. In a few years they had explored
this vast region, and established among the savages missions and trading
posts, first in the forests of Canada, than in the West, and finally in
New York and in the territory included within the present State of Vermont.
In the meantime England had been pushing her explorations and discoveries;
but the French laid claim to nearly the whole country, confining the English
to a narrow strip of land along the Atlantic coast, thus transplanting
the jealousies and rivalries which had long made them enemies in the Old
World, to the New Continent. The French sought the alliance of the Indian
tribes, and years of warfare followed, in which, however, the English at
last succeeded in gaining possession of a large amount of the land. The
first hostilities between them originated on William's accession to the
throne of England, in 1689, which terminated in the peace of Ryswic, in
1697. Queen Anne's war, so called, commenced in 1702, and continued to
the peace of Utretcht, in 1713. The third controversy was declared by George
II. in 1744, and continued until the preliminaries of peace were signed
between France and England, at Aix la Chapelle, in 1748. The last conflict
between these powers, anterior to the American revolution, was formally
declared by Great Britain, in 1756, and was reciprocated the same year
on the part of France, and finally terminated by the capture of Montreal,
in September, 1760, when the whole Province of Canada was surrendered to
Great Britain.
During this period of the French wars, the territory now included
within the county was the chief point of rendezvous for the French and
their Indian allies, in their hostile excursions against the English settlements
in the valley of the Connecticut. It was through here they generally led
their captives and carried their plunder, their usual route both in going
and returning being along Missisquoi Bay and Winooski River, crossing the
short carrying place between the river and Mallett's Bay. It was along
here the suffering captives from Deerfield, in the dead of winter, in 1704,
were led on their way to Canada; and here also was led the lad Enos STEVENS,
son of Capt. Phineas STEVENS, in 1748; and on the east shore of Missisquoi
Bay, the year previous, Mrs. Jemima HOWE found her son Caleb perishing
with hunger. Early skirmishes took place, too, within the territory, --
one as early as 1709, on the Winooski, in which Liet. John WELLS and John
BURT were killed, followed by another at the mouth of the river, where
several of the French and Indians were killed in turn. Upon this river,
also, Capt. John BARNET lost his life in a skirmish, in 1776. Indeed, the
whole territory teems with tales and anecdotes of those days of bloodshed.
These early wars, however, led to the first settlement of the State
by civilized people. Samuel CHAMPLAIN is supposed to have been the first
to visit the territory, having sailed up the lake he discovered, and which
has since borne his name, in 1609. In 1664, M. de Tracy, then Governor
of New France (the French possessions in America.), entered upon the work
of erecting a line of fortifications from the mouth of the Richelieu (Sorel)
River into Lake Champlain. The first year he constructed three forts upon
the river, and the next spring, 1665, he ordered Capt. de LA MOTTE to proceed
up Lake Champlain and erect another fortress upon an island which he designated.
It was completed that same year and named Fort St. Anne, and afterwards
it was called Fort La Motte, from the name of its builder, and which in
the end gave the name to the island on which it stood. The remains of the
fort are now to be seen, and the island still bears the name. In 1690,
a fort was built by Capt. de Narm, [In the Doc. Hist. of New York, this
name is given as de Warm.] at Chimney Point, in Addison County, about which
a thriving settlement soon sprang up; but it was not until 1724, at Fort
Dummer, that the first permanent settlement was commenced, and the garrison
of this fort were for several years the only white inhabitants of the territory.
After the close of the last French war, in 1759 '60, the settlement
of the country rapidly increased, as their old enemy, Canada, had been
transformed from a hostile to a friendly neighbor. Township charters were
rapidly granted by New Hampshire, under command of King George III., to
whom the inhabitants were only nominally subject, however, but obeyed only
the decrees of their own committees and conventions. At one of these conventions,
January 15, 1777, the New Hampshire Grants were declared to be an independent
State, "by the name, and forever hereafter to be called, known, and distinguished
by the name of New Connecticut, alias Vermont, etc." The latter name, derived
from the French verd mont, or Green Mountains, it still retains, and which
has gathered about itself, through all the vicissitudes which its sons
have passed, a halo of glory that shall pass away only with the demise
of Time. Such, briefly, is the outline of Vermont's history.
On February 11, 1779, the State was divided into two counties, the
Green Mountains forming the dividing line, the portion on the east being
called Cumberland, and that on the west Bennington County. Each county
was divided into two shires, that on the east into Westminster and Newbury,
and Bennington and Rutland on the west. This division of counties remained
till the extra session of the legislature, in February, 1781, when the
county of Rutland was incorporated from Bennington, and Windsor and Orange
Counties were incorporated from Cumberland, and the name of Cumberland
altered to Windham. Rutland County in turn extended through to the northern
line of the State for a period of four years, eight months and five days,
during which time the courts were held at Tinmouth. The State, then, on
October 18, 1785, dismembered the old county, incorporating from it a new
county, called Addison, which in turn extended to the north line of the
State, and made the towns of Addison and Colchester half shires. But the
connection of Chittenden with Addison County only continued for the term
of two years, and Colchester had not the honor of holding the courts of
that county but one term. Before the next stated term, at Colchester, the
county of Chittenden, named in honor of Thomas Chittenden, the first governor
of Vermont, was set off from Addison and incorporated into a distinct county,
October 22 1787.
* As an
error has crept into a great many local works, relative to the date of
this incorporation, we quote the following from Deming's Vermont Officers,
which clears up the apparent mystery: "Zadock Thompson, in his history
of Vermont, says, that Chittenden County was incorporated October 22 1782,
and Addison County February 27, 1787. This is a mistake as to both counties,
as will be seen by the following extract of a letter from Mr. Thompson
to a friend, who had addressed him on the subject: `While in Montpelier
a few days since, I was induced, by your suggestions, to examine the manuscript
acts in the office of the Secretary of State, and I there found that Addison
County was incorporated October 18, 1785, and that Chittenden County was
incorporated October 22, 1787.'" |
It then embraced all the territory between the north lines of Ferrisburgh,
Monkton, Bristol, Lincoln, and Warren, and the Province line, and was bounded
on the west by the west line of the State, which followed the deepest channel
of the lake, passing east of the Four Brothers, and west of Grand Isle
and Isle La Motte, and on the east by the west lines of Northfield, Montpelier,
Calais, Woodbury, Hardwick, and Greensborough, to the northwest corner
thereof, and then in the most direct course on town lines to the north
line of the State. But the population and business of the county increased
to such an extent that it soon became necessary that its turn should come
to be reduced in territory; and on November 5, 1792, a new county on the
north was incorporated, by the name of Franklin. The line that separated
Chittenden from Franklin County commenced "on the west line of Orange County
[as then established,] at the northeast corner of Worcester; thence westerly
on the north line of Worcester, Stowe, Mansfield, Underhill, Westford,
and Milton, to the waters of Lake Champlain; thence across to the north
of South Hero by the deepest channel between that and North Hero; and thence
on the west line of the State." Still further deductions, however, have
been made from the original limits: October 20, 1794, Starksboro was annexed
to Addison County; November 9, 1802, the county of Grand Isle was formed,
and South Hero and adjacent islands were set off to form a part of that
county. In addition, the county of Jefferson (now Washington) was incorporated
November 1, 1810, and to form a part of which, the towns of Mansfield,
Stowe, Waterbury, Duxbury, Fayston, Waitsfield, Moretown, Middlesex, and
Worcester, were taken from Chittenden. In 1839, the western part of the
town of Mansfield was annexed to the town of Underhill, and re-annexed
to the county of Chittenden.
Thus the county is situated at the present time, lying between lat.
44° 7' and 44° 42', and between long. 3° 41' and 4° 14',
bounded north by Franklin and Lamoille Counties, east by Washington and
Lamoille, south by Addison, and west by the deepest channel of Lake Champlain,
with an average length from north to south of about twenty six miles; and
from east to west, including the waters of the lake, of twenty three miles,
containing an area of about Sao square miles, divided into fifteen townships
and one city, in addition to Buel's Gore.
In surface, the county is diversified by lofty mountains, deep gorges
and ravines, gentle acclivities, wide spread verdant valleys, rivers, lakelets
and brooks, affording a landscape that is not only unexcelled in Vermont,
but which vies with many far more pretentious localities in foreign lands.
Taken together with its environs, it forms a scene upon which Nature has
lavished her treasures of beauty "with a full and unwithdrawing hand."
On the eastern part of its territory the Green Mountains rear their rocky
crests with a sharply defined contour, Mansfield and Camel's Hump cleaving
the clouds at an altitude of 4,329 and 4,083 feet respectively, the highest
peaks in the range, while the western part of the territory lies upon the
Red Sandrock chain, one of the four divisions of mountain systems in the
State, having a gradual slope on the eastern side, and a bold, rugged escarpment
on the western.
The principal streams are the rivers Winooski or Onion, Lamoille,
La Plotte, Brown's and Huntington. The Winooski, one of the largest rivers
in the State, enters near the center of the eastern line of the county,
flows a westerly course and falls into the Champlain between Burlington
and Colchester, thus completing its course of seventy miles, dung which
it waters 970 square miles of territory, and affords sites for unlimited
mill power. Nature, circumstances, and historical lore have combined in
rendering this stream one of peculiar interest, sufficient at least for
it to merit amore euphonious cognomen than the antiscorbutic "Onion," consequently
we have dropped it in this work. A controversy has long existed relative
to the derivation of its name, the popular theory being that Winooski is
an Indian name, composed of two words in the Abinaqui, or Algonquin tongue,
winoos, onions, or leeks, and ki, land, so that its literal signification
is land of onions. But as there are at least six different styles of authography
used by different writers, we cannot understand why they should not affect
the roots of the word According to a French map of 1732, the river is called
Ounousqui. In the letters of John A. GRAHAM, published at London, in 1797,
Mr. GRAHAM gives the following account of the naming of the river "Onion:"
"A Mr. Peleg SUNDERLAND, [who was also appointed by the Grand Committee,
at Bennington, as guide to Maj. John BROWN, in 1775, on his mission to
Canada to treat with the Indians respecting the approaching war,] in 1761,
while hunting for beaver on this stream, lost his way, and was nearly exhausted
with fatigue and hunger, when a party of Indians fortunately met him, and
with great humanity, relieved his wants and saved him from perishing. Their
provisions were poor; but what they had they freely gave, and their kindness
made amends for more costly fare. Their whole store consisted of onions,
and Mr. SUNDERLAND then gave the stream, near which he was so providentially
preserved, the name of Onion River, which it has retained ever since."
During the early French colonial wars it was called French River. But so
much for this; we have at least, we think, shown good cause for dropping
the vegetable portion of its name. The alluvial flats along its valley
are narrow until the river has passed the western range of the Green Mountains,
when they become broad and fertile. Its rocky gorges, etc., are spoken
of in connection with the sketch of Burlington, so we will omit their further
notice at this point.
Bolton Falls, on this stream, in the eastern part of the County,
are well worth visiting. They form a wonderful evidence of the mighty agency
of water, for an ordinary observer cannot fail to discover that the high
bluffs of rock on either side were once united, and formed a barrier through
which the stream has gradually worn its deep and narrow channel. The contemplative
mind at once reverts to the time when this barrier existed, and beholds
a long and narrow lake extending up the valley to Montpelier, and discovers
the reason why the streams emptying into the head of this lake should,
in the still water, deposit the sediment forming the numerous terraces
that are found in different portions of its valley. In the tranquil waters
of this lake the sediment brought down in the floods of the different streams
emptying into it, would settle at the bottom and partially fill it up.
Upon the opening of the rocky barrier, like the breaking away of a flume
or a portion of the dam of a mill pond partly filled with sediment, the
running stream would sweep down a portion of this sediment, by cutting
a channel through it, either in the center, leaving portions at each side,
or upon one side and leaving the other remaining. Thus the smoothly rounded
racks that project from the sides of the valley, as well as the striated
ones near the bed of the river, bear unmistakable testimony that by some
abrading agency, in which water played a conspicuous part, the rocks have
been worn down so as to give greater width to the valley.
The Lamoille River is not as large as the Winooski, nor quite as
long; yet it has, in a lesser degree, the same wild, picturesque channel,
and affords many excellent specimens of terraces. It rises in Greensboro,
from the union of several streams (formerly from Runaway Pond), runs southwest
to Hardwick, when it turns northwesterly, passes through the middle of
Lamoille County, the southern part of Franklin County, and finally joins
Lake Champlain in the northwestern part of this county, in the town of
Milton. It was discovered by Champlain, in 1609, and called by him la Mouette,
the French for mew, or gull, a species of water fowl, which were very numerous
about the mouth of the stream. In Mr. Anger's map of his surveys, in 1732,
it is called la riviere a la Mouelle, probably a mistake in the engraver
in not crossing his t's. "Thus," says Mr. Thompson, "to the mere carelessness
of a French engraver are we indebted for the smooth, melodious sounding
name Lamoille."
Brown's River, so named from Joseph BROWN, an early settler upon
its banks, in the town of Jericho, originates in Underhill and thence flows
a southwesterly course through the northern part of Jericho, into Essex,
where it turns north and passes through Westford into Fairfax, in Franklin
County, and there unites with the Lamoille. It is twenty miles in length.
Huntington River rises in the southern part of Huntington, and after
a rapid, serpentine course over a gravel or stony bottom for about twenty
miles, empties into the Winooski, in the town of Richmond. This stream,
from the many specimens of terraces its valley consists, its rocky gorges,
etc., is called one of the most interesting tributaries of the Winooski.
The La Plotte is a small stream, only fifteen miles in length, rising
in the southeastern part of Hinesburgh, and flows a westerly course through
a portion of Charlotte and Shelburne, into the head of Shelburne Bay. As
the interesting tradition relative to the origin of its name is spoken
of in connection with the Shelburne sketch, we will defer further mention
here. These are the principal streams of the county, though there are many
of almost equal importance, affording many mill sites, and ample irrigation
to the soil.
No inland lakes of importance are found, though there are several
small ponds, Shelburne and Hinesburgh in the southern part of the county
being the largest. But the unequaled Champlain lies upon its western border,
stretching north and south as far as the eye can reach, while directly
opposite, on its western shore, the blue Adirondacks spread far into the
interior at various points projecting their jagged spurs into the lake,
and often presenting lofty headlands, waving with forests or frowning in
bleak masses of naked granite, while wide fields spread between these headlands,
teaming with flocks and herds, and redolent in beauty and fertility. Not
less charming is the scene presented on its eastern shore, though of a
softer tone, and more of a pastoral beauty, while beyond, the horizon is
limited by the bold and serrated outline of the Green Mountains. Still,
this scene of transcendent natural beauty on either shore, is dimmed by
the exquisite loveliness of the lake itself, which divides them. Calm and
blue its waters lie, placid as the cloud shadows that fleck its bosom,
reflecting the mountains and headlands, and studded with numerous islands
to variegate and adorn the scene -- some of which are mere rocky shafts
shooting up from the surface of the waters; others, decked in their native
emerald, gleam like gems upon its breast; while others, of alluvial formation,
glow in their soft and gentle loveliness, and are unsurpassed in their
exuberant fertility.
Reader, at the beginning of this chapter we likened history to a
bridge, and purposed to journey with you across it, o'er the beautiful
country we have attempted to describe, to the days when its history, so
far as we are able to learn, was not. During this journey the beautiful
Champlain must Ire the principal point of interest, for around no other
section of our beautiful country cluster historical associations so brilliant
and memorable. For a century and a half, this lake, appropriately named
by the Indians Caniadere-Guarante, that is, " the lake which is the gate
of the country," was rendered classic ground by successive deeds of daring,
by bloody forays, by the romances of border warfare, and by the conflicts
of fleets and armies. During those merciless contests, in which France
and England were the allies of savage tribes; in the long and sanguinary
conflicts between those great powers; in the war of the Revolution, and
that of 1812, the whole course of the lake was stained with blood, and
emblazoned by feats of glory.
When Samuel Champlain, in 1609, entered upon the waters which have
perpetuated his name, silence and solitude brooded over the charming scene.
Grand primeval forests covered the territory where the verdant fields of
Chittenden County now lie, with not even an Indian wigwam to relieve its
desolation and stillness, for continuous savage wars had driven its transient
population into the recesses of the forests, and beyond the mountain barriers
for protection. But this peace and solitude were soon to be broken. Even
upon Champlain's first visit his arquebus carried fear and death to the
hearts of the savages, some of whom he met on the New York side of the
southern part of the lake. Soon after, canoes and batteaux, in summer,
were gliding over its pure waters on errands of blood and rapine, or, in
winter, a highway of its crystal pavement was formed for the same purpose,
over which the French and their savage associates traversed the lake, thence
up the Winooski, and penetrating the gorges of the Green Mountains, devastated,
often amid the snows and storms of winter, the fairest villages of New
England. Later on, upon its blue waters and sequestered shores, vast armies,
clothed in the pomp and panoply of modern warfare, have gathered. But as
our brief account of the war of 1812, the war of the Revolution, etc.,
properly belongs to articles under these respective heads, we must defer
particular mention until they, in their order, are reached.
As settlements began to spring up in the State, and the forests
to recede before the sturdy strokes of the pioneer, trade and commerce
began to assert their rights. As Skeensboro (now Whitehall) was the first
point at which the settlers touched the lake on their way north, and as
the intercourse became more frequent between Connecticut, Massachusetts
and the new settlements, Major Skeene, after whom the place was named,
to accommodate the small business which was springing up, built a sloop
in 1770, and with it opened a communication with the settlements on the
borders of the lake and Canada. This was probably the first vessel which
made any regular trips through the lake, or which was used for the purposes
of trade. Soon after this, however, the Revolutionary war broke out, stopping
all further settlements, and even drove off nearly all the people who had
come, so that the navigation of the lake was returned to the uses of the
military power.
After the close of the war, settlements rapidly sprung up and trade
with the Provinces was soon commenced with redoubled vigor, so that the
white wings of the trading sloops, and the rafts of heavy timber, dotted
the whole length of the lake. But the great stride in progress was not
until 1808, one year after Robert Fulton made the memorable trial trip
of his steamboat on the Hudson. It seems that parties in Burlington were
the first to see, or at least to take practical advantage of, the new field
opened by this event; for during this year they launched the second practical
steamboat ever made in the world, and during the following year, 1809,
it was completed and commenced navigating the lake, just two hundred years
after Champlain had entered upon its waters in his bark canoe. The owners
and builders of this boat were two brothers, James and John WINANS. It
was in appearance similar to a large class canal boat, except being about
forty feet longer and six feet wider. Her decks were clear, having no pilot
house, being steered by a tiller, and her engine an horizontal one, being
all under deck, only the smoke pipe appearing above. There was but one
room below, about twenty five by eighteen feet, in which were berths upon
the side, and which was used for a dining room as well as for a sleeping
apartment. She was fitted with a secondhand engine and boilers; cylinder
twenty inches by three feet, "side level bell crank," with a large balance
wheel some ten feet in diameter, -- withal very poor machinery. But they
were the best that could be procured at that time, as manufacturers of
general machinery little understood the proportioning of machinery to resist
the power of steam. The consequence was that the boat was constantly subject
to "break downs," which were a part of her programme, and could be relied
upon to make a trip from Whitehall to St. Johns and back in about a week.
In October, 1815, however, she had her last "break down." On her trip from
St. Johns the connecting rod became detached from the crank, and before
the engine could be stopped, it was forced through the bottom of the boat
and she was sunk a wreck near Ash Island, a few miles south of the Isle
Aux Noix. The Messrs. WINANS took out her engine and boilers, and sold
them to the Lake Champlain Steamboat Company.
The great improvements made in steamboat building since the time
of the building of the "Vermont" are well known. Even as early as 1815,
a steamer was built on the lake whose speed doubled that of its predecessor.
This boat, the “1st Phoenix," met a sad fate, being destroyed by fire on
the 5th of September, 1819, causing the death of six of its passengers.
It may be well to state, however, that this is the only wreck or conflagration
which has occurred on the lake with an attendant loss of life. From this
time forward boats were rapidly put out, increasing in power and size,
until the present "floating palaces" have attained almost perfection. Navigation
companies were established, and steamboat property came to be the most
profitable in which one could invest money. Its profit was diminished,
however, by the advent of its near relative, the locomotive, which took
a large share of its business. Still, there is an extensive business done
on the lake at the present time, which will doubtless continue, notwithstanding
the building of railroads. We should like, did space permit, to add a sketch
of the establishment and progress of the several transportation companies,
but as it does not, we shall have to be content with giving, on the opposite
page, a table of the steamers that have been built on the lake, their dimensions,
by whom built, date of building, etc., which we hope will prove of interest
to many. Yet it may not be invidious to remark, that The Champlain Transportation
Co. is the oldest company existing on the lake, and that to its enterprise
and energy is owing, in a great degree, the past and present prosperity
of the transportation business. As early as October 26, 1826, the Vermont
legislature granted its charter, the following well known names appearing
as the company: Ezra MEACH, Martin CHITTENDEN, Stephen S. KEYS, Luther
LOOMIS, Roswell BUTLER, and Eleazer H. DEMING.
GEOLOGICAL
The geological formation of this county does not materially differ,
in general structure, from that of most of the other counties of the State.
Its rocks are distributed, like those of the others, in parallel ledges,
or ranges, extending nearly in a north and south direction. Passing eastward
from the lake shore, the first of these veins is a ledge of Trenton limestone,
which enters Charlotte from Addison County, underlying nearly the whole
extreme western part of that town, where it finally passes under the lake,
to appear again in Grand Isle and Isle La Motte, thence extending into
Canada. Although this rock has four distinct or chief varieties, one very
soon learns to distinguish it from all others, by its common characters
of black schistose layers, associated with slaty seams of limestone and
occasionally argillaceous matter. There are some varieties, however, that
can be assigned to this formation only by their fossils, in which the whole
group is peculiarly rich. The thickness of the Trenton limestone is 400
feet in New York, and is stated by Prof. ADAMS, in his second report, to
be of the same thickness in Vermont; but in one of his notebooks he suggests
that it may be even thicker. Mr. HAGAR, however, in his "Geology of Vermont,"
says he should think that 400 feet is rather too great a thickness for
it, as it generally appears in Vermont, though he has made no measurements
to settle the question.
A bed of Utica slate comes next in order, crossing the western part
of Charlotte and Shelburne, thence passing under the lake and cropping
out again in the extremity of Colchester Point, and thence across to Grand
Isle County. This formation is a continuation of the calcareous shales
of the Hudson River group of rocks downward, until they meet the slaty
limestone of the Trenton limestone, and it is extremely difficult to distinguish
between them and the shales of the Hudson River group in Vermont, except
by their fossils. The range has a thickness of about one hundred feet.
Next to this bed comes a range of rocks known as Hudson River slates,
about a mile in width, passing through Charlotte and Shelburne, the western
portion of Colchester, and thence under the lake. Lithologically, it consists
of deposits of pure and impure limestone, clay slate, calcareous slate,
interstratified with small beds of limestone, often sparry, silicious slate,
sandstones, brecciated limestone, and slate filled with veins of calcite,
etc. Prof. Thompson speaks of this variety in Chittenden County as follows:
"The black slate is generally contorted or crushed, and abounds in seams
of white calcite, varying from a line to a foot in thickness. Still there
are places where the spar has not been injected, and where the lamination
has not been disturbed. Cases of this kind may be seen on the eastern side
of Pottier's Point, and at Appletree Point. But all this slate doubtless
contains too much lime, and is too brittle to be used for any better purpose
than making roads. This slate, in many places, particularly where it is
fragmentary, has its surface covered with a black glazing, giving it very
much the appearance of anthracite. This may be seen near the meeting house
in Charlotte, and at Rock Point, and it has led some to suppose that coal
might be found in connection with it. But I believe very little, if any,
money has been thrown away, in the vain search for coal in this county."
The group is 930 feet in thickness, and is the highest member of the lower
silurian rocks.
Parallel with and adjacent to this range is an immense bed of red
sandrock, having a mean width of about four miles, and extending through
nearly the whole length of the county, making the principal rock formation
of the towns of Charlotte, Hinesburgh, Shelburne, Colchester and Milton.
Stratigraphically considered, this bed occupies the position of
the Medina Group, of New York, or its equivalent, the Levant series of
Pennsylvania and Virginia. The sandstones and shales bear a close resemblance
to those of the latter, not only in color, but in the profusion of fucoid
like markings which they display on some of the parting surfaces. The series
of reddish and gray limestones which rest upon these massive arenaceous
beds form an interesting feature in the geology of Vermont. Their altercation
with layers of sandstone and shale, and their frequently reddish tint,
would lead us to regard them as a continuation of the lower mass under
somewhat new formative conditions. In the prolongation of this belt of
sandstones and limestones toward the north, as in the vicinity of Burlington,
the latter mass is seen to consist, in great part, of a pinkish white,
fine grained limestone, which toward its base contains layers of reddish
limestone, interstratified with red sandstone, making the transition from
the arenaceous to the calcareous form of deposit. This latter variety forms
a very durable and handsome building material. The whole formation, however,
embraces a great variety of rocks, and there is some difficulty experienced
in associating them together, because of the general absence of fossils.
The general variety is a reddish brown or chocolate colored sandstone.
It becomes calcareous, and is frequently interstratified with dolomitic
layers of corresponding color. The grains of sand composing the rock are
often transparent, sometimes mixed with minute fragments of feldspar. A
slight metamorphic action has sometimes rendered the grains nearly invisible,
and made the whole rock compact. North of Burlington the variety is mostly
red and variegated dolomites. At Milton a grayish quartz rock appears,
probably equivalent to the red rock. The red color is owing to the change
in the combination of the iron which enters into its composition, produced
by heat.
Extending through the center of the county, with a mean width of
about three miles, underlying portions of the towns of Hinesburgh, Charlotte,
Shelburne, Williston, Burlington, Essex, Colchester, Westford and Milton,
is a range of Eolian limestone, or marble, one of the most important and
useful rocks in Vermont. It furnishes the beautiful white marble, equal
to the finest Italian, known all over the world as the product of this
State. Such a rock, and such marble, certainly deserve a name as beautiful
and as euphonical as the epithet Eolian. There is more variety in the limestone
of this group than in almost any other formation in the State; yet the
variations are mostly slight in themselves chemically, but considerable
as far as external appearance is concerned, producing the numerous shades
of variegated marble, each surpassing the other in beauty, ranging from
the purest white to inky blackness. An excellent opportunity is afforded
the curious for comparing our native marbles, both of this and other States,
with that imported from Italy, at the extensive manufactory of J. W. GOODELL
& Co., of Burlington, where immense quantities are kept on hand, enabling
one to examine the rocks side by side, both before and after they have
been cut and polished. An excellent quality of variegated marble, containing
many beautiful fossils, is quarried near Mallett's Bay, in Colchester.
The coloring matter in this species of limestone is usually derived from
minute particles of slaty matter disseminated through them. Hence they
never fade or disappear, or change their position in the slabs after they
have been quarried. The occasional stains which appear may be produced
by a small portion of pyrites, affording a dirty, brownish hue. Most of
the iron rust stain upon the blocks of marble at the mills is temporarily
produced by particles of iron worn from the saws. The thickness of
the Eolian limestone bed is estimated at 2,000 feet.
Leaving the vein of marble, we find next in order a deposit of clay
slate, about a mile in width, extending from the northeastern part of Milton
to the southern line of the county. The varieties in clay slate are few,
unless we refer to color. The rock is usually simple and homogeneous, composed
of finely comminuted, hardened clay. If it has a good deal of iron, and
if this is passing to the state of peroxide, we shall have red slate, such
as is quarried within the limits of New York, and in several localities
in Vermont. The red and gray slates, and also those of a greenish color,
are also found. Whoever will compare a bed of clay where the layers have
been deposited quietly above one another, with the slates used for roofing,
will notice a strong resemblance of form and composition; and he cannot
but suspect that the latter has been derived from the former. He can, if
he will, trace out the steps of the process. Clay hardened by the sun and
filled with cracks, seems to be a sort of first step in the process. Among
the newer sandstones he will see similar layers, called shale, which is
sometimes only a little harder than clay. These changes are produced in
the shales by the more powerful influence of metamorphic agencies, which
generally also super-induce other divisional planes in the rock, such as
cleavage and joints. But cleavage planes in most of the clay slates of
Vermont, coincide essentially with those of deposition; and the slaty layers
seem to be mostly strata or laminae modified. If the modifying force were
pressure, it seems to have operated to convert the planes of lamination
and stratification into those of cleavage, increasing the number of the
latter. The bed in this county, however, might more properly be termed
shales, and is unfit for roofing purposes.
An immense bed of talcose conglomerate, about four miles in width,
extending through the whole length of the county, and underlying a greater
or less portion of the towns of Hinesburgh, Huntington, Jericho, Williston,
Essex, Westford and Milton, lies next to the clay slate vein on the east.
According to Prof. Adams, in his report of 1845, this rock was called magnesian
slate, but later its present name was considered more appropriate, and
consequently adopted. The vein is a purely conglomerate species, having
associated together in its formation the following varieties of rocks:
Sandstones, breccias, quartz rock; calcareous rocks, novaculite schist,
talcose schist, and coarse conglomerates. The sandstones are few, while
the quartz variety is quite abundant. A large bed of the latter in almost
a distinct formation lies in the southern part of the county, extending
into the towns of Hinesburgh, Richmond and Williston. Prof. Thompson called
these rocks Taconic, and has left the following note concerning them: "These
rocks commence east of the clay slate and Eolian limestones, and extend
eastward; but I shall not attempt to assign their eastern limits. They
consist entirely of schistose rocks, composed chiefly of quartz, and most
of them more or less magnesian. There is a belt extending through Westford
and the east part of Essex, and the west part of Jericho to Winooski River,
which is quite chloritic. This is often thick bedded, and answers very
well for a building stone, though rather soft. It has been considerably
used for doorsteps, and has been transported to Burlington for that purpose.
Some of the strata appear to be a coarse sandstone, or rather a fine conglomerate.
Some places, as at Essex, exhibit a fine, compact magnesian slate, which
is easily sawed into any form, and is used as a fire stone. In many places
the slaty laminae are covered with fine talc glazing. The slate generally,
in the eastern part of the county, may perhaps be called talcose, but the
proportion of talc, in the greater part of it, is quite small. The predominant
mineral in it is quartz, and it often occurs, either white or limpid, in
seams several inches in thickness." In the Geological Reports of 1861,
Prof. Hagar says: "We have made no estimate of the thickness of the talcose
conglomerates, but know that they must be very thick. They must be 2,000
or 3,000 feet thick at the least calculation. We suppose that this bed
of rocks includes the Sillery sandstones of Canada. These are estimated
at 4,000 feet, in Canada." No fossils have been found in this range.
Adjacent to this vein of conglomerate is a large range of talcose
schist, extending eastward nearly to the county line. Talcose schist proper
consists of quartz and talc; but with this bed there are associated together,
consisting integral parts of the formation, clay slate, with plumbaginous,
aluminous and pyritiferious varieties; hornblende schist, gneiss, quartz
rock, sandstones and conglomerates, limestone and dolomites. Prof. Zadock
Thompson has the following respecting this range in Chittenden County:
"Along the foot of Mansfield Mountain, in Underhill, a thick bedded mica,
slate occurs, which makes a very good building stone. The stratification
is so completely obliterated, that much of it, like granite, splits in
all directions with nearly equal facility. In connection with these beds,
seams of chlorite occur. Some of the strata ranging north and south through
Underhill, Jericho, Bolton, and Huntington, are of a ferruginous character,
and iron ores in small quantities have been found in several places, but
not enough to justify the expectation of finding it in quantity. Near this
range of ferruginous slate, a narrow range of plumbaginous slate shows
itself in several places, as in Huntington and Jericho. This is doubtless
a continuation of the same narrow range of plumbaginous slate, which occurs
in Cambridge, Waterville, and the western part of Montgomery and Richford.
To the eastward of the synclinal axis passing through Underhill, and the
eastern part of Jericho, the rock perhaps should be called mica slate,
although it usually contains more or less talc. The rocks on the summit
of Mansfield Mountain appear, in places at least, to be talcose slate.
A great part of the slate which forms the mountains extending from the
chin towards the north, along the eastern border of the county, abounds
in octahedral crystals of magnetic iron."
The rocks underlying the residue of the county are of the Azoic
period and of gneiss formation. The essential ingredients of gneiss are
quartz, feldspar, and mica, forming a rock closely resembling granite,
differing from it only in having a distinctly stratified, slaty or laminated
structure. For this reason it makes a very handsome and convenient building
stone, as the sheets or strata can be easily obtained at the quarries,
and it can then be split or divided into any required thickness. “The thickness
of the gneiss in Vermont," says Mr. HITCHCOCK, "must be very great. The
section across Mount Holley, in Rutland County, .may perhaps give an average
of its thickness. About 8,000 feet of strata have been removed there, of
which we should estimate about 6,000 feet to have been of gneiss. Yet as
the bottom of the formation may not have been reached here, the true thickness
may be greater."
This ends our brief sketch of the principal rocks entering into
the geological formation of the county, and we will now turn our attention
for a few moments to its surface geology, then drop the subject, to be
taken up by far more competent hands than ours. That the whole of this
beautiful territory of Vermont, not excepting the summits of its most lofty
mountains, was once the bottom of a great ocean; that its verdant and flower
bedecked valleys were the basin or channel of mighty lakes and rivers;
that the whole was once covered by stupendous glaciers and ice floes, are
facts incontrovertible. Each of these epochs or periods has left its history,
written as plainly as the records upon the pyramids of Egypt, leaving behind,
as it were, "Footprints of their Creator." But they who have deciphered
the history, or "Testimony of the Rocks," have not, as has the Archeologist
that of the pyramids, arrived at the truth by delving in the ruins of a
forgotten language, but from the scroll of nature, descending into the
bowels of the earth, and reaching forth into the uttermost parts of the
limitless heavens for information. For –
"All infinite,
all limitless in awe,
Heaven
to great minds was given:
Yet, with
all his littleness, down to his inch
Man can
draw – the heaven."
Such is
the province of the geologist.
But to return to the several changes we have mentioned. Among men
of science it has become the common, if not the prevailing opinion, that
all the elements with which we meet were first in an ethereal, or gaseous
state that they slowly condensed, existing for ages as a heated fluid,
by degrees becoming more consistent that thus 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,
is known to geologists as elementary or molten. Then came another age,
in which this 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 over 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
vapors 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 would cover the earth with mighty ice floes
and glaciers, forming what is known as the drift, or glacial period. Evidences
of these several epochs are left in Chittenden County by terraces, moraines,
drift bowlders, etc.
First, terraces. -- These are simply shelves, or water marks, left
on the sides of valleys and mountains, proclaiming that they were once
the beach of a lake or ocean., while the fossils left will decide which
of the two it was. These terraces are the most fully developed in the valley
of the Winooski; yet the Lamoille valley, and that of the other several
streams, contain fine specimens. The deposits of sand, too, proclaiming
the bed of an ocean, are numerous and extensive, particularly in the towns
of Milton, Colchester, and Burlington. They are for the most part superficial,
varying in depth from a few inches to eighty or ninety feet, and in general
have a regular and nearly horizontal stratification. They usually terminate
downward in brown or blue clay, and in many places the mixture of clay
and sand is in the proper proportion for making brick, as at the foot of
Winooski Falls. The elevation of the surface of these sand deposits varies
from twenty to two hundred and sixty feet above Lake Champlain. The mean
elevation of those plains (terraces) to the westward of the range of limestone
extending from Rock Point to Mallett's Head, and thence to Milton, may
be estimated at forty feet; and the mean elevation of the extensive sandy
plains commencing in Burlington, and extending through the southwestern
part of Essex, and through the central parts of Colchester and Milton,
is about 200 feet. Marine shells are found in this sand in numerous places.
At one place in Burlington, half a mile northeast from Rock Point, and
by the side of the road, they abound in a coarse gravel about 130 feet
above the lake; and two miles northeast of Mallett's Bay, in Colchester,
is a large deposit of them at an elevation of more than zoo feet above
the lake. At both places they are much broken, and mingled with rather
coarse gravel. It would appear in these places, that the shells had been
worked up above the line of the shore composed of drift, and that the gravel
of the drift was mingled with them by the action of the waves, and these
and larger objects, like the fossil whale, were buried by the washing down
of the drift materials.
Second, drift. -- We think it will not be difficult for almost any
inhabitant to form an accurate idea of drift. For in almost every part
of the county occur accumulations of bowlders, or large blocks of stone,
with the angles more or less rounded, lying upon the solid ledges, or upon,
or in the midst of a mixture of smaller fragments, with gravel and sand;
the whole mingled confusedly together, and evidently abraded by some powerful
agency from the rocks in place, and driven along pell mell often to great
distances; for if the bowlders and fragments be examined, they will for
the most part be found not to correspond to the ledges beneath, but to
others many miles perhaps to the north or northwest.
Third, moraines. -- These are a class of terraces formed by ice
instead of water. The theory of their formation is as follows: In the glacial
period, icebergs became stranded at the base and on the sides of hills,
and deposits were made around and upon them, and they would have been level
topped if the ice had remained; but in consequence of its melting they
are now extremely irregular. At Underhill Flats the moraine terraces are
abundant, and beautifully rounded, upon both sides of Brown's River.
Gazetteer
and Business Directory of
Chittenden
County, Vt. For 1882-83
Compiled
and Published by Hamilton Child
Printed
At The Journal Office, Syracuse, N. Y,
August,
1882.
Pages 33-50.
Transcribed
by Karima Allison ~ 2004
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