Glen Ellyn, Illinois

Glen Ellyn is a village in DuPage County, Illinois, United States. As of the 2010 Census, the village population was 27,450.

History

The first landowner in Glen Ellyn was Deacon Winslow Churchill. He and his family moved to Glen Ellyn from New York in 1834. Other newcomers to the area built town necessities such as a tavern and school.

Moses Stacy, a soldier in the War of 1812, arrived here in 1835. His inn, Stacy's Tavern, built in 1846 and his second home, was a halfway stop between Chicago and the Fox River Valley and a probable stop for Galena, Illinois stagecoaches on their way to Rockford, Illinois. Stacy's Tavern, now a historical monument, stands at what is now the intersection of Geneva Road and Main Street.

In 1849, construction of a railroad line through Glen Ellyn was finished. The area around the railroad became the center of the town. At first, trains running through the town on the railway did not stop there. A local man named Lewey Q. Newton made an offer to the railroad company: Newton would build a depot and water tank out of his own pocket if the railroad would require trains to stop there. The depot that Newton built became known as Newtown Station.

Glen

A glen is a valley, typically one that is long, deep, and often glacially U-shaped, or one with a watercourse running through it. Whittow defines it as a "Scottish term for a deep valley in the Highlands" that is "narrower than a strath".

The word is Goidelic in origin: gleann in Irish and Scottish Gaelic, glion in Manx. In Manx, glan is also to be found meaning glen. It is cognate with Welsh glyn. The word is sometimes found in tautological placenames where its meaning was opaque to a new linguistic community, an example perhaps being Glendale (literally "valley valley") which is a combination of Norse "dale" and Gaelic "glen".

As the name of a river, it is thought to derive from the Irish word glan meaning clean, or the Welsh word gleindid meaning purity. An example is the Glens of Antrim in Northern Ireland where nine glens radiate out from the Antrim plateau to the sea along the coast between Ballycastle and Larne.

In the Finger Lakes Region of New York State, the southern ends of Seneca Lake and Cayuga Lake in particular are etched with glens, although in this region the term "glen" refers most frequently to a narrow gorge, as opposed to a wider valley or strath. The steep hills surrounding these lakes are filled with loose shale from glacial moraines. This material has eroded over the past 10,000 years to produce rocky glens (e.g. Watkins Glen and Treman State Parks) and waterfalls (e.g., Taughannock Falls) as rainfall has descended toward the lakes below.