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Before the City — Lakeville
Pass 1 laid this ground's frame — the survey grid, the cession lines, the plotted taking. this section goes under it: the town stands on stacked glacial drift laid by more than one ice lobe, on a clay till plain that held its water as marsh until men ditched it, south of a river whose valley is a reversed meltwater channel and beside — not under — a glacial lake whose drained bed became the Grand Kankakee Marsh. Two small lakes survive of the township's original wet ground, and the township's water, when it leaves, runs to the Gulf of Mexico. Every statement below carries its source class; where the record ends, the file says so.
Three lobes, and the multilobe revision
Howard 1907 · IGS 2024
The classic account meets the modern framework — and the ground turns out to be more than one ice sheet's work. Howard's county history states that three glacial lobes met at South Bend: the Michigan Lobe, the Saginaw Lobe, and…
Drift, bedrock, the till plain, and the moraine rim
The ground's dimensions
Two hundred feet of drift over shale, a clay plain under the town, and a moraine belt on the county's western rim. Howard reckoned the county's drift "will probably average two hundred feet", the only piercing to rock in his day…
The meltwater reversal, and the Torrent
The valley that changed direction
The St. Joseph once ran to the Kankakee; the capture that reversed it is the county's great meltwater event. The basin's deglacial drainage ran first south to the Wabash, then west to the Kankakee, before the final drainage to…
Glacial Lake Kankakee: beside it, not under it
c. 14,000–13,000 years ago
The township fed the lake meltwater across its surface; the lake's own waters ended southwest of South Bend. Glacial Lake Kankakee formed about 14,000 years ago from the outwash of all three lobes, covered more than 3,000 square…
The two surviving lakes, whole
Riddles Lake · Pleasant Lake
Round, kettle-shaped survivors of the wet ground — measured by the state, gauged by the USGS, and thinner in the record than they look. Howard, citing the state geologist's 1900 report, already described the county's lakes as…
The drainage divide: this ground runs to the Gulf
The headline answer
Union Township drains south to the Mississippi basin — not north to Lake Michigan. The chain, link by link. (1) The state's potentiometric map of the county (IDNR Division of Water, 2011) splits the county between the St. Joseph…
The marsh that was ditched away
Settlement to 1923
Headwater marsh, not the great marsh — and the ditching era that unmade both. Howard states the township's original ground directly: "It was chiefly heavily timbered clay and marsh land; and while the soil was a strong and…
The fossil test: negative for this township
Searched, not assumed
No documented mastodon, mammoth or fossil find in Union Township — in a region where ditching struck them regularly. The test was run across the published and indexed record — proboscidean occurrence searches for the county and…
The record's edge, and the peoples
What a fuller record requires
The limits of this section, stated — and the human ground pointed to where it is carried whole. There is no modern geological-survey county monograph for St. Joseph County in the record reached: the detailed USGS work covers only…
The before-the-city file's geology and peoples stand banked; its audit rows are the sequence and the mechanisms — who was first, in what sense; the first passage, dated; the traders, person by person; and the machinery by which one band stayed while the rest were removed. This addendum states the two "first" facts as two, dates the passage to the month with its conflict whole, and reads the exception in the statute that codified it.
The peoples sequence, stated as two facts
Two different "first peoples" stand for this ground, and the build prints them as two facts, never as one. First in the record: the unnamed makers of the finds Chapman reports in Sections 6 and 8 of this township — stone-walled…
The first passage: La Salle at the portage, December 1679 — the 3rd or the 5th
The first documented European passage of this valley is dated to the month — and its day stands in conflict, printed whole. The course: René-Robert Cavelier, Sieur de La Salle, built Fort Miami at the St. Joseph River's mouth in…
The trader line, person by person
Five men carry the valley's trade era in the reached record; their posts stood on the river and the portage, not on this township's ground. William Burnett — the line's head: "the first successful trader to occupy the St. Joseph…
How one band stayed: the mechanism, read in the statute
L. 103-323 (1994)
The Pokagon Band stayed by a negotiated article, a Catholic identity the treaty itself recited, a land purchase, and — once — a judge: the mechanism stands in four documented parts. The article: the United States' own findings…
The second removal, 1840: the located record is a trader's papers
The 1840 removal from this valley is documented, located, and unread — its archive is named here in full. The located record: the Patrick Marantette Papers (1833–1879) at the Archives of the University of Notre Dame …