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Origin of the Oak Ridges Moraine information


The Oak Ridges Moraine is a geological landform that runs east-west across south central Ontario, Canada. It developed about 12,000 years ago, during the Wisconsin glaciation in North America. A complex ridge of sedimentary material, the moraine is known to have partially developed under water. The Niagara Escarpment played a key role in forming the moraine in that it acted as a dam for glacial meltwater trapped between it and two ice lobes.

In order to understand the process by which the moraine formed, it is necessary to understand the physical geography in which it currently exists (that is, its physiography), and the layers of sediments found within it (the stratigraphy of the moraine).

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Origin of the Oak Ridges Moraine

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The Oak Ridges Moraine is a geological landform that runs east-west across south central Ontario, Canada. It developed about 12,000 years ago, during the...

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Oak Ridges Moraine

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The Oak Ridges Moraine is an ecologically important geological landform in the Mixedwood Plains of south-central Ontario, Canada. The moraine covers a...

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Terminal moraine

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A terminal moraine, also called an end moraine, is a type of moraine that forms at the terminal (edge) of a glacier, marking its maximum advance. At this...

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Canadian Shield

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of exposed Precambrian igneous and high-grade metamorphic rocks. It forms the North American Craton (or Laurentia), the ancient geologic core of the North...

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Moraine

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southeastern New York Oak Ridges Moraine – Glacial till landform above Lake Ontario, Canada Valparaiso Moraine – Moraine in the midwestern United States...

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Proglacial lake

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geology, a proglacial lake is a lake formed either by the damming action of a moraine during the retreat of a melting glacier, a glacial ice dam, or by meltwater...

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Younger Dryas

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re-advanced during the Younger Dryas, depositing a moraine from west Lake Superior to southeast Quebec. Along the southern margins of the Great Lakes, spruce...

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Esker

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surfaces". The Irish word was and is used particularly to describe long sinuous ridges, which are now known to be deposits of fluvio-glacial material. The best-known...

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Lake Chicago

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formed moraines, the Park Moraine in present-day Illinois and the Lake Borders Moraine in Indiana and Michigan. The ice continued northward forming the next...

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Last Glacial Period

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terminal moraines that form Long Island, Block Island, Cape Cod, Nomans Land, Martha's Vineyard, Nantucket, Sable Island, and the Oak Ridges Moraine in south-central...

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Pleistocene

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Philipp (8 June 2017). "New fossils from Jebel Irhoud, Morocco and the pan-African origin of Homo sapiens" (PDF). Nature. 546 (7657): 289–292. Bibcode:2017Natur...

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Ice age

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Esmark discovered the similarity between moraines near Haukalivatnet lake near sea level in Rogaland and moraines at branches of Jostedalsbreen. Esmark's...

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Last Glacial Maximum

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north–south moraine system along the eastern coast of Chiloé Island (41.5–43° S). By that time the glaciation at the latitude of Chiloé was of ice sheet...

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Interglacial

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pollen zone E4 in the type area (city of Amersfoort, Netherlands). Here this zone is characterized by the expansion of Quercus (oak), Corylus (hazel)...

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Last Interglacial

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well above the Arctic Circle at 71°10′21″N 25°47′40″E / 71.17250°N 25.79444°E / 71.17250; 25.79444. Hardwood trees such as hazel and oak grew as far...

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Kame

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Provincial Park. Drumlin Esker Glacial Kame culture Glacial landforms Moraine Outwash fan "Knob And Kettle | Encyclopedia.com". "kame". Oxford English...

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Glacial erratic

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in rows, trains or clusters along the lateral moraines as opposed to being located on the terminal moraine or in the general glacial field. Erratics provide...

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Laurentide Ice Sheet

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created much of the surface geology of southern Canada and the northern United States, leaving behind glacially scoured valleys, moraines, eskers and glacial...

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Wisconsin glaciation

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principally to the west through the passes of the coast range. Whenever the ice sheet melted from the north at a moraine, water would begin to pond in the divide...

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Till plain

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Ground moraines are formed with melts out of the glacier in irregular heaps, forming rolling hills. Till plains are common in areas such as the Midwestern...

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Glacial history of Minnesota

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terminal moraine region, the kettles are fairly small but deep, to fit between the moraine's steep and hilly ridges. If the ice had advanced outward and...

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Lake Agassiz

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the highest shoreline of Lake Agassiz. The Big Stone Moraine formed the southern boundary of the lake. During the Lockhart Phase the lake is estimated to...

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Lake Algonquin

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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...

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Older Dryas

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core samples whereas the changing abundance pattern of fauna and flora are most commonly used when examining lake sediments. Moraine belts are usually studied...

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Driftless Area

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farming, except on ridge tops and in river valleys. The sides of the ridges are often too steep for farming, and are usually forested. The Coulee Experimental...

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Monte Rosa

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range lying between the Dent d'Herens and the Pizzo Bianco near Macugnaga. The minor ridges on the north side of the border are parallel to this latter range...

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