Strange is a hamlet on the western outskirt of King City

King City, Ontario

King City is an affluent, unincorporated village in King Township, Ontario, Canada, located just north of Toronto. It is the largest community in King Township, with 1,629 dwellings and a population of 4,902.-History:...

 located in King Township

King, Ontario

King is a township in York Region north of Toronto, within the Greater Toronto Area in Ontario, Canada.The rolling hills of the Oak Ridges Moraine are the most prominent visible geographical feature of King. The Holland Marsh, considered to be Ontario's "vegetable basket", straddles King Township...

, Ontario

Ontario

Ontario is a province of Canada, located in east-central Canada. It is Canada's most populous province and second largest in total area. It is home to the nation's most populous city, Toronto, and the nation's capital, Ottawa....

, Canada

Canada

Canada is a North American country consisting of ten provinces and three territories. Located in the northern part of the continent, it extends from the Atlantic Ocean in the east to the Pacific Ocean in the west, and northward into the Arctic Ocean...

. It is directly north of Laskay, and is a sparsely populated agricultural area.

Strange was founded as Williamstown in 1841 with the opening of a general store. In 1854, the community's first post office closed, but another opened on 1 March 1880 through the efforts of Frederick William Strange

Frederick William Strange

Frederick William Strange was an English-born physician, surgeon and political figure in Ontario, Canada. He represented York North in the Canadian House of Commons from 1878 to 1882 as a Liberal-Conservative member....

, from whom the post office and the community took their name. Today, only a few buildings remain, but only the Presbyterian Church and two graveyards provide links to its past.

Ecology

The Strange Till Plain is a flat ground moraine

Moraine

A moraine is any glacially formed accumulation of unconsolidated glacial debris which can occur in currently glaciated and formerly glaciated regions, such as those areas acted upon by a past glacial maximum. This debris may have been plucked off a valley floor as a glacier advanced or it may have...

 with underlying glacial

Glacier

A glacier is a large persistent body of ice that forms where the accumulation of snow exceeds its ablation over many years, often centuries. At least 0.1 km² in area and 50 m thick, but often much larger, a glacier slowly deforms and flows due to stresses induced by its weight...

 till. It was formed by the Ontario ice lobe during the Port Huron Stadial. It is believed that this till

Till

thumb|right|Closeup of glacial till. Note that the larger grains in the till are completely surrounded by the matrix of finer material , and this characteristic, known as matrix support, is diagnostic of till....

 plain exhibits the original surface; very little erosion

Erosion

Erosion is when materials are removed from the surface and changed into something else. It only works by hydraulic actions and transport of solids in the natural environment, and leads to the deposition of these materials elsewhere...

 or surface deposition

Sediment

Sediment is naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of fluids such as wind, water, or ice, and/or by the force of gravity acting on the particle itself....

 is observable throughout its 3 square kilometre range.

This Till plain is located between and within the Albion and Uxbridge wedges of the Oak Ridges Moraine

Oak Ridges Moraine

The Oak Ridges Moraine is an ecologically important geological landform in the Mixedwood Plains of south-central Ontario, Canada. The moraine covers a geographic area of between Caledon and Rice Lake, near Peterborough...

, and is a constituent part of that moraine.