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    Lake Ontario bathymetric map. The action of the ice occurred along the pre-glacial Ontarian River valley which had approximately the same orientation as today's basin.

    Material that was pushed southward by the ice sheet left landforms such as drumlinskamesand morainesboth on the modern land surface and the lake bottom, [15] reorganizing the region's entire drainage system. As the ice sheet retreated toward the north, it still dammed the St.

    Lawrence valley outlet, so that the lake surface was at a higher level. This stage is known as Lake Iroquois. When the ice finally receded from the St. Lawrence valley, the outlet was below sea leveland for a short time the lake became a bay of the Atlantic Ocean, in association with the Champlain Sea. Since the ice receded from the area last, the most rapid rebound still occurs there.

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    This means that the lake bed is gradually tilting southward, inundating the south shore and turning river valleys into bays. Both north and south shores experience shoreline erosion, but the tilting amplifies this effect on the south shore, causing loss to property owners. The lake was a border between the Huron people and the Iroquois Confederacy in the pre-Columbian era.

    In the s, the Iroquois drove out the Huron from southern Ontario and settled the northern shores of Lake Ontario. As was their practice, the French explorers introduced other names for the lake. In andthe lake was referred to as Lac de St.

    Louis or Lake St. He was a French soldier, courtier, and Governor General of New France from to and from to his death in Artifacts which are believed to be of Norse origin have been found in the area of Sodus Bayindicating the possibility of trading by the indigenous peoples with Norse explorers on the east coast of North America.

    After the French and Indian Warall forts around the lake were under British control. The United States did not take possession of forts on present-day American territory until the signing of the Jay Treaty in Permanent, non-military European settlement began during the American Revolution.

    As the easternmost and nearest lake to the Atlantic seaboard of Canada and the United States, population centres here are among the oldest in the Great Lakes basin, with Kingston, Ontarioformerly the capital of Canadadating to the s Fort Frontenac. The lake became a hub of commercial activity following the War of with canal building on both sides of the border and heavy travel by lake steamers.

    Steamer activity peaked in the midth century before competition from railway lines. In the late 19th and early 20th centuries, a type of scow known as a stone hooker was in operation on the north-west shore, particularly around Port Credit and Bronte.

    Stonehooking was the practice of raking flat fragments of Dundas shale from the shallow lake floor of the area for use in construction, particularly in the growing city of Toronto. Many of these special species are associated with shorelines, particularly sand dunes, lagoons, and wetlands. The importance of wetlands to the lake has been appreciated, and many of the larger wetlands have protected status.

    However, these wetlands are changing in part because the natural water level fluctuations have been reduced. Many wetland plants are dependent upon low water levels to reproduce. This is particularly true of meadow marsh also known as wet meadow wetlands ; for example, in Eel Bay near Alexandria Bay, regulation of lake levels has resulted in large losses of wet meadow.

    Eutrophication may accelerate this process by providing nitrogen and phosphorus for the more rapid growth of competitively dominant plants. In some areas more than 90 percent of the forest cover has been removed and replaced by agriculture. Certain tree species, such as hemlock, have also been particularly depleted by past logging activity. Algae are the basis of the open water food web, and the source of primary production that ends up as Lake Trout and Walleye at the top of the open water food web.

    Lake Sturgeon were abundant in and had been driven to near extinction by Like the other Great Lakes, Lake Ontario used to have an important commercial fishery. It has been largely destroyed, mostly by over-fishing. Consider the Lake Sturgeon as but one example. The females mature slowly and require decades to reach sexual maturity. It was once an abundant species in Lake Ontario.

    Once its value was realized, "They were taken by every available means from spearing and jigging to set lines of baited or unbaited hooks laid on the bottom to trapnets, poundnets and gillnets.

    The fishery collapsed, largely by They have never recovered. Like most sturgeons, the lake sturgeon is rare now, and is protected in many areas. Populations in the Oswego River are being actively managed for recovery. Lake Ontario food web This food web has been damaged not only by over-fishing, and changes in nutrient levels, but also by other types of pollution from industrial chemicals, agricultural fertilizers, untreated sewage, phosphates from laundry detergents, and pesticides.

    Some pollutant chemicals that have been found in the lake include DDTbenzo[a]pyrene and other pesticides; PCBsaramitechromiumleadmirexmercuryand carbon tetrachloride. The International Joint Commission has identified areas where pollution is particularly intense point sources and mapped them as Areas of Concern.

    A Remedial Action Plan has been developed for each area. Fish eating birds such as osprey, bald eagle and cormorant were being poisoned by contaminated fish. Since the s and s, environmental concerns have forced a cleanup of industrial and municipal wastes.

    Cleanup has been accomplished through better treatment plants, tighter environmental regulations, deindustrialization and increased public awareness. Today, Lake Ontario has recovered some of its pristine quality; for example, walleyea fish species considered as a marker of clean water, are now found.

    However, regional airshed pollution remains a concern. The lake has also become an important sport fisheryalthough with introduced species Coho and Chinook salmon rather than the native species. Bald eagle and osprey populations are also beginning to recover. Invasive species are a problem for Lake Ontario, particularly lamprey and zebra mussels. Lamprey are being controlled by poisoning in the juvenile stage in the streams where they breed. Zebra mussels in particular are difficult to control, and pose major challenges for the lake and its waterways.

    Climate[ edit ] The lake has a natural seiche rhythm of eleven minutes. Ice sheets typically form along the shoreline and in slack water bays, where the lake is not as deep. In the winter ofthe ice cover was stable enough that the American naval commander stationed at Sackets Harbor feared a British attack from Kingstonover the ice. When the cold winds of winter pass over the warmer water of the lake, they pick up moisture and drop it as lake effect snow.

    Since the prevailing winter winds are from the northwest, the southern and southeastern shoreline of the lake is referred to as the snowbelt.

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    The "Hill", as it is often referred to, typically receives more snow than any other region in the eastern United States. As a result, Tug Hill is a popular location for winter enthusiasts, such as snow-mobilers and cross-country skiers. Lake-effect snow often extends inland as far as Syracusewith that city often recording the most winter snowfall accumulation of any large city in the United States.

    Foggy conditions particularly in fall can be created by thermal contrasts and can be an impediment for recreational boaters.

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    In a normal winter, Lake Ontario will be at most one quarter ice-covered, in a mild winter almost completely unfrozen. Lake Ontario has completely frozen over on five recorded occasions: Cool onshore winds also retard early bloom of plants and flowers until later in the spring season, protecting them from possible frost damage.

    Such microclimatic effects have enabled tender fruit production in a continental climate, with the southwest shore supporting a major fruit-growing area. Applescherriespearsplumsand peaches are grown in many commercial orchards around Rochester.

    The wine-growing region extends over the international border into Niagara and Orleans counties. Apple varieties that tolerate a more extreme climate are grown on the lake's north shore, around Cobourg.

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