During the melting of the Wisconsin Glacier about 10, 000 years ago, a lake formed in present-day Indiana, comparable to one of the modern Great Lakes.

Aggradational floodplain: This floodplain of a small meander ing stream in La Plata County, Colorado, is underlain by silt deposited above a dam formed by a terminal moraine left by the Wisconsin glaciation | Wisconsin Glacier.

The Lehigh Valley starts at the terminal moraine of the Wisconsin Glacier slightly north of Belvidere.

Then the Wisconsin Glacier covered the northern part of the county from 21, 000 to 13, 000 BC.

After the Wisconsin Glacier melted around 13, 000 B. C., the area slowly warmed.

The Wisconsin Glacier in Warren and Sussex County was retreating northward.

This was formed during the melting of the Wisconsin Glacier about 10, 000 years before present.

The topography of Champaign County was formed by the Wisconsin Glacier about 20, 000 years before the present.

After the retreat of the Wisconsin Glacier, a mighty glacial lake called Glacial Lake Passaic formed in this area that, about 15, 000 to 11, 000 years ago, extended for in length and was wide.

Amerinds occupied the areas that would become New Jersey and Madison following the retreat of the Wisconsin Glacier for many thousands of years.

The area was first tundra when the Wisconsin Glacier melted and then as the area warmed formed taiga / boreal forests, along with vast meadows.

After the Wisconsin Glacier melted around 13, 000 BC, half of Parsippany was filled with water as this was Lake Passaic.

The Wisconsin Glacier covered all of Branchville from 21, 000 BC to 13, 000 BC, covering the top of Kittatinny Mountain.

The Wisconsin Glacier covered all of the township from 21, 000 BC to 13, 000 BC.

About 18, 000 years ago, Connecticut, Long Island Sound, and much of Long Island were covered by a thick sheet of ice, part of the Late Wisconsin Glacier.

After the Wisconsin Glacier melted, grasses and trees slowly grew.

Approximately 17, 000 years ago the terminal moraine of the receding Wisconsin Glacier that formed Long Island established a string of hills and kettles in the northern part of the park and a lower lying outwash plain in the southern part.

When the Wisconsin Glacier melted 14, 000 years ago, part of the meltwaters formed the proglacial Lake Maumee, the ancestor to Lake Erie.

When the Wisconsin Glacier began melting back to the north about 10, 000 years ago, the landscape would undergo dramatic changes.

The lake was formed of waters released by the retreating Wisconsin Glacier, which had pushed large quantities of earth and rock ahead of its advance, blocking the previous natural drainage of the ancestral Passaic River through a gap in the central Watchung Mountains.

This changed when the Wisconsin Glacier, a massive continental ice sheet which formed during the last ice age, advanced on the region and permanently plugged the gap.

Approximately 20, 000 years ago, the Wisconsin Glacier advanced across northern New Jersey, expanding differentially across the land as it encountered variable terrain.

The Hackensack lobe of the Wisconsin Glacier piled a massive moraine into the Short Hills Gap and northern Blue Brook Valley, effectively creating a permanent dam even after the ice began retreating to the north.

The first VM / CMS TCP / IP stack came from the University of Wisconsin.

According to Ojibwa oral history, Spirit Island, located near the Spirit Valley neighborhood, was the " Sixth Stopping Place " where the northern and southern branches of the Ojibwa Nation came together and then proceeded to their " Seventh Stopping Place " near the present city of La Pointe, Wisconsin.

The first wave of expansion to the league came in 1996 as the Northern League entered Wisconsin and North Dakota.

Loggers came up the rivers and floated pine logs out in spring and early summer log drives, down the Big Rib River into the Wisconsin River, down the Black River to the south, and west down the Jump and the Yellow River into the Chippewa.

Many of the immigrants came from New Iceland near Lake Winnipeg, along with other Icelanders who moved into the area from colonies in Wisconsin.

Initially trains had to be ferried across the river between Marquette and Prairie du Chien, Wisconsin, in order to continue their journey, but this system came to an end when Prairie du Chien businessman John Lawler had a permanent pontoon bridge built to connect the two cities ' rail lines.

a Norwegian, settled in the western half of the southwest quadrant of section 36 in 1856 and John Osmunsen, another Norwegian, came from Wisconsin and settled on the eastern half of the southeast quadrant of the same section the followunbg year.

In 1855 John L. Johnson came to the township from Wisconsin and built a sod shanty in a grove of trees in section 4 that had a large, red rock in it.

Frazier came from Wisconsin in 1881 to become principal of the Verndale school.

The figures were quoted in the Madison Land Company's brochure by Bishop Hugh Miller Thompson, the second Episcopal Bishop of the Diocese of Mississippi and a Madison resident, who originally came from Wisconsin.

In 1857 John and Margaret Prey, adult sons, John W., Thomas, and William, and teenage children, David and Rebecca, came from Wisconsin to preempt land near the proposed town called " Olathe.

In 1951 Alfred Colby Hockings and his wife — he was a well-known illustrator for Field and Stream magazine, originally from Wisconsin but most recently living in the artists ' community of Tryon, North Carolina —- built a home up the street from the Gasques and Sorrys and across from the Baarslags ; at almost the same time another Dutch family — Gerbrand and Nellie Poster, the son-in-law and daughter of the Baarslags, came down from New York City to visit her parents for Christmas, decided to stay, and built a home next door to her parents.

In 1910 Amanda Stoltzfus organized the Tuleta Agriculture High School, the first of its kind in Texas ; its faculty came from such prestigious institutions as Smith College and the University of Wisconsin.

About 177 firefighters from 20 fire departments responded, not counting the Wisconsin Department of Natural Resources ( DNR ) firefighters, who came from as far away as Hayward.

The late H. L. Russell, Dean of the College of Agriculture at the University of Wisconsin – Madison, conceived the idea of school forests when he came upon them while traveling in Australia.

When the Wisconsin Central / Soo railroad came thru the area, there was a depot stop created as Camp Lake.

The largest town in Valdres is Fagernes, but many immigrants arriving in Wisconsin came from the valleys of Vestre Slidre and Øystre Slidre, when hunger ( sult ) in these rocky hillside farms was far from unheard of.

At the time when Wisconsin was a frontier territory, The Wades came to establish a village on the developing frontier.

In 1891 a line was built in from Centralia ( now Wisconsin Rapids ), a line was built out to Greenwood, and a line from Wausau came in to Marshfield from the north.

Lincoln, Kewaunee County, Wisconsin, third most Belgian American town, was originally named Grandlez, after Grand-Leez where Belgian founding migrants came from.

Especially Mexicans / Latinos came into states like Illinois ( mostly in Chicagoland ), Indiana especially the Northern section, Iowa, Kansas, Michigan ( i. e. the Detroit metropolitan area ), Minnesota, Missouri, Nebraska and Wisconsin due to needs of the region's industrial manufacturing base.

The first full car of freight came over the line to Ahnapee ( now Algoma, Wisconsin ) in September 1892.

John B. Arpin and his twin brother Antoine came from Quebec and had been logging in this part of Wisconsin since the 1860s.

Perhaps the most influential musical output of Wisconsin came from Grafton, Ozaukee County during the 1920s, when Paramount Records released a series of blues and jazz recordings by artists from the South.