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Many different kinds of burgers and combos, the burgers and fries were excellent! There is seating inside and outside. Ok, not a restaurant like Sauble Beach sorely needs - see my reviews of Sauble eateries - but this joint is among the finest snackeries during a hot summer evening when the family has abandoned you for shopping.

A totally McDonalds set-up - walk up counter, overhead menu, wait for your order to be cooked then scoot out to an available table - but the burgers are way better. Juicy, cooked perfectly medium, with many different combos.

Served with fries whether you want them or not. You will. Had lunch twice there. It was awesome. Had pineapple on the burger. Poutine was good. Beach Burger was awesome! Me and my family took a trip to Sauble Beach for the day and got hungry, so we looked up on here and found This wonderful place. Burgers are delicious!!!!!

Marine Dr 10, Oakville, Ontario, L6L1B7 — Point2 Canada

Very convenient, we were able to eat on the beach! I highly recommend the Son of a Beach Burger! Great place. Own or manage this property?

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These water level fluctuations are an integral part of lake ecology , and produce and maintain extensive wetlands. Baymouth bars built by prevailing winds and currents have created a significant number of lagoons and sheltered harbors, mostly near but not limited to Prince Edward County, Ontario and the easternmost shores.

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Perhaps the best-known example is Toronto Bay , chosen as the site of the Upper Canada Ontario capital for its strategic harbour. These sand bars are often associated with large wetlands , which support large numbers of plant and animal species, as well as providing important rest areas for migratory birds.

One unique feature of the lake is the Z-shaped Bay of Quinte which separates Prince Edward County from the Ontario mainland, save for a 2-mile 3. The lake basin was carved out of soft, weak Silurian -age rocks by the Wisconsin ice sheet during the last ice age.

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 drumlins , kames , and moraines , both 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 the lake surface was at a higher level. This stage is known as Lake Iroquois.

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When the ice finally receded from the St. Lawrence valley, the outlet was below sea level , and for a short time the lake became a bay of the Atlantic Ocean, in association with the Champlain Sea. Lawrence area. Since the ice receded from the area last, the most rapid rebound still occurs there. This means 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.

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As was their practice, the French explorers introduced other names for the lake. In and , the 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 Bay , indicating the possibility of trading by the indigenous peoples with Norse explorers on the east coast of North America.

After the French and Indian War , all 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, Ontario , formerly the capital of Canada , dating 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. The Great Lakes watershed is a region of high biodiversity, and Lake Ontario is important for its diversity of birds, fish, reptiles, amphibians, and plants. 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. Most of the forests around the lake are deciduous forests dominated by trees including maple, oak, beech, ash and basswood. 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.

The open water is less-affected by shoreline features, such as wetlands, and more affected by nutrient levels that control the production of algae. 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. 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. 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 DDT , benzo[ a ]pyrene and other pesticides; PCBs , aramite , chromium , lead , mirex , mercury , and 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. By the s and s, the increased pollution caused frequent algal blooms to occur in the summer.