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Lillinonah Trail
The Lillinonah Trail is a '' Blue-Blazed'' hiking trail "system" in the lower Housatonic River valley in Fairfield County and, today, is entirely in Newtown. Most of the trail is in the upper block of Paugussett State Forest. The mainline (official "Blue-Blazed") trail circles the Paugussett State Forest "upper block". The west, north and east portions of the trail are shared with the northern section of Al's Trail—a ten-mile trail in Newtown. The Lillinonah Trail today is composed of four sides in a square "loop". Notable features include the Hanover Road parking lot and boat launch, semi-obscured (by trees) scenic views of Pond Brook inlet and Lake Lillinonah (Housatonic River), a climb to a high point of , a very large oak tree, several stone fences and foundations and a demonstration of a maple sugaring technique known as "sugarbush" near the Echo Valley Road parking lot.Connecticut Walk Book: A Trail Guide to the Connecticut Outdoors. 17th Edition. The Connecticut F ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Newtown, Connecticut
Newtown is a town in Fairfield County, Connecticut, United States. It is part of the Greater Danbury metropolitan area as well as the New York metropolitan area. Newtown was founded in 1705, and later incorporated in 1711. As of the 2020 census, its population was 27,173. History In 1705, English colonists purchased the Townsite from the Pohtatuck Indians, a branch of the Pasgussett. It was originally known as Quanneapague. Settled by migrants from Stratford and incorporated in 1711, Newtown residents had many business and trading ties with the English. It was a stronghold of Tory sentiment during the early Revolutionary War. Late in the war, French General Rochambeau and his troops encamped there in 1781 during their celebrated march on their way to the siege of Yorktown, Virginia, which ended the Revolution. An important crossroads throughout its early history, the village of Hawleyville briefly emerged as a railroad center. The town's population grew to over 4,000 . ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Zoar
Lake Zoar is a reservoir on the Housatonic River in the U.S. state of Connecticut. It was formed by the completion of the Stevenson Dam, which flooded an area of Oxford and Stevenson named "Pleasantvale" or "Pleasant Vale". The towns of Monroe, Newtown, Oxford, and Southbury border Lake Zoar. The name Zoar originates from corner of Newtown and Monroe that once called itself Zoar after the Biblical city Zoara near the Dead Sea. Lake Zoar Authority The Lake Zoar Authority (LZA) is an organization for promoting safety on the lake and improving water quality. The members represent the four towns bordering the lake and meet on a monthly basis. Authority is granted through the Connecticut General Statutes, section 7-151a (of the 1969 supplement). Notable events *1984: Joyce Stochmal, 19, murdered and her body dumped into the lake. *November 1986: Richard Crafts murdered his wife Helle Crafts in Newtown, froze the body, cut it up with a chainsaw and finally put it through a woodchi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shepaug River
The Shepaug River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed April 1, 2011 river in western Connecticut, in the United States. The river originates at the south end of the Shepaug Reservoir in the town of Warren. The reservoir is fed at its northern end by the West Branch Shepaug River and East Branch Shepaug River. The Shepaug runs south through Washington, Roxbury, and Southbury, where it joins the Housatonic River at Lake Lillinonah () dammed by the hydroelectric Shepaug Dam. The river's watershed area comprises approximately , which encompasses the towns of Cornwall, Goshen, Torrington, Warren, Litchfield, Washington, Morris, New Milford, Roxbury, Bridgewater, and Southbury. The vicinity of the Shepaug River has been inhabited by humans since around 4000 B.C., though according to archaeology, there was a decline in population around 1000 B.C. The river is a primary source of drinking water for the c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Lillinonah
Lake Lillinonah is a manmade lake located in Fairfield, Litchfield and New Haven counties of Western Connecticut, approximately northeast of New York City. It is the second largest lake in Connecticut, smaller only than Candlewood Lake. The lake is bordered by six towns: Brookfield, Bridgewater, Newtown, New Milford, Roxbury, and Southbury. It was formed in 1955 by impoundment of the Housatonic River and the Shepaug River by the Shepaug Dam which was built by the Connecticut Light and Power Company. Some of the most expensive real estate in the Greater Danbury Greater Danbury, also known as the Housatonic Valley Region, is a region in the state of Connecticut centered on the city of Danbury. It consists of the city of Danbury and adjacent towns in the areas around the Housatonic River and the Still Ri ... area is located on the shores of the lake, in the towns of Brookfield, Bridgewater and Newtown. References External links www.lakelillinonahauthority. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pond Brook
A pond is an area filled with water, either natural or artificial, that is smaller than a lake. Defining them to be less than in area, less than deep, and with less than 30% emergent vegetation helps in distinguishing their ecology from that of lakes and wetlands.Clegg, J. (1986). Observer's Book of Pond Life. Frederick Warne, London Ponds can be created by a wide variety of natural processes (e.g. on floodplains as cutoff river channels, by glacial processes, by peatland formation, in coastal dune systems, by beavers), or they can simply be isolated depressions (such as a kettle hole, vernal pool, prairie pothole, or simply natural undulations in undrained land) filled by runoff, groundwater, or precipitation, or all three of these. They can be further divided into four zones: vegetation zone, open water, bottom mud and surface film. The size and depth of ponds often varies greatly with the time of year; many ponds are produced by spring flooding from rivers. Ponds m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
