Lake Tonawanda | |
---|---|
Location | North America |
Group | Great Lakes |
Coordinates | 43°04′55″N78°44′56″W / 43.0819°N 78.7488°W |
Lake type | former lake |
Etymology | Tonawanda, which means "swift waters," was the name given to the area by Neuter and Erie Indians, the area's original inhabitants, and it probably refers to the Niagara River current. Early Visitors. |
Primary inflows | Early Lake Erie |
Primary outflows | Lake Iroquois |
Basin countries | United States |
First flooded | 10,000 years before present |
Max. length | 42 mi (68 km) |
Max. width | 15 mi (24 km) |
Surface elevation | 476 ft (145 m) |
References | Ernest H. Muller (1977), LATE GLACIAL AND EARLY POSTGLACIAL ENVIRONMENTS IN WESTERN NEW YORK; Annals of the New York Academy of Sciences 288 |
Lake Tonawanda was a prehistoric lake that existed approximately 10,000 years ago at the end of the last ice age, in Western New York, United States. [1]
The lake existed on the southern (upper) side of the Niagara Escarpment east of the present course of the Niagara River between Early Lake Erie to the south and Glacial Lake Iroquois (the ancestor of Lake Ontario) to the north. During the retreat of the glaciers, the water levels of the Great Lakes were higher. Lake Tonawanda was created and fed by the elevated waters of Lake Erie. Lake Tonawanda itself was drained into Lake Ontario by a series of falls over the escarpment, including one at present day Lockport, New York.
The lake evaporated when the waters of Lake Erie dropped below the level of the feeder streams to the lake. Subsequently Lake Erie drained over the escarpment entirely through Niagara Falls, which marks roughly the western terminus of the former lake bed.
The remains of the previous falls, which rivaled Niagara Falls in grandeur, can be seen along the escarpment. The sinking of homes in the lakebed has been an ongoing problem in communities such as Amherst, New York.
The Erie Canal is a historic canal in upstate New York that runs east–west between the Hudson River and Lake Erie. Completed in 1825, the canal was the first navigable waterway connecting the Atlantic Ocean to the Great Lakes, vastly reducing the costs of transporting people and goods across the Appalachians. In effect, the canal accelerated the settlement of the Great Lakes region, the westward expansion of the United States, and the economic ascendancy of New York State. It has been called "The Nation's First Superhighway."
The Niagara River is a river that flows north from Lake Erie to Lake Ontario. It forms part of the border between the province of Ontario in Canada and the state of New York in the United States. There are differing theories as to the origin of the river's name. According to Iroquoian scholar Bruce Trigger, Niagara is derived from the name given to a branch of the locally residing native Neutral Confederacy, who are described as being called the Niagagarega people on several late-17th-century French maps of the area. According to George R. Stewart, it comes from the name of an Iroquois town called Ongniaahra, meaning "point of land cut in two".
Erie County is a county along the shore of Lake Erie in western New York State. As of the 2020 census, the population was 954,236. The county seat is Buffalo, which makes up about 28% of the county's population. Both the county and Lake Erie were named for the regional Iroquoian language-speaking Erie tribe of Native Americans, who lived in the area before 1654. They were later pushed out by the more powerful Iroquoian nations tribes.
Niagara County is in the U.S. state of New York. As of the 2020 census, the population was 212,666. The county seat is Lockport. The county name is from the Iroquois word Onguiaahra; meaning the strait or thunder of waters.
Pendleton is a town on the southern edge of Niagara County, New York, United States. It is east of the city of Niagara Falls and southwest of the city of Lockport. The population was 6,397 at the 2010 census.
The Niagara Escarpment is a long escarpment, or cuesta, in Canada and the United States that starts from the south shore of Lake Ontario westward, circumscribes the top of the Great Lakes Basin running from New York through Ontario, Michigan, and Wisconsin. The escarpment is the cliff over which the Niagara River plunges at Niagara Falls, for which it is named.
Tonawanda is a town in Erie County, New York, United States. As of the 2020 census, the town had a population of 72,636. The town is at the north border of the county and is the northern inner ring suburb of Buffalo. It is sometimes referred to, along with its constituent village of Kenmore, as "Ken-Ton". The town was established in 1836, and up to 1903 it included what is now the city of Tonawanda.
Tonawanda Creek is a small tributary of the Niagara River in Western New York, United States. After rising in Wyoming County, the stream flows through Genesee County before forming part of the boundary between Erie County and Niagara County.
Glacial Lake Iroquois was a prehistoric proglacial lake that existed at the end of the last ice age approximately 13,000 years ago. The lake was essentially an enlargement of the present Lake Ontario that formed because the St. Lawrence River downstream from the lake was blocked by the ice sheet near the present Thousand Islands. The level of the lake was approximately 30 m (~100 ft) above the present level of Lake Ontario.
Interstate 990 (I-990) is an auxiliary Interstate Highway located entirely within the town of Amherst in Erie County, New York, in the United States. It runs in a roughly north–south direction for 6.35 miles (10.22 km) through the southwestern and central parts of Amherst from an interchange with I-290 north of Buffalo to an intersection with New York Route 263 south of Lockport. The highway serves as a connection between Buffalo, the University at Buffalo, and Lockport. Like I-590 in nearby Rochester, I-990 does not physically meet I-90, its parent Interstate Highway; instead, the highway makes the connection by way of a "sibling" highway (I-290). I-990 is the highest numbered Interstate Highway in the US.
The Buffalo and Niagara Falls Railroad was a part of the New York Central Railroad system, connecting Buffalo, New York to Niagara Falls. It is still used by CSX for freight and Amtrak for passenger service.
Lake Algonquin was a prehistoric proglacial lake that existed in east-central North America at the time of the last ice age. Parts of the former lake are now Lake Huron, Georgian Bay, Lake Superior, Lake Michigan, Lake Nipigon, and Lake Nipissing.
New York State Route 425 (NY 425) is a north–south state highway in the western portion of New York in the United States. It extends for 23.85 miles (38.38 km) from an interchange with Interstate 290 (I-290) in the town of Tonawanda to an intersection with NY 18 on the shore of Lake Ontario in the village of Wilson. As it heads north, it connects to several regionally important routes, including U.S. Route 62 (US 62) and NY 104. The section between I-290 and the city of North Tonawanda is a four-lane arterial known as the Twin Cities Memorial Highway. North of the city, the route is primarily a two-lane rural highway.
Early Lake Erie was a prehistoric proglacial lake that existed at the end of the last ice age approximately 13,000 years ago. The early Erie fed waters to Glacial Lake Iroquois.
Ellicott Creek is a stream in Western New York, United States. It is a tributary of Tonawanda Creek, which in turn flows into the Niagara River.
New York State Route 265 (NY 265) is a 19.75-mile (31.78 km) long state highway located in the western part of New York in the United States. NY 265 is a north–south route that roughly parallels the western parts of the Niagara River in Erie County and Niagara County. For much of its southern course, it is more frequently referred to by its longtime name, Military Road, which dates back to 1801 as a road to connect the city of Black Rock and Fort Niagara near Lake Ontario.
New York State Route 270 (NY 270) is a north–south state highway in western New York in the United States. It runs through rural and wooded areas of the town of Amherst in Erie County and the town of Pendleton in Niagara County. The southern terminus of the route is at an intersection with NY 263 south of the hamlet of Getzville. Its northern terminus is at a junction with NY 31 and NY 93 west of the city of Lockport. The entirety of NY 270 is known as Campbell Boulevard, named after New York State Senator William W. Campbell of the Niagara–Orleans district.
The International Railway Company (IRC) was a transportation company formed in a 1902 merger between several Buffalo-area interurban and street railways. The city railways that merged were the West Side Street Railway, the Crosstown Street Railway and the Buffalo Traction Company. The suburban railroads that merged included the Buffalo & Niagara Electric Street Railway, and its subsidiary the Buffalo, Lockport & Olcott Beach Railway; the Buffalo, Depew & Lancaster Railway; and the Niagara Falls Park & River Railway. Later the IRC acquired the Niagara Gorge Railroad (NGRR) as a subsidiary, which was sold in 1924 to the Niagara Falls Power Company. The NGRR also leased the Lewiston & Youngstown Frontier Railroad.
The Erie Plain is a lacustrine plain that borders Lake Erie in North America. From Buffalo, New York, to Cleveland, Ohio, it is quite narrow, but broadens considerably from Cleveland around Lake Erie to Southern Ontario, where it forms most of the Ontario peninsula. The Erie Plain was used in the United States as a natural gateway to the North American interior, and in both the United States and Canada the plain is heavily populated and provides very fertile agricultural land.