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SAMUEL ORCUTT
Golden Hill Indians
The Housatonic
The Wepawaug
Cupheags and Pequannock
Weantinock
Goodyear's Island
Indian Slaves
Indian Remnants
Indian Troubles
New Indian Papers
Wm. Howard Wilcoxson
Stratford Indians
Trouble with
the Indians
Establishing
Title to the Land
Indian Deeds and
Relics
White Hills
Purchase
FORREST MORGAN
Lifestyles, Government, Religion and War Indian Titles and Mohegan Land Troubles Sowheag, Uncas, and Miantonomo Owenoco, the Son of Uncas
THE
HOUSATONIC
CHARD POWERS SMITH
The Promised Land
Heathen in the Land
The Lord's Scouts
The Land and The Lord
The Next Seven Tribes
ALEXANDER JOHNSTON
Connecticut Indian History
The Pequot War
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Chard Powers Smith - The Housatonic
The Promised Land
The First Billion and a Half Years
New England has never quite forgotten that in the old days
it was a separate continent. The old
days were the first five and most of the sixth day of Biblical creation. Or, if you prefer, they were almost all of
a billion and a half years of geologic history which the scientists find
recorded in the rocks. It is only in
the last fifty million years or so that New England has accepted the
inevitable and joined the unwieldy continental union which we call North America.
The old continent of New England went north into Canada about as far as the present St.
Lawrence River, and south to include Long Island. Its eastern shore was a good way out in
what we call the Atlantic, and sometimes its western shore included most of
modern New York
State. The scientists called it Acadia, because
that is a pretty name, or perhaps because they lack proper respect for New England. To
the northwest, beyond a stretch of ocean, was another little continent which
they call Canadia. To the southwest
was another names Appalachia.
From the earliest geologic time, western Acadia, where the valley was to be, has been “the place
beyond the mountains.” From the age of
fire and steam, when the earth’s crust was cooling into shape, it remained
restless over this upland. Every
twenty or thirty million years, either the underlying fire or the lateral
pressure of the contracting earth’s crust would heave up volcanic peaks five
or six miles into the sky. Then the
volcanoes would quirt down, the broken crust would lie jagged in upended
fragments, and for a quiet aeon frost and water would whittle down the
giants, spilling out the sediment in strata that filled the valleys and lay
eastward and westward over lowlands and out over the ocean floor. Then another period of fire and shrinking
crust would thrust up mountains again, and the whole process would be
repeated. October
Mountain, Monument, Bear, Everett, Riga, Cannan, Sharon, Skiff, and the
hundreds of others are the worn stumps pf what were once the loftiest
mountains in the world. Throughout
these ages, the drainage of Acadia’s western
highland was into either the western or the eastern ocean. There was no ancestral, north-and-south Housatonic Valley where a great river ran into
the southern sea.
During most if the billion and a half years of
the old days there was life of sorts around Acadia
or upon it. For the first billion
years it was all in the sea or in the rivers, with a little greenery groping
into the air along the shores. During
this time, the fish got such a head start that the Yankees haven’t yet been
able to catch them all. After a
billion years, real forests and flowering plants began to cover the gray
rocks, and the oldest fossils in New England
are of some of the later from the western mountains where the valley was to
be. Certain fish experimented with
breathing air, and out of these amphibians reptiles emerged that ranon the
land and forgot the water entirely.
The old days ended picturesquely with the dinosaurs, the biggest
animals that ever lived. They left
their footprints and bones here and carried their ponderosity up into the
western mountains. After the dinosaurs
were exterminated-by what process is still in doubt—the new days, the epoch
of recent life, dawned with little mammals that suggested their modern
descendants. On the biblical analogy,
the sixth and last day of creation began.
This end of the old days and the dawn of the new
occurred about fifty million years ago.
Geologically, it was marked by a very special mountain uplift which
involved dew if any volcanic eruptions and was not a local affair in Acadia. It
likewise involved Canadia and Appalachia,
generally the whole eastern part of the great new continent whose coast line
is lifted out of the ocean. From
southern Appalachia, in modern Alabama, to northern Arcadia, in modern
Quebec, it was as if some earth-huge Titan put his hands on the carpet of the
earth’s crust about two hundred miles apart and pushed them steadily together
for perhaps a million years. The
carpet, much of which had before been on the ocean floor, bowed up in a
thousand-mile-long welt running exactly northeast and southwest. The welt was the whole Appalachian ridge,
the backbone of eastern North America. It shed off the sea between Appalachia and Acadia and Canadia forever, and lifted its western
slope far out to drain the ocean from the great plains and complete the rough outlines of
the big continent. The high point of
the new range was in New York,
a little west of where the primordial Berkshires had been. Everywhere from
the new heights, new rivers began to pour southeast to the Atlantic, the
beginnings of most of the great rivers of the eastern seaboard today, the
Santee, the James, the Potomac, the Rappahannock, the Susquehanna, the
Delaware, the Connecticut, The Merrimack, the Kennebec, and among them the
Housatonic.
In the beginning, the Housatonic was a straight
river flowing southeast all the way, and the lower third of the modern
stream, traveling southeast from the big bend at Scatacook in northern Sherman, still runs in
its primeval, fifty-million-year-old-bed.
Above the bend, the original upper reaches came straight down from the
northwest, far over in New York State beyond the future Hudson Valley. For a precarious age, it looked as if one
of New England’s big rivers was going to be sourced in New York.
But the primitive Hudson, them a mere
tributary of the Delaware,
took care of that. Nibbling its way
headward, it broke through the banks of the Housatonic
and stole its headwaters. What had
before been the biggest tributary of the Housatonic, running south out of Massachusetts to join
at Scatacook, became the main stream that has since boiled around the big
bend there. Deprived of its original
sources, the Housatonic became a smaller
river, as its old shore lines high along the hills below Gaylordsville bear
witness. But it became exclusively a
New England river, and the geologic honors of both New
York and New England were
saved.
Meanwhile, the promised land had swarmed
increasingly with life. At first it
was a tropical jungle, with the diminutive ancestors of tigers, elephants,
rhinoceroses, tapirs, horses, and dogs.
Later, as the climate grew cooler, the forest took its modern form,
and the animals began to look like moose, deer, wolf, bear, and bison, while
the monarchs were the mastodon and the saber-toothed tiger.
A million years ago, the Glacial Ages began. For four periods about a hundred thousand
years each, the valley lay under an ice sheet at least a thousand feet
deep. Between the glaciations there
were long temperature periods when life returned. The weigh and slow flow of the glaciers did
not alter the topography of the region.
But it did scoop off the precious topsoil from the hills and dump it
into the ocean south of Long Island that
until very recently was part of the mainland.
Having scraped off the soil, the ice sandpapered and scratched he
underlying granite, deposited piles of gravel here and there, and scattered
everywhere the billions of boulders that the Yankees have hauled out of the
ground and piled into walls.
It was only twenty thousand years ago that the
fourth ice sheet was all gone, and the time since had been to short for much
topsoil to weather out of the rocks.
The landscape was taking its complete modern aspect, and the new
forest teemed with the creatures man has known, including the vanished heath
hen, passenger pigeon and wild turkey.
In migration time, the flocks of pigeons overshadowed the sun and made
a fluttering twilight in the forest.
Waterfowl and fish crammed the streams and ponds, and every spring
lamprey eels and solid shoals of shad ran up the river and its
tributaries. Otter and beaver were
plentiful a vast natural larfer and wardrobe was preparing.
There is no evidence that the valley-or any other
part of America-ever cradled any of the primitive ancestors of Man. That grave responsibility was left to the
more experimental, old world. After he
finally entered this continent from the west, New
England was probably the last region to accept this strange,
nervous creature. No one knows just
when he slipped through the mountains into the valley of the Housatonic. But
it the rock-recorded, geologic time is an hour, it was less than a thousandth
of a second ago. It was late in the
twilight of the sixth day of Biblical creation, and here the analogy of Genesis breaks
down. Having set man in New England, the Lord neither rested nor let him rest.
If you
have any questions email me at:
shesabo@netzero.net
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THE
HISTORY OF CONNECTICUT
BENJAMIN TRUMBULL
The Perfect Savages
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ALEXANDER JOHNSTON
Connecticut Indian History
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SOUTHPORT SWAMP
Great Swamp Fight
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Colonial History of Pequot Swamp
GUIDE TO PUTNAM
MEMORIAL CAMP
COLONIAL INDIAN ARCHIVES
Stratford
Colonial Land Deeds
Fairfield
Colonial Land Deeds
Derby Colonial
Land Deeds
THE
HISTORY OF GUILFORD
Hon. Ralph D.
Smith
A
HISTORY OF THE TOWNS
OF
HADDAM AND EAST HADDAM
David D. Fields
EARLY NEW HAVEN
Sarah
Day Woodward
Winthrop’s Journal
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