Why The Treaty Of Paris Left Lingering Questions

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Treaty of Paris

Marinus Willett, ca 1791, by Ralph Earl, CC0, via Wikimedia Commons

Colonel Marinus Willett sloshed through the icy marsh with growing concern. It had been two hours since midnight. They should have seen the fort by now.

Even as the Treaty of Paris was being crafted to end the Revolutionary War, the frigid night of February 9, 1783, gave way to the frozen morning of February 10. On New York’s western frontier, Willett found himself leading one final secret mission for George Washington.

Willett pushed his way to the head of the column. “Where’s the guide?” he asked. The lead soldier shrugged. They had not seen the guide in quite some time and were doing their best to follow his tracks. The soldier pointed forward as the last light of the setting moon shone upon the footprints in the silvery, shadowed snow ahead of them.

With urgent impatience, Willett hurriedly followed the freshly made steps. It took him thirty minutes to catch up to the Oneida scout. The Indian stood like a statue, frozen as the snow around him. He was scared. Worse than that, he was lost.

Washington’s words reverberated in Willett’s head. “You can always waste time, but never recover it… in such an enterprise as yours, want of time will be a certain defeat.”1 The misdirection delayed them. They were late. The element of surprise was gone.

Willett was forced to abort and return to Fort Rensselaer.

*     *     *     *     *

George Washington wanted one last victory before the war officially ended. With the defeat of Cornwallis at Yorktown in October 1781, the British lost any taste for further fighting. In March 1782, Parliament effectively abandoned further offensive operations in America. With the exception of their Indian allies, the year remained relatively quiet.

Yet, there was no formal peace treaty.

Was the war really over?

In Philadelphia, many assumed the clash with King George was coming to an end. Along New York’s murky western frontier, however, such certainty remained elusive.

British regulars may have been quiet in 1782, but that didn’t mean the soldiers weren’t at work. They busied themselves rebuilding Fort Ontario. Abandoned in 1778, early in the Revolutionary War, it was located on the east bank of the mouth of the Oswego River, high above Lake Ontario. Clearly, the British weren’t taking chances. Whatever diplomats might eventually agree upon, military planners on the frontier still prepared for war. At a minimum, they intended to protect their lucrative fur trade.

The possibility of renewed conflict remained. Washington also wished to take no chances. With his army camped in New Windsor, New York, the Continental’s Commander-in-Chief decided upon one final military gamble. His target: Fort Ontario.

The prominent fortress represented Britain’s closest and most formidable stronghold on the frontier. Unlike Fort Niagara, which guarded the Confederacy’s western gateway, Fort Ontario lay deep within the former territory of the Six Nations, just beyond New York’s western-most settlements.

In January 1783, Washington developed a plan to surprise the British and take Fort Ontario. He selected Colonel Marinus Willett to lead the operation. Willett was in command when his troops pursued and killed “the notorious Captain Walter Butler” on October 20, 1781, just ten days after the surrender of Cornwallis.2 So vilified was Butler that it’s been said news of his death brought more cheers in the Mohawk Valley than Washington’s victory at Yorktown.3

Despite the apparent finality of Cornwallis’ defeat, Washington wasn’t going to be lulled into a false sense of security. He presented the Colonel with strict instructions to operate under sealed orders. The fewer who knew the purpose of the mission, the better they could conceal it from the enemy.

Alas, an errant Oneida scout lost his way guiding Willett’s troops to the fort. Forced to forsake the mission, Washington’s hand-picked man returned to Fort Rensselaer and soon learned that American leaders had received Lafayette’s letter reporting a treaty had been agreed to.

Was Lafayette negotiating on America’s behalf? The short answer is “No.” That responsibility fell to Benjamin Franklin, John Adams, John Jay, and Henry Laurens. The longer answer is a bit more complicated. If you thought the competing European claims and the Royal mess surrounding Western New York were complex, ending the Revolutionary War required just as many moving parts.

For peace to become reality, not only did Great Britain and the United States have to agree, but so did France (hence, Lafayette) and Spain.

(Did you notice who was missing from the negotiating table?)

It was the preliminary multinational agreement reached in January 1783 that Lafayette reported to American leaders. The formal Treaty of Paris would be finalized later that year and officially ratified in 1784.

Much to America’s delight, George III agreed to cede all British territory south of the Great Lakes, including lands extending to the Mississippi River. Naturally, this would include Western New York.

On paper.

It’s one thing to draw a map showing boundaries. It’s quite another thing to turn that map into reality. And for the Greater Western New York region, that reality remained as murky as the night of February 9th was to Colonel Willett.

For one thing, the British still occupied their chain of forts within what was now nominally the United States of America. These included both Fort Ontario and Fort Niagara.

This wasn’t an oversight. Article 7 of the Treaty of Paris specifically said “his Britannic Majesty shall with all convenient speed…withdraw… from every Post, Place and Harbour…”4 The wording in the Treaty was clear. Despite this, when asked to comply, General Sir Frederick Haldimand, Governor of the Province of Quebec and Commander-in-Chief of British forces in North America, stated that he was aware of the Treaty but had not yet received orders to evacuate the forts.5

Whether he admitted it or not, Haldimand had several reasons for this delaying tactic. Occupying the forts provided the British with leverage over the Americans.6 It protected British trade interests.7 It helped ameliorate the restless Iroquois who felt betrayed when the British ceded lands they felt were theirs.8 Finally, the British understood the United States was too weak to enforce the Treaty9, so there was little downside in breaching it.

The Treaty changed the maps, but it didn’t change the reality on the ground. The British still held the forts. Their former allies, particularly the Seneca, remained a powerful presence on the frontier. There also remained the question of the precise boundary along the Niagara River.

This reality posed a challenge to the new nation of America. A new nation bound by the fragile Articles of Confederation. The Articles offered little money and little authority. In short, they provided the United States with no practical ability to enforce its frontier claims.

Not that New York State was in any better position. In fact, it was worse.

By the end of the Revolutionary War, most of the other competing colonial claims for this territory had been resolved. Massachusetts, however, continued to rely on the wording of its provincial charter. The Bay State insisted those provisions still conveyed rights in the Greater Western New York region.

The Treaty of Paris may have settled the war between Britain and the United States, but it left too many matters unresolved. For the coastal cities, independence had been indisputably achieved. For the frontier of Western New York, it only created more questions.

And a vast void of authority.

Into that void rushed old claims, forgotten charters, and competing visions of who possessed the right to the frontier. One dispute in particular would shape the future of Western New York forever.

1 Willett, William M., “Washington Letter to Willett, February 2d, 1783,” A Narrative of the Military Actions of Colonel Marinus Willett, G.&C.&H. Carvill, New York, 1831, p.147.
2 Halsey, Francis Whiting, The Old New York Frontier, Charles Scribner’s Sons, New York, 1902, p. 306.
3 David A. Charters, “BUTLER, WALTER,” in Dictionary of Canadian Biography, vol. 4, University of Toronto/Université Laval, 2003–, https://www.biographi.ca/en/bio/butler_walter_4E.html, retrieved June 8, 2026.
4 Article 7, Treaty of Paris (1783), National Archives, https://www.archives.gov/milestone-documents/treaty-of-paris, retrieved June 3, 2026.
5 Collections of the New York Historical Society for the year 1878, Publication Fund Series Vol XI, New York, 1879, p. 193.
6 Broadhead, John Romeyn, Documents Relative to the Colonial History of the State of New York V10, E.B. O’Callaghan, ed, Weed, Parsons & Co., 1858, p. 1004.
7 Sessional Papers Volume 5, Second Session of the Parliament of the Dominion of Canada, A. Senecal, Ottawa, 1888, p. xx.
8 Stone, William L., Life of Joseph Brant – Thayendenegea Including the Border Wars of the American Rev, H.&E. Phinney, Cooperstown, 1838, p. 271.
9 Ibid., p. 263.

Sullivan’s Soldiers Discover The Genesee Valley

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Genesee ValleyToday, we call it the Genesee Valley. To Sullivan’s soldiers, the broad plain surrounding the great Seneca town of Chenussio was the Genesee Flatts, a beautiful vista that remained etched in memory long after the campaign ended. Soon, very soon, to American pioneers scanning maps of the western frontier, the entire region would come to be known simply as the Genesee Country.

Before that, however, there was the Sullivan Expedition. It entered the Genesee Valley as a military campaign. It left behind something far more enduring. More than 4,000 soldiers carried home eyewitness accounts of a fertile country few Americans had ever seen.

Shortly after noon on Tuesday, September 14th, 1779, Lieutenant Erkuries Beatty and his fellow soldiers had finished destroying a “great abundance” of corn and beans.1 He—and the men with him—were about to behold a sight unlike anything they had seen before. For a Continue Reading “Sullivan’s Soldiers Discover The Genesee Valley”

Lafayette’s Farewell Tour: Riding The Ridge (Road)

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Previous: The Natural Wonder Of Niagara Falls, Goat Island, And Lewiston

Western Portion of 1825 Erie Canal map showing Niagara Escarpment (upper shaded line) and Onondaga Escarpment (lower shaded line). If you look closely you’ll see Ridge Road just north of the Niagara Escarpment. Source: Laws of the State of New York, in relation to the Erie and Champlain canals / Published by authority, under the direction of the Secretary of State (E. and E. Hosford, printers, Albany, 1825)

Over the eons, what would become the North American continent heaved and hoed. Rock strata, once flat with the earth when created, now undulated in waves. Each layer born in a different geological epoch bore their own unique properties. Some too loose and soft to sustain the onslaught of wind, water, and ice; others stubbornly sturdy, able to withstand those same powerful forces.

As the most recent period of glaciation receded into Canada and further north, the melting ice revealed the natural formations known as cuestas. These landforms represent a gentle upward slope on one side and dramatic fall – often evidenced by a face of rock on the frontslope.

This precipitous cliff is called an escarpment. Western New York contains three such Continue Reading “Lafayette’s Farewell Tour: Riding The Ridge (Road)”

How Ice On The Rocks Reveals Our Destiny (Part II)

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Previously: How Ice On The Rocks Reveals Our Destiny (Part I) |


You wouldn’t be here if it weren’t for the glaciers.

No, really. You might be somewhere, but you wouldn’t likely be here.

And you can thank the glaciers for that.

You can’t live in Western New York (in general) and our area (specifically) without recognizing the significance of the glaciers. Our neighborhoods contain the remnants of drumlins, kames, and other glacial debris. You see it in the eskers you walk upon in Mendon Ponds Park. You see it in the cobblestone houses that dot our landscape. In fact, you see it every day, only you probably don’t notice it.

As the once majestic Acadia range eroded into what is now the Greater Western New York region, it buried the marine flora and fauna, leaving the fossil record we see today. But it’s not as easy as that, for intervening events would bury these treasures deeper beneath the surface.

“An awful lot of this is later covered by sediments trapped by the glaciers,” says George McIntosh, Paleontologist, RMSC (Emeritus) who specializes in the geology and fossils of the Devonian Period. “The giant continental glaciers that came in here starting about 2 million years ago, or so. But there are some good exposures. People from all over the world – from China, Australia, Europe, and certainly people from North America – come to Western New York to study our fossils in our rocks. There’s good exposure obviously down at Letchworth and there’s good exposures in a variety of different places.”

The Grand Canyon of the East – Letchworth State Park – stands as a testament to the forces of nature that ultimately guide our lives. The gorge itself stands as a monument to nature’s relentless fury – not just the Genesee River’s role in eroding the various Devonian Period (remember that?) shales, sandstones and siltstones. It’s something bigger, something stronger, something with powers and abilities far beyond those of mortal men!

“In this part of New York State, everything above the Devonian Period has been eroded from this part of the world by early rivers, but more recently by the glaciers during what we call the Pleistocene Period or the Pleistocene Era,” says Professor Richard Young (Distinguished Service Professor, Emeritus, SUNY@Geneseo). “And that’s divided into many sub-partitions when the ice advanced across this region, probably at least 10 times roughly every hundred thousand years. But the Pleistocene as it’s defined today is approximately 2.6 million years old.”

Much of the topography we see around us today emerged from beneath the retreating glaciers during the most recent Ice Age. It wasn’t a singular event, but a series of actions over tens of thousands of years.

“The last ice advance during the Pleistocene is called Wisconsin and the Wisconsin is divided into three parts, the early Wisconsin, the middle Wisconsin, and the late Wisconsin,” says Young. “What you see around you and the landscape was all formed pretty much during the late Wisconsin. That was when the ice advanced all the way down to Long Island approximately 25-30,000 years ago.”

Ultimately, two geological forces sculpted the land around us. The pure weight of the mile high ice crushed and depressed the entire landmass and smoothed the ridges. This caused Lake Iroquois – the larger predecessor of Lake Ontario – to empty into the Atlantic Ocean through the Mohawk River rather than the St. Lawrence River as it does today. It’s also why the northern topography of Western New York is much smoother than the jagged landscape of the Southern Tier.

At the same time, moving water chiseled into the earth and carried debris to create new landforms – moraines, eskers, drumlins, kettles, and kames. As the glacier melted its way back to Canada, it unveiled a new landscape, one which would reveal our fate.

“Approximately 16,900 years ago the glacier was in Dansville,” says Young. “Then it slowly retreated northward across the State for about 4,000 years. In the process it created a series of ridges that run east-west. Those regions are places where the ice temporarily was still – it was melting, at the same rate that it was advancing. So it dropped a lot of sand and gravel and there are roughly a dozen moraines between Pennsylvania and Lake Ontario.”

You may recognize some of these familiar features.

“One of the moraines runs through the University of Rochester and that’s called the Pinnacle Hills, where all those radio towers are,” says Young. “One of the more interesting features that formed, along with the moraines, is a whole series of other irregular land forms. We have small ponds which form where ice blocks melted. And we have piles of sand and gravel called kames. Kames are simply places where piles of sand and gravel were dumped more than elsewhere, so they stand above the local landscape. But the moraines are these long ridges and a fairly complex sequence of moraines, kames and kettles formed at the location known as Mendon Ponds.”

Not only do the glaciers reshape the earth, but they can also change the course of mighty rivers.

“The Genesee Valley is formed mostly by the Genesee River, but not only by the modern Genesee River,” says Young. “There was a series of rivers over the last 2 million years. And each time there was a glacier advancing from the north, that would be followed by a reformation of the River after the ice melted.”

“The present course of the River is very complicated,” continues Young. “There are old valleys, like the one at Dansville, and the one through Nunda from the south end of Letchworth Park and Portageville to Nunda. And the newest part of the River system is Letchworth Park, and that’s clear because it’s formed in bedrock.”

We can identify the newly established river paths by the lack of sediment on the ancient rock.

Young says, “The signature for young valleys in this part of the world is that they are formed in bedrock are the ones that formed after the last ice melted. The Genesee River formed a new course that it hadn’t occupied before entirely and that’s the one through Letchworth. Then it continued on past Geneseo and through to the area of Rochester.”

But that’s not the way it used to be.

“There’s also an older channel that is often discussed in the literature and that’s where the Genesee River turns to the east in the area of Rush and then flows north into what is today Irondequoit Bay,” says Young. “But that probably happened more than once, and each time the ice advanced, it made the valleys a little bit bigger or shaped them or carved them a little bit deeper so that some of them are actually below sea level, or at least the bedrock of the valley is below sea level. Since the last Ice Age roughly 13,000 years ago, the Genesee River has never flowed to Irondequoit Bay, although it did, in the long ago distant past and maybe more than once, but the present day channel is the one that formed as the ice retreated northward and the River ended up flowing through Rochester.”

The Truth Behind The Mystery Of Weather Forecasting

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Ah, winter. Remember that? Well, if for some reason you had forgotten, last week certainly provided a useful reminder.

Of course, if you live in New England, you got your reminder a few days earlier with a classic Nor’easter.

Yes, that’s the way the National Weather Service (“NWS”) spells this famous type of storm. These weather events feature notorious low pressure systems that travel up the eastern seaboard. They’re so named because the winds along the coast come from the northeast.

Nor’easters are not limited to the winter. The NWS tells us these storms generally occur in Continue Reading “The Truth Behind The Mystery Of Weather Forecasting”

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