Fort Wayne Before the City: Glaciers, Rivers and the First Peoples

Before Fort Wayne · the place before the city

Every other section of this record begins with people. This one begins with the ground, because the ground is why everything else happened here. Before there was a city, a fort, or a town of any nation, there was a place: three rivers meeting on a low glacial divide, a lake that had drowned the country to the east and burst through this ground in the greatest flood the region's geology records, a swamp that walled off the east for a hundred miles, and a carrying place — a few wet miles of marsh — that joined the waters of the Great Lakes to the waters of the Mississippi. Human beings used this place for some ten thousand years before it had a name anyone wrote down. This section is the record of the place itself: what was here, in the order the earth made it, exactly as far as the geological surveys, the archaeologists, and the earliest written accounts establish it — and no further. The peoples who held this ground have their own section (Tribes), the question of who legally owned it and who bought it has its own (The Land), and the story of forts and city that begins in the 1700s opens the Story. What belongs here is the stage they all stood on.

Three rivers, one confluence

THE GROUND THAT DECIDED EVERYTHING AFTER

Fort Wayne stands where two rivers become a third. The St. Joseph River comes down out of southern Michigan, flowing south-southwest for roughly a hundred miles from its rise near the Michigan lakes country. The St. Marys River comes up out of west-central Ohio — its headwaters lie in Auglaize County — flowing northwest. Where they meet, in the middle of the present city, their combined water turns northeast as the Maumee River and runs some 130 miles through the flat lake plain to Toledo and Lake Erie. The Maumee drains the largest watershed of any river flowing into the Great Lakes — more than 6,300 square miles of Indiana, Ohio, and Michigan — and all of it funnels past this one confluence.

The ground at the meeting is unremarkable to look at, and that is the point. The city occupies a broad, low swell of glacial debris at roughly 780 to 800 feet above sea level — high enough to stand above the flood plain of its rivers, low enough that the climb out of the valley is barely a climb at all. Three of the region's great surface units meet in Allen County: the flat clay floor of an ancient lake (the Maumee Lacustrine Plain) to the east, the rolling till plain to the south and west, and the moraine ridge the retreating glacier dropped across the middle. The St. Marys, in the description carried in the National Register nomination for the Richardville house, forms part of the boundary between the till plain and the lake plain. A city could have stood anywhere along these rivers. It stands here because of what the next sections describe: the divide, the portage, and the lake that made both.

Sources: U.S. Geological Survey and Indiana Geological and Water Survey watershed and physiographic descriptions of the Maumee basin; National Park Service, National Register nomination for the Akima Pinšiwa Awiiki (Chief Jean-Baptiste de Richardville House), Fort Wayne (the river courses and the till-plain / lake-plain boundary).

The divide and the carrying place

A FEW FEET OF EARTH BETWEEN TWO OCEANS' WORTH OF WATER

Fort Wayne sits on the continental divide between the Great Lakes–St. Lawrence drainage and the Mississippi drainage. Rain that falls on the city flows north and east, down the Maumee to Lake Erie, the St. Lawrence, and the Atlantic. Rain that falls a short distance west of the confluence flows the other way — into the Little River, down the Wabash and the Ohio, into the Mississippi and the Gulf of Mexico. The Richardville house nomination states it precisely: rain falling two miles west of the confluence at Fort Wayne runs to the Mississippi. The 1880 History of Allen County, describing the marshy summit west of the city, put the whole geography of the place into one sentence: only about four feet of earth prevented the waters of the St. Marys system and the Little River system from mingling outright.

Between the two systems lay the Maumee–Wabash portage, the carrying place. Its eastern end was the great western bend of the St. Marys, at what is now the Swinney Park–Rockhill Park ground in the city's west end — the Allen County–Fort Wayne Historical Society marked the spot in Rockhill Park in 1959. Its western end was the headwaters of the Little River in today's Aboite Township, near the crossing of Hamilton Road and U.S. 24. From there the Little River runs some twenty-two to twenty-four miles southwest to join the Wabash at the Forks, below Huntington. The carry between navigable water on the two sides was one of the shortest portages anywhere in the interior of the continent — the only land barrier on the shortest trade route between Quebec and New Orleans, as the Historical Society's marker text puts it.

How long was it? The record gives a family of answers rather than one, and they are printed here together because the truth is that the portage changed length with the water. George Croghan, who came through in 1765, reported the carrying place at about nine miles. The Myaamia-language record carried in the Richardville nomination likewise calls it the "nine-mile portage." Charles Poinsatte's standard history of early Fort Wayne measures seven miles from the confluence to the Little River. The Historical Society's 1959 marker calls it an "eight-mile carry." The News-Sentinel's Cityscapes history of the route reconciles the spread: usually about nine miles — but in drought, or when beavers had dammed the creeks, a canoe might have to be carried forty miles, all the way to the Wabash at modern Huntington; and in great flood, the marsh between the rivers filled so completely that a canoe could be paddled the entire distance from the St. Marys to the Little River without any carrying at all. The summit between the rivers was not dry land with a path over it. It was a marsh — some 18,000 acres of swamp in Aboite Township alone — that was water, mud, or something between, depending on the season.

The Myaamia, who controlled the portage and inherited that control through named families, called the Little River pwaawikamisiipi — the "weak-water river" — for the slack little stream at the far end of the carry. And the place at the near end had the most famous description ever given it. Little Turtle — Mihšihkinaahkwa — speaking of Kekionga in the treaty councils of the 1790s, called it "that glorious gate … through which all the good words of our chiefs had to pass, from the north and the south, and from the east and the west." The gate was the portage. Everything in Fort Wayne's later history — the forts, the canal, the railroads, the city — is an attempt by successive powers to hold, tax, or replace this few miles of wet ground.

The ground itself no longer shows it. The great drainage works of the 1880s emptied the Aboite swamp, and as the News-Sentinel's account concludes, the drainage "has all but destroyed the frontier appearance of the land"; the actual track of the portage is lost, and its modern trace is a street name — Portage Boulevard, on the city's west side. The canal that replaced it, and the highway that follows the old channel, belong to the Story. What belongs here is the fact the canal-builders were exploiting: the divide at Fort Wayne is so low, and the marsh at the summit so wet, that for part of the year the two great watersheds of the continent's interior very nearly touched.

Sources: National Park Service, National Register nomination for the Akima Pinšiwa Awiiki (the divide, the "nine-mile portage," the Myaamia river names, the Little Turtle quotation); Charles Poinsatte, Outpost in the Wilderness: Fort Wayne, 1706–1828 (1976) (the seven-mile measure; the Little Turtle quotation from the Greenville councils); Allen County–Fort Wayne Historical Society, X Marks the Spot (1964) (the "Glorious Gate" marker text: "eight-mile carry," the Quebec–New Orleans route); History of Allen County, Indiana (Kingman Bros., 1880) (the "four feet of earth"); News-Sentinel, Cityscapes, "Coveted portage anchored early Fort Wayne," 19 October 1993 (the nine-mile usual length, the forty-mile drought carry, the flood passage, the 18,000-acre Aboite swamp and its drainage).

A lake stood here · the ice, Lake Maumee, and the Torrent

ABOUT 14,000 TO 17,000 YEARS AGO · THE FLOOD THAT CUT THE LITTLE RIVER VALLEY

Underneath everything at Fort Wayne is older rock — Silurian limestone and dolomite, laid down in a tropical sea more than 400 million years ago, reef rock among it — but almost none of it shows. What a person standing at the three rivers actually stands on is the wreckage of the last ice age. In the late Wisconsin glaciation, the Erie lobe of the Laurentide Ice Sheet ground southwestward across the Erie basin and over this ground, and as it retreated northeastward it dropped the ridges of unsorted debris — till — that geologists map as the Wabash moraine system. One of those ridges, the Fort Wayne Moraine, crossed the basin exactly where the city now stands, and for a time it worked as a dam.

Behind the dam, meltwater ponded into Glacial Lake Maumee, the first and highest of the ancestral lakes that preceded Lake Erie, occupying the Erie basin and drowning the low country northeast of the moraine — including the eastern part of present Allen County. The lake has a local christening: the name Lake Maumee was first applied in 1888 by G. R. Dryer of the Indiana Geological Survey, in his official report on the geology of Allen County. The classic survey of the lake is Leverett and Taylor's The Pleistocene of Indiana and Michigan and the History of the Great Lakes (U.S. Geological Survey, 1915). At its highest stage the lake's surface stood at about 800 feet above sea level — very near the elevation of the moraine crest the city occupies today, which is another way of saying that at the lake's maximum, the ground of downtown Fort Wayne was at or near the surface of a glacial lake, and the streets of the lake-plain neighborhoods to the east were on its bottom. As the ice front shifted, the lake stood at successive levels the surveys name as stages — Maumee I at about 800 feet, a lowest Maumee II at about 760 feet after new outlets opened toward the Grand River and Lake Chicago, and a Maumee III at about 780 feet draining through the Imlay channel in Michigan. At each stage the shoreline cut beach ridges of sand and gravel into the plain; the surveyors noted a century ago that those ridges, being the only dry footing across the flats, later became the routes of trails and highways.

Then the dam failed. Possibly helped by a last readvance of the ice at the lake's eastern end, the water rose against the Fort Wayne Moraine until it overtopped a sag — a low spot — in the moraine at present-day Fort Wayne, and the lake poured through into the ancestral Little River and down the Wabash. Geologists call the event the Maumee Torrent, or, in the title of the Geological Society of America's 2018 restudy of the upper Wabash valley, the Maumee Megaflood. How long ago it happened is a genuine disagreement in the literature, and both sides stand here: the traditional survey chronology, and most reference summaries, put the breach at roughly 14,000 years ago; Fleming and his co-authors' 2018 GSA study dates the breach of the moraine to about 17,000 years ago. The published range for the event is accordingly given as 14,000 to 17,000 years before present. What is not in dispute is the scale. The escaping lake scoured a channel one to two miles wide running southwest from Fort Wayne to the Wabash — the Wabash–Erie Channel — stripped the earlier sediment out of it in bulk, and deepened the valley floor by some twenty feet. A second, smaller outlet opened through Six-Mile Creek into the St. Marys and so to the same channel. Near Huntington, a sill of the hard Silurian reef limestone set a floor below which even the Torrent could not cut, and the flood, dropping its load and scouring onward down the Wabash, left the largest natural bedrock exposures in heavily glaciated northern Indiana along the upper Wabash gorge. The flood may have lasted only a few weeks. The landscape is still adjusting to it.

The channel the Torrent cut is still the largest single landform in Allen County — the Indiana Geological Survey's geology of the Little River valley calls it exactly that, the largest topographical feature in the county. It runs about twenty-four miles from the western bank of the St. Marys in Fort Wayne to the Forks of the Wabash below Huntington, and U.S. Route 24 follows it today. Into that oversized, abandoned floodway the drainage later reversed and settled: as much as thirty feet of fine sand, silt, and organic sediment accumulated on its floor, and the stream that inherited it is the Little River — a small, weak-water creek flowing through a valley cut for a megaflood. The broad, wet valley floor became, in time, a wetland of some 25,000 acres between Fort Wayne and Huntington, rich in game — the hunting ground the Little River Wetlands Project's history describes, and one of the reasons human beings kept returning to this corridor for the next ten thousand years.

Sources: Frank Leverett and Frank B. Taylor, The Pleistocene of Indiana and Michigan and the History of the Great Lakes, U.S. Geological Survey Monograph 53 (1915) (the lake stages, the 800-foot highest surface, the Fort Wayne outlet, the beach ridges as trail and highway routes); Anthony H. Fleming and others, "The Maumee Megaflood and the geomorphology, environmental geology, and Silurian–Holocene history of the upper Wabash Valley," Geological Society of America Field Guide (2018) (the ~17,000-year breach date, the weeks-long flood, the reef-rock sill and gorge); Indiana Geological Survey, "Geology of the Little River Valley" and Allen County — A Geologic Atlas (the channel as the county's largest topographical feature, the thirty feet of later fill, Dryer's 1888 naming of Lake Maumee in his Allen County report); Ohio Department of Natural Resources, Ohio Coastal Atlas, ch. 9 (the Maumee I/II/III stage elevations); Tony Fleming, "History and Physical Setting of Eagle Marsh," Little River Wetlands Project (the 25,000-acre wetland).

The Black Swamp · the lake bottom that walled off the east

1,500 SQUARE MILES OF WATER, CLAY, AND TIMBER · DRAINED 1859–1885

When Lake Maumee finally fell away, its southwestern floor did not become dry land. It became the Great Black Swamp. The lake plain was paved with clay-rich glacial till — in places twenty to eighty feet of it over the limestone — laid down nearly level, so that water stood on it instead of running off. On that drowned clay floor grew a dense swamp forest of elm, ash, and soft maple, broken by marsh and wet prairie: a network, in the standard summary, of forests, wetlands, and grasslands filling the whole country between the Maumee and its parallel beach ridges. The swamp's boundaries were set by the ancient beaches of Lakes Maumee and Whittlesey, and it stretched from the Fort Wayne ground eastward roughly a hundred miles — some accounts say 120 — to the Lake Erie shore near Port Clinton and Sandusky, and twenty-five to forty miles wide. Its area is commonly estimated at about 1,500 square miles; published estimates run higher, to some 2,600 square miles, and an Ohio Department of Natural Resources figure of 3,072,000 acres counts the Lake Erie marshes with it. The disagreement is over what to count as swamp, and it is carried here as a disagreement.

For Fort Wayne, the swamp is the eastern fact of the place. The city grew at the swamp's southwestern tip, on the first ground above the lake plain where the three rivers could be reached — and for the first decades of settlement, everything east of the city was effectively closed. Wheeled travel across the swamp in the wet season was measured in days or weeks when it was possible at all; the corduroy road built through the Maumee Road lands in 1825 was overlaid with gravel in 1838 and still dissolved into the mud each spring. The swamp fed the region's fevers, stopped armies' supply lines and settlers' wagons, and is the reason the Maumee valley's American settlement clung to the river corridors and the beach-ridge roads. It endured, as a landscape, from the falling of the glacial lake until the ditch laws: Ohio's ditching law of 1859 and the tile-drainage era emptied it between roughly 1859 and 1885, converting the lake bottom into some of the most productive farmland on the continent. The eastern tier of Allen County — the townships along the Maumee — is that lake bottom; the flat, black-soiled fields east of the city are the floor of Lake Maumee, farmed.

Sources: The Great Black Swamp, Ohio History Connection / Ohio Department of Natural Resources summaries (extent, dimensions, the 1859 ditch law, the 1859–1885 draining); Carolyn V. Platt, "The Great Black Swamp," Timeline (Ohio History Connection, 1987) (the swamp's character and the travel record); National Museum of the Great Lakes, Toledo (the swamp's reach inland to the three rivers at Fort Wayne).

The land as the first accounts describe it

CORN "AS FAR AS THE EYE CAN SEE" · THE WRITTEN LANDSCAPE, 1765–1790s

The first written descriptions of this ground were made by men who came to it through the portage, and what they describe is a worked, farmed, inhabited landscape — not a wilderness. George Croghan's 1765 report, the earliest official English account of the place, fixes the carrying place at about nine miles. In the winter of 1789–90, Henry Hay, a Detroit merchant's agent, lived at Kekionga and kept a diary of his stay and his visits roundabout — one of the few original eyewitness sources for the town and its country in those years. The description the state's own historical marker at the Kekionga site carries is of the town in the 1790s: a very large settlement, called Miami Town in the American records, standing on ground above the flood plain of the Maumee and the St. Joseph, and surrounded by wide expanses of corn fields, "as far as the eye can see." The corn was the landscape. Elmore Barce's The Land of the Miamis, working from the early accounts, lays out the town's ground in detail: the village running north from the confluence along the high east bank of the St. Joseph — the modern Lakeside shore — with the Indian gardens to its south, extensive corn fields and meadows east and north of the town, forest beyond the fields to the north and west, and the high, steep banks of the Maumee just below the junction. Down the rivers and up them it was the same pattern: cleared fields on the bottoms and terraces, oak and hickory woods on the rises, wet prairie and marsh in the summit flats and the Little River bottoms.

The most detailed early English description of a Miami town's country is one step removed, and it is printed here as exactly that. Christopher Gist, agent of the Ohio Company of Virginia, spent February 1751 at Pickawillany, the Miami town on the Great Miami River in Ohio that Memeskia's people had planted out from Kekionga only a few years before — and Gist's journal describes that sister town as a place of about four hundred families, "one of the strongest Towns upon this part of the Continent," set in country he praised in terms that became famous: "The Land … is very rich level and well timbered, some of the finest Meadows that can be … The Grass here grows to a great Height in the clear fields, of which there are a great number, & the Bottoms are full of white Clover, wild Rye and Blue Grass." It is a description of Pickawillany, not of Kekionga, and no honest record can move it. But it is what the river-bottom world of the Miamis looked like to a professional surveyor in 1751 — rich level bottoms, tall grass, cleared fields in number — and it is the closest contemporary picture of the world that stood at the three rivers in the same decade.

Sources: Indiana Historical Bureau, Kekionga marker, Edgewater Avenue, Fort Wayne (the 1790s description, the flood-plain siting, the corn fields); Elmore Barce, The Land of the Miamis (the town's ground, gardens, fields, and forests as laid out from the early accounts); Otho Winger, "The Indians Who Opposed Harmar," Ohio History Journal (Croghan's 1765 report and Henry Hay's 1789–90 diary as the original sources for Kekionga); Christopher Gist's journal, February 1751 (the Pickawillany description, quoted from the published journal).

The first peoples in the ground · ten thousand years of use

THE ARCHAEOLOGICAL RECORD, OLDEST FIRST

The state's historical marker at the Kekionga site states the span plainly: this area of the Three Rivers "was a site of settlement of Native Americans for as much as 10,000 years." The archaeology behind that sentence is a surface and survey record rather than a dug one — Indiana has no excavated, undisturbed Paleoindian site, and what is known of the first peoples here is known mostly from the distribution of their stone tools, recorded county by county. Stated at the level the record supports, the sequence at Fort Wayne's ground is this.

Paleoindian (about 10,000–7500 B.C. in the Indiana chronology). As the ice withdrew, the first peoples entered a cold, newly deglaciated country of spruce parkland and glacial lakes. Their signature is the fluted spear point — Clovis and Gainey forms in this region — and fluted points have been reported from nearly every Indiana county, in low densities. The specialist study is White and McCullough's Paleoindian Chronology and Technology in Northeastern Indiana (IPFW Archaeological Survey, Reports of Investigation 501, 2005), which assembled the northeastern Indiana find record. Its telling detail is the stone: some Clovis and Gainey points found in the northeast of the state are made of Wyandotte chert from southern Indiana, Attica chert from west-central Indiana, and Upper Mercer and Flint Ridge cherts from Ohio — raw material carried hundreds of miles, evidence of the long seasonal rounds (the literature models them on the north–south migrations of caribou between Ontario and the southern lakes) that the first peoples walked across this ground within a few thousand years of the Torrent. No Paleoindian camp in Allen County has been excavated in place; the Division of Historic Preservation and Archaeology's chronology is explicit that none has been anywhere in Indiana.

Archaic (about 8000–800 B.C.). The long Archaic occupation is the county's best-documented deep layer, because two university surveys worked Allen County ground systematically. At Fox Island County Park, southwest of the city — a wooded sand-dune complex ringed by wet prairie and marsh, with upland forest within a mile — Ball State University's Archaeological Resources Management Service recorded sixteen archaeological sites (Reports of Investigation 004, 1980). The artifacts showed an occupational sequence spanning approximately 8,000 years, from the Early Archaic through the historic Native occupation of the area, and a primary reliance on chert from near Huntington — stone outcropping in the very gorge the Maumee Torrent had cut through the reef rock downstream, so that the flood's geology and the Archaic people's toolkits are, literally, the same stone. Five years later the same laboratory surveyed 900 acres of the Wabash moraine in southwestern Allen County for the Greater Fort Wayne Chamber of Commerce Foundation (Reports of Investigation 015, 1985): in a 250-acre sample it recorded 54 sites, most of them single artifacts or small scatters — a density of one site to every 4.6 acres — and read the pattern as a resource-extraction locale: upland till country away from permanent water, visited again and again for dispersed resources rather than settled. Together the two surveys draw the Archaic map of the county: camps and villages on the dry ground by the water — dunes, terraces, moraine edges above the marshes — and a thin scatter of hunting and gathering traces everywhere else.

Glacial Kame (Late Archaic, roughly 1500–700 B.C. in the literature's range). The signature burial tradition of the northern Indiana–Ohio–Michigan lake country is named for this region's own geology. The Glacial Kame people buried their dead in the natural gravel hills — kames — that the melting ice had dropped across the country: tightly flexed burials, singly or in pairs, in circular pits in the gravel, a few burials in some kames and several dozen in others. The grave goods are what make the tradition recognizable across four modern states and Ontario: ornaments of copper, beads and gorgets of marine shell — above all the three-holed, sandal-sole gorget cut from the Gulf of Mexico Busycon conch — attesting trade or travel networks reaching from the Gulf to the upper lakes by 1000 B.C. The culture was defined in Cunningham's A Study of the Glacial Kame Culture in Michigan, Ohio, and Indiana (University of Michigan, 1948); its type site is the Ridgeway kame in Hardin County, Ohio, uncovered by railroad gravel-digging in 1856. Northeastern Indiana lies inside the tradition's mapped range, and its kame cemeteries were recorded in the same gravel-working way — a fact with a consequence the record states plainly: most Glacial Kame cemeteries in the region were found by the gravel pit, and many were destroyed by it, so the surviving record is richest where a supervisor or a collector happened to write things down. Dating in the modern summaries runs from about 1500 to 1000 B.C. (the Oxford reference formulation) with some county histories carrying the fluorescence to about 700 B.C.; at the Zimmerman kame in Ohio the tradition's latest burials are accompanied by the region's earliest basic pottery, at the threshold of the Woodland period.

Woodland (about 800 B.C.–A.D. 1650). For the mound-building Woodland centuries, Allen County's record thins — and the honest account of why is in the next section. At the regional scale, northern Indiana's Middle Woodland is the Goodall tradition, a Hopewellian pattern (about 200 B.C.–A.D. 500) of mound and earthwork burial spread across northern Indiana and western Michigan and defined, like Glacial Kame before it, by cemeteries in glacial gravel ridges. The great Adena and Hopewell earthwork centers, however, lay south and east — in the Whitewater and Ohio valleys and southern Indiana — and Allen County stood at the northern margin of that world. Its Woodland record in the professional surveys is real but modest: Woodland-period material among the Fox Island sites, and, for the Late Woodland, a determination that matters to the last section of this record — the Fox Island Late Woodland occupation was affiliated with the Younge Tradition of southeastern Michigan, the Western Basin world of the Maumee and western Lake Erie: settled, corn-growing village peoples of the lake plain, the direct predecessors, in place and in lifeway, of the world the French found at Kekionga.

Sources: Indiana Department of Natural Resources, Division of Historic Preservation and Archaeology, "Cultural Chronology of Indiana" and Early Peoples of Indiana (the period framework; fluted points in nearly every county; no in-situ Paleoindian excavation in Indiana); Andrew A. White and Robert G. McCullough, Paleoindian Chronology and Technology in Northeastern Indiana, IPFW Archaeological Survey ROI 501 (2005) (the northeastern Indiana find record and its nonlocal cherts); Donald R. Cochran, An Archaeological Assessment of Fox Island County Park, Ball State University ROI 004 (1980) (sixteen sites, the 8,000-year sequence, the Huntington chert, the Younge Tradition affiliation); Donald R. Cochran and Jeanette E. Buehrig, An Archaeological Survey on the Wabash Moraine, ROI 015 (1985) (54 sites, site density, the resource-extraction reading); Wilbur M. Cunningham, A Study of the Glacial Kame Culture in Michigan, Ohio, and Indiana (1948), with the Oxford Dictionary of Archaeology formulation of its dates and Christine K. Keller's Ball State study of the sandal-sole gorgets (2008); Goodall focus summaries, Ball State Applied Anthropology Laboratories.

Mounds and earthworks · the antiquarian record

WHAT THE COUNTY HISTORIES RECORDED BEFORE THE PLOW AND THE GRAVEL PIT TOOK IT

Almost everything known about Allen County's mounds comes from one generation of local antiquarians, and it must be read as what it is: a 19th-century account, written before professional archaeology existed here, describing works that were already being plowed down as the writers watched. The account is R. S. Robertson's chapter "Prehistoric Remains" in the History of Allen County, Indiana (Kingman Bros., 1880), repeated with little change in Brant & Fuller's Valley of the Upper Maumee River (1889). Its framing — a vanished "Mound-builder" race distinct from the Indians — was the standard theory of its decade and is not the modern one: archaeology now attributes the mounds to the ancestors of Native peoples, Woodland peoples among them. The observations underneath the framing, however, were made on the ground by a man who walked to the sites, and they are the only record most of these works will ever have.

Robertson's map of the county's earthworks has a clear shape. The mounds and earthworks of the region crowd thick along the Cedar Creek valley in DeKalb County, thin as they come south into Allen County, are "few, if any … along the Maumee," and are wholly wanting in the southern part of the county. What the county had, it had along the St. Joseph and its Cedar Creek tributary. His inventory, as he gives it: on Cedar Creek near Stoner's station, on the high ground between Cedar and Willow creeks, a group of four mounds — two in a line north and south about forty feet apart, two more some fifteen rods east in a line nearly east and west; three had been partially excavated years before and were said to have contained a large number of human bones, arrowheads, and copper ornaments, and the fourth, excavated in Robertson's presence, disclosed only lumps of charcoal and a layer of hard-baked earth near its base. At Cedarville, on the St. Joseph near the mouth of Cedar Creek, three mounds about a hundred feet apart in a line running northwest, parallel to the river; and at the creek's mouth itself the most southern mound in the county. Down the St. Joseph on its west side, opposite Antrap's Mill, stood the county's one recorded fortification: a semi-circular "fort" with its ends on the river bank, about 600 feet in arc, its earthwork still nearly two feet high when he saw it, with a well-defined ditch on the outside.

Robertson also recorded the historic-period ground, and the distinction he drew is itself evidence: mound burial, he noted, divided the older peoples from the Indians of the historic era, who rarely raised mounds over their dead. The three prominent Indian burying grounds he names are a map of the Kekionga world in miniature — on the series of sand hills in the west end of Fort Wayne; on the St. Joseph just north of the city, near the site of the Miami town; and at Cedarville, on the banks of the St. Joseph. Stone implements, he adds, had been found in the county in considerable quantity, most of them belonging to the historic peoples. That is the whole of the county's mound record as the 19th century left it: a handful of small works along one river corridor, a semicircular earthwork, three burying grounds — and a county history honest enough to say, in its first paragraph on the subject, that Allen County's monuments were "not as many, nor so extensive, as ones found in Ohio or to the southern part of Indiana." No Allen County mound from Robertson's list is known to survive as a protected site today, and none was professionally excavated; the antiquarian chapter is the record.

Sources: R. S. Robertson, "Prehistoric Remains," in History of Allen County, Indiana (Kingman Bros., 1880), and the same account in Valley of the Upper Maumee River, vol. I (Brant & Fuller, 1889) — quoted and paraphrased as an account of its time, its "Mound-builder" framing identified as the period's theory where the text relies on it.

Kekionga as a place · the town on the eve of the forts

A CLUSTER OF VILLAGES AT THE CONFLUENCE, AS THE EARLY ACCOUNTS LAY IT OUT

When written records begin, the place at the three rivers is not one town but a cluster of them, spread across both banks of both rivers at the head of the Maumee — the capital country of the Miami, known in their language as Kekionga and to the incoming French and English as Miami Town. The peoples, chiefs, councils, and wars of that world belong to the Tribes section and the Story; what belongs here is the physical layout, which the early accounts fix with unusual precision because the ground plan still shows through the modern city.

The principal Miami town stood on the east side of the St. Joseph, its southern end at the point of junction with the St. Marys, extending north along the high bank — the shore of today's Lakeside neighborhood, along present St. Joe Boulevard and Edgewater Avenue, at the eastern end of the present Lakeside bridge. It stood, the marker's phrase runs, on ground above the flood plain, and its working landscape ran with it: gardens immediately south of the town, the great corn fields and meadows east and north of it, forest closing in beyond the fields. Close around it stood the satellite towns. On the east side of the St. Joseph also stood the town of the head chief Pecanne (Pecan). On the western bank of the St. Joseph, facing the main town across the river, was LeGris' Town, a mixed village of French and Indians, ringed by its own corn fields, with the little wooded creek called Spy Run running south of it and the St. Marys beyond. The Allen County–Fort Wayne Historical Society's 1957 account places the French village of "Miami town" in the southeastern pocket of present Spy Run, across the river from Kekionga at the eastern end of the Lakeside bridge.

The fullest count of the cluster is the one H. S. Knapp's history of the Maumee Valley preserved for the moment of Harmar's approach in 1790, and it is the closest thing the record has to a census of the place on the eve of its destruction: the main Miami village at Lakeside; a second Miami village across the river between the St. Marys and the St. Joseph, of thirty houses; a Shawnee village, Chillicothe, two miles down the Maumee, of fifty-eight houses (the ACGSI's modern siting puts it south of the Catholic Cemetery on Lake Avenue, on both sides of the Maumee west of Coliseum Boulevard, in the same Lakeside ground), with another Shawnee village of eighteen houses across the river from it; two Delaware villages two miles up the St. Marys, of forty-five houses between them; and another Delaware village three miles up the St. Joseph. The houses in all the villages were counted at one hundred eighty-five — with the count's own caveat attached: the original number was not known, because the inhabitants had burned many of their houses before the army arrived.

Beyond the confluence cluster, the portage world had an outer ring, and its anchor was on the Eel River. Little Turtle's village stood on the Eel River about sixteen miles northwest of Kekionga, and two miles up the river from it stood the famous Eel River trading post, where furs were collected to be brought down and across the portage to the Maumee. Between the Eel River towns and the confluence ran the trail to the carrying place; between the confluence and the lake ran the Maumee; and the whole arrangement — capital at the gate, chiefs' towns up the feeder rivers, the trading post at the portage's far reach — is the physical form of the words Little Turtle used for it: a gate, with everything passing through.

The European posts, when they came, were planted into this layout rather than onto empty ground, and their siting is part of the place's record. The first French fort in the area is marked just south of the St. Marys bank on the east side of Van Buren Street, in the city's modern street grid; the French post and its successor garrisons stood in the Spy Run pocket and along the St. Marys within the town cluster's own ground. Five forts would eventually stand at Fort Wayne between the first French post and the last American one, whose narrative belongs to the Story. The last fact of the place, before the record turns to forts, is a date the marker carries: Kekionga "remained a place of native settlement until the Miami were forcibly removed from Indiana in 1846." The city and the town shared the ground for a generation. What the town was as a people — its bands, its chiefs, its confederacy, its removal — is told in Tribes; what its ground legally became, treaty by treaty and deed by deed, is told in The Land.

Sources: Elmore Barce, The Land of the Miamis (the main town's siting along Lakeside, Pecanne's town, LeGris' Town, the gardens, fields, and forests); H. S. Knapp, History of the Maumee Valley, as preserved in Otho Winger, "The Indians Who Opposed Harmar," Ohio History Journal (the seven-village count of 1790, the house numbers, Little Turtle's Eel River village and the trading post); Allen County–Fort Wayne Historical Society, The Wabash and Erie Canal and Historic Sites of Fort Wayne, Old Fort News (1957) (Kekionga at the eastern end of the Lakeside bridge along St. Joe Boulevard, the French village in the Spy Run pocket, the first French fort marker south of the St. Marys at Van Buren Street); Indiana Historical Bureau, Kekionga marker (the flood-plain siting and the 1846 removal date); Allen County Genealogical Society of Indiana (the siting of the Shawnee Chillicothe in the Lakeside ground).