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Keating Channel

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The Keating Channel is a 1,000-metre (3,300 ft) long waterway in Toronto , Ontario , Canada. It connects the Don River to inner Toronto Harbour (Toronto Bay) on Lake Ontario . The channel is named after Edward Henry Keating (1844-1912), a city engineer (1892-1898) who proposed the creation of the channel in 1893. The channel was built to connect Ashbridge's Bay to the harbour; later, the Don was diverted into the channel, and its river mouth infilled in the early 1910s.

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72-536: Prior to the 19th century, the Don River naturally entered Toronto Harbour in two mouths, one roughly near where Keating Channel now flows out and one further south. In the late 19th century, a public works program was started to straighten the lower part of the Don River south of the Winchester Street Bridge . The project was called the "Don Improvement Project". The goal of the project was to alleviate floods on

144-409: A body of water from 2 hectares (5 acres) to 8 hectares (20 acres). Pioneering animal ecologist Charles Elton regarded lakes as waterbodies of 40 hectares (99 acres) or more. The term lake is also used to describe a feature such as Lake Eyre , which is a dry basin most of the time but may become filled under seasonal conditions of heavy rainfall. In common usage, many lakes bear names ending with

216-680: A circulation of 87,929 and readership of 890,000. The magazine is a major winner of the Canadian National Magazine Awards , leading current publications with 110 gold awards including 3 awards for Magazine of the Year in 1985, 1989, and 2007. Toronto Life also won the Magazine Grand Prix award at the 2021 National Magazine Awards, with the jury writing that it is "alert to the cultural moment, bold in its journalistic exposés, up-to-the-minute in its services reportage and smart about

288-496: A comprehensive analysis of the origin of lakes and proposed what is a widely accepted classification of lakes according to their origin. This classification recognizes 11 major lake types that are divided into 76 subtypes. The 11 major lake types are: Tectonic lakes are lakes formed by the deformation and resulting lateral and vertical movements of the Earth's crust. These movements include faulting, tilting, folding, and warping. Some of

360-402: A form of organic lake. They form where a buildup of partly decomposed plant material in a wet environment leaves the vegetated surface below the water table for a sustained period of time. They are often low in nutrients and mildly acidic, with bottom waters low in dissolved oxygen. Artificial lakes or anthropogenic lakes are large waterbodies created by human activity . They can be formed by

432-538: A higher perimeter to area ratio than other lake types. These form where sediment from a tributary blocks the main river. These form where sediment from the main river blocks a tributary, usually in the form of a levee . Lakes formed by other processes responsible for floodplain basin creation. During high floods they are flushed with river water. There are four types: 1. Confluent floodplain lake, 2. Contrafluent-confluent floodplain lake, 3. Contrafluent floodplain lake, 4. Profundal floodplain lake. A solution lake

504-510: A hypolimnion; accordingly, very shallow lakes are excluded from this classification system. Based upon their thermal stratification, lakes are classified as either holomictic , with a uniform temperature and density from top to bottom at a given time of year, or meromictic , with layers of water of different temperature and density that do not intermix. The deepest layer of water in a meromictic lake does not contain any dissolved oxygen so there are no living aerobic organisms . Consequently,

576-428: A lake consists of a large area of standing water that occupies an extensive closed depression in limestone, it is also called a karst lake . Smaller solution lakes that consist of a body of standing water in a closed depression within a karst region are known as karst ponds. Limestone caves often contain pools of standing water, which are known as underground lakes . Classic examples of solution lakes are abundant in

648-470: A large number of studies agree that small ponds are much more abundant than large lakes. For example, one widely cited study estimated that Earth has 304 million lakes and ponds, and that 91% of these are 1 hectare (2.5 acres) or less in area. Despite the overwhelming abundance of ponds, almost all of Earth's lake water is found in fewer than 100 large lakes; this is because lake volume scales superlinearly with lake area. Extraterrestrial lakes exist on

720-489: A natural outflow and lose water solely by evaporation or underground seepage, or both. These are termed endorheic lakes. Many lakes are artificial and are constructed for hydroelectric power generation, aesthetic purposes, recreational purposes, industrial use, agricultural use, or domestic water supply . The number of lakes on Earth is undetermined because most lakes and ponds are very small and do not appear on maps or satellite imagery . Despite this uncertainty,

792-555: A new channel just north of Lake Shore Boulevard or straight south to link up or cut the inner basin shipping channel to the south of the Keating Channel. The environmental assessment process is ongoing. Proponents of restoring the mouth of the Don to a more natural state have argued that this restoration would ameliorate the damage expected from a rare flood with water-flow equal to or greater than that from 1954's Hurricane Hazel . In 2018,

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864-403: A result of meandering. The slow-moving river forms a sinuous shape as the outer side of bends are eroded away more rapidly than the inner side. Eventually a horseshoe bend is formed and the river cuts through the narrow neck. This new passage then forms the main passage for the river and the ends of the bend become silted up, thus forming a bow-shaped lake. Their crescent shape gives oxbow lakes

936-522: A result of the 1959 Hebgen Lake earthquake . Most landslide lakes disappear in the first few months after formation, but a landslide dam can burst suddenly at a later stage and threaten the population downstream when the lake water drains out. In 1911, an earthquake triggered a landslide that blocked a deep valley in the Pamir Mountains region of Tajikistan , forming the Sarez Lake . The Usoi Dam at

1008-490: A small shipyard, the Toronto Shipyard Company , which built vessels for the war effort. The channel has always been dredged, to continue to allow navigation. In the 21st century, with its role as a cargo route over, the channel is only dredged to a depth of 5.8 metres (19 ft). Toronto Life quoted Toronto harbour master Angus Armstrong 's explanation that the current dredging efforts are aimed at "whatever

1080-422: A variation in density because of thermal gradients. Stratification can also result from a density variation caused by gradients in salinity. In this case, the hypolimnion and epilimnion are separated not by a thermocline but by a halocline , which is sometimes referred to as a chemocline . Lakes are informally classified and named according to the seasonal variation in their lake level and volume. Some of

1152-443: Is sag ponds . Volcanic lakes are lakes that occupy either local depressions, e.g. craters and maars , or larger basins, e.g. calderas , created by volcanism . Crater lakes are formed in volcanic craters and calderas, which fill up with precipitation more rapidly than they empty via either evaporation, groundwater discharge, or a combination of both. Sometimes the latter are called caldera lakes, although often no distinction

1224-403: Is a lake occupying a basin formed by surface dissolution of bedrock. In areas underlain by soluble bedrock, its solution by precipitation and percolating water commonly produce cavities. These cavities frequently collapse to form sinkholes that form part of the local karst topography . Where groundwater lies near the grounds surface, a sinkhole will be filled water as a solution lake. If such

1296-546: Is barged out to the Leslie Street Spit where it is dumped in a containment area built for this purpose. In 2005, the annual amount of silt dredged was about 35,000 cubic metres. The containment area has the capacity to take 50 years of Don River dredgeate [1] . In 1980 Ontario's Minister of the Environment was asked, during question period , about an exemption from environmental regulations, granted to those who dredged

1368-462: Is dammed behind an ice shelf that is attached to the coastline. They are mostly found in Antarctica. Fluvial (or riverine) lakes are lakes produced by running water. These lakes include plunge pool lakes , fluviatile dams and meander lakes. The most common type of fluvial lake is a crescent-shaped lake called an oxbow lake due to the distinctive curved shape. They can form in river valleys as

1440-461: Is in contrast to the Humber River to the west, which has a natural mouth and is home to about 44 species. Another problem affecting the channel is floating debris that is washed down the Don. Composed largely of logs and dead wood, there is also an assortment of garbage that collects in the channel. The TRCA corrals this material with a boom across the channel. There can be significant flotsam where

1512-734: Is localized in a basin or interconnected basins surrounded by dry land . Lakes lie completely on land and are separate from the ocean , although they may be connected with the ocean by rivers . Lakes, as with other bodies of water , are part of the water cycle , the processes by which water moves around the Earth. Most lakes are freshwater and account for almost all the world's surface freshwater, but some are salt lakes with salinities even higher than that of seawater . Lakes vary significantly in surface area and volume of water. Lakes are typically larger and deeper than ponds , which are also water-filled basins on land, although there are no official definitions or scientific criteria distinguishing

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1584-448: Is made. An example is Crater Lake in Oregon , in the caldera of Mount Mazama . The caldera was created in a massive volcanic eruption that led to the subsidence of Mount Mazama around 4860 BCE. Other volcanic lakes are created when either rivers or streams are dammed by lava flows or volcanic lahars . The basin which is now Malheur Lake , Oregon was created when a lava flow dammed

1656-502: Is needed for the health of the river." The channel's impact on the Don River is varied. Both sides of the channel are lined with concrete dock wall which creates a barrier and provides little habitat for fish and other water dwelling creatures. The Don is home to about 21 species of fish. Only about four or five species can be found near the mouth. This is partly due to poor water quality but also due to lack of habitat. The dock wall continues, mostly unbroken, north to Riverdale Park . This

1728-429: Is unknown but is estimated to be at least 2 million. Finland has 168,000 lakes of 500 square metres (5,400 sq ft) in area, or larger, of which 57,000 are large (10,000 square metres (110,000 sq ft) or larger). Most lakes have at least one natural outflow in the form of a river or stream , which maintain a lake's average level by allowing the drainage of excess water. Some lakes do not have

1800-574: The Coatsworth Cut at the foot Coxwell Avenue. However, the portion east of the Don River was never completed and it was closed in 1916. The channel was completed in 1922 after eight years of construction. The completed channel now runs from the harbour east to the mouth of the river, a distance of about 800 metres. The original mouth of the Don is buried under infill near where the Gardiner Expressway meets Cherry Street. The original course from

1872-752: The Malheur River . Among all lake types, volcanic crater lakes most closely approximate a circular shape. Glacial lakes are lakes created by the direct action of glaciers and continental ice sheets. A wide variety of glacial processes create enclosed basins. As a result, there are a wide variety of different types of glacial lakes and it is often difficult to define clear-cut distinctions between different types of glacial lakes and lakes influenced by other activities. The general types of glacial lakes that have been recognized are lakes in direct contact with ice, glacially carved rock basins and depressions, morainic and outwash lakes, and glacial drift basins. Glacial lakes are

1944-540: The Proto-Indo-European root * leǵ- ('to leak, drain'). Cognates include Dutch laak ('lake, pond, ditch'), Middle Low German lāke ('water pooled in a riverbed, puddle') as in: de:Wolfslake , de:Butterlake , German Lache ('pool, puddle'), and Icelandic lækur ('slow flowing stream'). Also related are the English words leak and leach . There is considerable uncertainty about defining

2016-399: The density of water varies with temperature, with a maximum at +4 degrees Celsius, thermal stratification is an important physical characteristic of a lake that controls the fauna and flora , sedimentation, chemistry, and other aspects of individual lakes. First, the colder, denser water typically forms a layer near the bottom, which is called the hypolimnion . Second, normally overlying

2088-583: The Earth by extraterrestrial objects (either meteorites or asteroids ). Examples of meteorite lakes are Lonar Lake in India, Lake El'gygytgyn in northeast Siberia, and the Pingualuit crater lake in Quebec, Canada. As in the cases of El'gygytgyn and Pingualuit, meteorite lakes can contain unique and scientifically valuable sedimentary deposits associated with long records of paleoclimatic changes. In addition to

2160-527: The Keating Channel enters Toronto Harbour, especially after a big storm. On the north side of the channel a slight bend in Lake Shore Boulevard has created a narrow open space. In 1998, the Task Force to Bring Back the Don planted Staghorn Sumac ( Rhus typhina ), Sandbar Willow ( Salix exigua ), and Red Osier Dogwood ( Cornus stolonifera ) in this area. Despite poor soil conditions, the willow and

2232-551: The Lusatian Lake District, Germany. In India, Sudarshana Lake is a historical artificial lake located in the semi-arid region of Girnar, Gujarat, originally constructed during the reign of Chandragupta Maurya. See: List of notable artificial lakes in the United States Meteorite lakes, also known as crater lakes (not to be confused with volcanic crater lakes ), are created by catastrophic impacts with

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2304-535: The Reichmann family which ... there was no reasonable basis for" and said it now realized that "none of the allegations and insinuations should ever have been raised." Stephen Trumper, the president of Toronto Life Publishing Co., said “we should have been much more rigorous in that process and more precise in our conclusions,” and that “any and all negative insinuations and allegations in the article... are totally false.” In April 2015, Canadian entrepreneur Michael Elder,

2376-456: The article defamed their family. In 1991, after exhausting the cover of Toronto Life 's libel insurance policy, an out-of-court settlement was reached between the parties that saw the article retracted and Toronto Life make “a substantial donation to four charities” designated by the Reichmanns. In its apology, Toronto Life said its article "incorporated many allegations and insinuations about

2448-856: The base of the valley has remained in place for more than 100 years but the terrain below the lake is in danger of a catastrophic flood if the dam were to fail during a future earthquake. Tal-y-llyn Lake in north Wales is a landslide lake dating back to the last glaciation in Wales some 20000 years ago. Aeolian lakes are produced by wind action . These lakes are found mainly in arid environments, although some aeolian lakes are relict landforms indicative of arid paleoclimates . Aeolian lakes consist of lake basins dammed by wind-blown sand; interdunal lakes that lie between well-oriented sand dunes ; and deflation basins formed by wind action under previously arid paleoenvironments. Moses Lake in Washington , United States,

2520-555: The channel. Member of Provincial Parliament (MPP) Bryden was quoting Donald Chant 's recommendation concerning the Keating Channel, and why the recommendation had been ignored, when she was interrupted by the Minister. Chant was then the chairman of the Premier 's steering committee on environmental assessment. According to the MPP, Chant's recommendations had questioned whether dredging the channel

2592-915: The courses of mature rivers, where a river channel has widened over a basin formed by eroded floodplains and wetlands . Some lakes are found in caverns underground . Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice age . All lakes are temporary over long periods of time , as they will slowly fill in with sediments or spill out of the basin containing them. Artificially controlled lakes are known as reservoirs , and are usually constructed for industrial or agricultural use, for hydroelectric power generation, for supplying domestic drinking water , for ecological or recreational purposes, or for other human activities. The word lake comes from Middle English lake ('lake, pond, waterway'), from Old English lacu ('pond, pool, stream'), from Proto-Germanic * lakō ('pond, ditch, slow moving stream'), from

2664-513: The creation of lakes by the disruption of preexisting drainage networks, it also creates within arid regions endorheic basins that contain salt lakes (also called saline lakes). They form where there is no natural outlet, a high evaporation rate and the drainage surface of the water table has a higher-than-normal salt content. Examples of these salt lakes include Great Salt Lake and the Dead Sea . Another type of tectonic lake caused by faulting

2736-622: The difference between lakes and ponds , and neither term has an internationally accepted definition across scientific disciplines or political boundaries. For example, limnologists have defined lakes as water bodies that are simply a larger version of a pond, which can have wave action on the shoreline or where wind-induced turbulence plays a major role in mixing the water column. None of these definitions completely excludes ponds and all are difficult to measure. For this reason, simple size-based definitions are increasingly used to separate ponds and lakes. Definitions for lake range in minimum sizes for

2808-509: The east end is the start of the Don Valley Parkway . In the 1940s the watershed further up the Don River became more urbanized. This caused an increasing amount of silt to flow down the river. The silt collects in the channel where there is very little water flow. Since that time, the Toronto and Region Conservation Authority (TRCA) has been dredging the channel. The dredgeate material

2880-523: The exception of criterion 3, the others have been accepted or elaborated upon by other hydrology publications. The majority of lakes on Earth are freshwater , and most lie in the Northern Hemisphere at higher latitudes . Canada , with a deranged drainage system , has an estimated 31,752 lakes larger than 3 square kilometres (1.2 sq mi) in surface area. The total number of lakes in Canada

2952-410: The hardy sumac have thrived. It is now a long narrow grove of small trees and shrubs. Another small green space at the eastern end was also planned for restoration but the project was abandoned after one planting. There was also a proposal to remove part of the dock wall to improve fish habitat. These projects were suspended when it became apparent that a larger project would be starting soon. In 1999,

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3024-422: The hypolimnion is a transition zone known as the metalimnion . Finally, overlying the metalimnion is a surface layer of warmer water with a lower density, called the epilimnion . This typical stratification sequence can vary widely, depending on the specific lake or the time of year, or a combination of both. The classification of lakes by thermal stratification presupposes lakes with sufficient depth to form

3096-907: The intentional damming of rivers and streams, rerouting of water to inundate a previously dry basin , or the deliberate filling of abandoned excavation pits by either precipitation runoff , ground water , or a combination of both. Artificial lakes may be used as storage reservoirs that provide drinking water for nearby settlements , to generate hydroelectricity , for flood management , for supplying agriculture or aquaculture , or to provide an aquatic sanctuary for parks and nature reserves . The Upper Silesian region of southern Poland contains an anthropogenic lake district consisting of more than 4,000 water bodies created by human activity. The diverse origins of these lakes include: reservoirs retained by dams, flooded mines, water bodies formed in subsidence basins and hollows, levee ponds, and residual water bodies following river regulation. Same for

3168-466: The karst regions at the Dalmatian coast of Croatia and within large parts of Florida . A landslide lake is created by the blockage of a river valley by either mudflows , rockslides , or screes . Such lakes are most common in mountainous regions. Although landslide lakes may be large and quite deep, they are typically short-lived. An example of a landslide lake is Quake Lake , which formed as

3240-444: The lake level. Toronto Life Toronto Life is a monthly magazine about entertainment , politics and life in Toronto , Ontario , Canada. Toronto Life also publishes a number of annual special interest guides about the city, including Real Estate , Stylebook , Eating & Drinking , City Home and Neighbourhoods . Established in 1966, it has been owned by St. Joseph Communications since 2002. Toronto Life has

3312-648: The largest lakes on Earth are rift lakes occupying rift valleys, e.g. Central African Rift lakes and Lake Baikal . Other well-known tectonic lakes, Caspian Sea , the Sea of Aral , and other lakes from the Pontocaspian occupy basins that have been separated from the sea by the tectonic uplift of the sea floor above the ocean level. Often, the tectonic action of crustal extension has created an alternating series of parallel grabens and horsts that form elongate basins alternating with mountain ranges. Not only does this promote

3384-528: The layers of sediment at the bottom of a meromictic lake remain relatively undisturbed, which allows for the development of lacustrine deposits . In a holomictic lake, the uniformity of temperature and density allows the lake waters to completely mix. Based upon thermal stratification and frequency of turnover, holomictic lakes are divided into amictic lakes , cold monomictic lakes , dimictic lakes , warm monomictic lakes, polymictic lakes , and oligomictic lakes. Lake stratification does not always result from

3456-560: The level of a lake are controlled by the difference between the input and output compared to the total volume of the lake. Significant input sources are precipitation onto the lake, runoff carried by streams and channels from the lake's catchment area, groundwater channels and aquifers, and artificial sources from outside the catchment area. Output sources are evaporation from the lake, surface and groundwater flows, and any extraction of lake water by humans. As climate conditions and human water requirements vary, these will create fluctuations in

3528-459: The lower Don that were periodically washing out bridges. It was also done to create additional wharf space for the Toronto harbour. When it was completed, the river was directed south into Ashbridge's Bay. At the time Ashbridge's Bay was still a lacustrine marsh . It was heavily polluted by local industry. The water from the river was diverted into the bay with the hope that it would flush the bay of

3600-481: The mainland; lakes cut off from larger lakes by a bar; or lakes divided by the meeting of two spits. Organic lakes are lakes created by the actions of plants and animals. On the whole they are relatively rare in occurrence and quite small in size. In addition, they typically have ephemeral features relative to the other types of lakes. The basins in which organic lakes occur are associated with beaver dams, coral lakes, or dams formed by vegetation. Peat lakes are

3672-424: The mode of origin, lakes have been named and classified according to various other important factors such as thermal stratification , oxygen saturation, seasonal variations in lake volume and water level, salinity of the water mass, relative seasonal permanence, degree of outflow, and so on. The names used by the lay public and in the scientific community for different types of lakes are often informally derived from

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3744-485: The moon Titan , which orbits the planet Saturn . The shape of lakes on Titan is very similar to those on Earth. Lakes were formerly present on the surface of Mars, but are now dry lake beds . In 1957, G. Evelyn Hutchinson published a monograph titled A Treatise on Limnology , which is regarded as a landmark discussion and classification of all major lake types, their origin, morphometric characteristics, and distribution. Hutchinson presented in his publication

3816-415: The morphology of the lakes' physical characteristics or other factors. Also, different cultures and regions of the world have their own popular nomenclature. One important method of lake classification is on the basis of thermal stratification, which has a major influence on the animal and plant life inhabiting a lake, and the fate and distribution of dissolved and suspended material in the lake. For example,

3888-406: The most numerous lakes in the world. Most lakes in northern Europe and North America have been either influenced or created by the latest, but not last, glaciation, to have covered the region. Glacial lakes include proglacial lakes , subglacial lakes , finger lakes , and epishelf lakes. Epishelf lakes are highly stratified lakes in which a layer of freshwater, derived from ice and snow melt,

3960-616: The mouth upstream now lies underneath railway tracks used by GO Transit for storage. The channel is flanked on the north by the elevated Gardiner Expressway and Lake Shore Boulevard East . The south side is occupied by the PortsToronto (also called the Toronto Port Authority ) works yard and the Keating Channel Pub. At the west end Cherry Street crosses the channel over a single-sided drawbridge rarely used by ships. At

4032-791: The names include: Lakes may be informally classified and named according to the general chemistry of their water mass. Using this classification method, the lake types include: A paleolake (also palaeolake ) is a lake that existed in the past when hydrological conditions were different. Quaternary paleolakes can often be identified on the basis of relict lacustrine landforms, such as relict lake plains and coastal landforms that form recognizable relict shorelines called paleoshorelines . Paleolakes can also be recognized by characteristic sedimentary deposits that accumulated in them and any fossils that might be contained in these sediments. The paleoshorelines and sedimentary deposits of paleolakes provide evidence for prehistoric hydrological changes during

4104-562: The organic-rich deposits of pre-Quaternary paleolakes are important either for the thick deposits of oil shale and shale gas contained in them, or as source rocks of petroleum and natural gas . Although of significantly less economic importance, strata deposited along the shore of paleolakes sometimes contain coal seams . Lakes have numerous features in addition to lake type, such as drainage basin (also known as catchment area), inflow and outflow, nutrient content, dissolved oxygen , pollutants , pH , and sedimentation . Changes in

4176-504: The platforms it uses to deliver content to readers. The issues its editorial team assembled during the pandemic showed just how relevant and useful a first-class city magazine can be." It is also known for publishing an annual 50 most influential people in Toronto list. Established in November 1966, Toronto Life was purchased by Michael de Pencier in 1972 and held until 2002, when it was sold to St. Joseph Media. The publisher also owns

4248-430: The poor water. However the flow of water introduced raw sewage in the river into the bay. The bay water remained stagnant and was increasingly becoming a serious health risk. The Keating Channel was proposed as a method of directing the dirty river water into the harbour thus dispersing it more rapidly. The channel was planned to go from the northeast corner of the inner harbour east towards Leslie Street and join up with

4320-416: The position from 1972 to 1974 and was succeeded by Alexander Ross. Thomas Hedley was editor-in-chief from 1977 to 1978 and Don Obe was editor-in-chief from 1978 to 1981. Peter Herrndorf was the publisher of Toronto Life from 1983 to 1992. In 2015, an article titled "Jennifer Pan’s Revenge: The inside story of a golden child, the killers she hired, and the parents she wanted dead" by Karen K. Ho brought

4392-492: The previously relatively obscure Jennifer Pan murder case to international attention. In October 2018, it was announced that Toronto Life will launch a membership program with access to Toronto Life ’s events, as well as special offers from local venues. In November 1987, Toronto Life published a 50,000-word article on the Reichmanns family written by Elaine Dewar. In January 1988, Paul, Albert and Ralph Reichmann sued Dewar and Toronto Life for $ 102 million, claiming that

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4464-467: The son of Jim Elder , attempted to sue the magazine to prevent publication of a feature about him. Superior Court dismissed the motion for an injunction and awarded the magazine $ 17,000 in costs. In March 2014, Toronto Life was required to shut down its unpaid internship program implemented in 2009, after the Ontario Ministry of Labour declared that its longstanding practice of not paying interns

4536-404: The thermal stratification, as well as the degree and frequency of mixing, has a strong control over the distribution of oxygen within the lake. Professor F.-A. Forel , also referred to as the "Father of limnology", was the first scientist to classify lakes according to their thermal stratification. His system of classification was later modified and improved upon by Hutchinson and Löffler. As

4608-407: The three levels of government announced plans to revitalize Toronto's waterfront . Among the four initial projects was a plan to restore the mouth of the Don to a more natural outlet. In 2005, an environmental assessment was initiated to investigate options to restore the original mouth of the Don. Some of the options being considered would fill in the Keating Channel and direct the Don River through

4680-456: The times that they existed. There are two types of paleolake: Paleolakes are of scientific and economic importance. For example, Quaternary paleolakes in semidesert basins are important for two reasons: they played an extremely significant, if transient, role in shaping the floors and piedmonts of many basins; and their sediments contain enormous quantities of geologic and paleontologic information concerning past environments. In addition,

4752-481: The tourism magazine Where Canada (published in several large cities), Fashion , Wish , Wedding Bells , and several smaller magazines. The current editor-in-chief is Malcolm Johnston, who succeeded long-time editor Sarah Fulford (since 2008) in February 2022. Marq de Villiers was editor-in-chief from 1981 to 1992 and then publisher. John Edward Macfarlane was editor-in-chief from 1992 to 2007. He had previously had

4824-641: The two. Lakes are also distinct from lagoons , which are generally shallow tidal pools dammed by sandbars or other material at coastal regions of oceans or large lakes. Most lakes are fed by springs , and both fed and drained by creeks and rivers , but some lakes are endorheic without any outflow, while volcanic lakes are filled directly by precipitation runoffs and do not have any inflow streams. Natural lakes are generally found in mountainous areas (i.e. alpine lakes ), dormant volcanic craters , rift zones and areas with ongoing glaciation . Other lakes are found in depressed landforms or along

4896-469: The western end was narrowed as part of the construction of Ookwemin Minising (formerly Villiers Island). Ookwemin Minising is a new island, which has the Keating Channel as its northern shore. The Polson slip will be naturalized, and its channel extended to the Don River. Lake A lake is an often naturally occurring, relatively large and fixed body of water on or near the Earth's surface. It

4968-462: The word pond , and a lesser number of names ending with lake are, in quasi-technical fact, ponds. One textbook illustrates this point with the following: "In Newfoundland, for example, almost every lake is called a pond, whereas in Wisconsin, almost every pond is called a lake." One hydrology book proposes to define the term "lake" as a body of water with the following five characteristics: With

5040-473: Was in contravention of the Employment Standards Act . The magazine responded, saying "The idea that we can start paying everybody completely misunderstands the nature of the economics of the magazine industry at the moment." Toronto Life' s first (unpaid) intern, Derek Finkle, started with the magazine in 1993. During his internship he wrote a cover story for the magazine for free. He weighed in on

5112-611: Was originally a shallow natural lake and an example of a lake basin dammed by wind-blown sand. China's Badain Jaran Desert is a unique landscape of megadunes and elongated interdunal aeolian lakes, particularly concentrated in the southeastern margin of the desert. Shoreline lakes are generally lakes created by blockage of estuaries or by the uneven accretion of beach ridges by longshore and other currents. They include maritime coastal lakes, ordinarily in drowned estuaries; lakes enclosed by two tombolos or spits connecting an island to

5184-444: Was worthwhile: "That the issue of the need for dredging Keating Channel remains unresolved and that a hearing on this specific issue should be held as soon as possible and before any irrevocable approvals are given. Canada's Federal cabinet published a tender for a railway swing bridge over the channel in 1896. Construction began in 1900. Early in its history the banks of the channel were lined with industrial enterprises, including

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