Land of lakes.Canada has more lakes than any other country in the world; so many that we don't know Don't know (DK, DKed) "Don't know the trade." A Street expression used whenever one party lacks knowledge of a trade or receives conflicting instructions from the other party. exactly how many. If any body had an accurate count it should be Environment Canada. But, that federal department's website says only that: "There are an estimated two million lakes in Canada covering approximately 7.6% of Canada's land area." This is a much higher proportion of freshwater coverage than any other country. But, this abundance is a bit of an illusion. About 60 percent of Canada's fresh water drains north, while 85 percent of the population lives along the southern border with the United States. Not surprisingly then, Canada is rich in fresh water. Our rivers discharge close to nine percent of the world's renewable water supply, while Canada has about half of one percent of the world's population. Everybody knows about the Great Lakes; they make up the largest surface area of fresh water found in one place anywhere in the world. In addition, there are more than 31,000 freshwater lakes in Canada that are larger than three [km.sup.2] in area; about 560 are more than 100 [km.sup.2]. The official definition of a lake is: "Water bodies deep enough (greater than two metres) to contain water for long periods of time and to sustain fish during the winter by not freezing to the bottom." Then, of course, the boffins throw in an exception: "Some shallow water bodies, especially in the Arctic, are considered lakes simply because of their enormous surface area." The major common factor is that lakes are bodies of fresh water: if the water is salty they become inland seas--Black Sea, Dead Sea. Back to those boffins. People who study lakes have a fondness for jargon--words and phrases they use among themselves that the rest of us find a bit baffling baf·fle tr.v. baf·fled, baf·fling, baf·fles 1. To frustrate or check (a person) as by confusing or perplexing; stymie. 2. To impede the force or movement of. n. 1. . Here are a few: * Allochthonous Adj. 1. allochthonous - of rocks, deposits, etc.; found in a place other than where they and their constituents were formed autochthonous - of rocks, deposits, etc.; found where they and their constituents were formed and autochthonous autochthonous /au·toch·tho·nous/ (aw-tok´thah-nus) 1. originating in the same area in which it is found. 2. denoting a tissue graft to a new site on the same individual. . Once a lake is formed it begins to fill up with sediments that will, eventually, cause the lake to disappear. Some of the sediment material comes by wind and erosion (allochthonous), and some from materials formed within the lake (autochthonous). As the sediments build up, marshes, meadows, and forests grow on what was once a lake. For the deepest lakes the process of filling with sediment takes millions of years to complete; * Eutrophication eutrophication (y trō'fĭkā`shən), aging of a lake by biological enrichment of its water. In a young lake the water is cold and clear, supporting little life. . This describes concentration of nutrients, such
as nitrogen or phosphorous phos·pho·rousadj. Of, relating to, or containing phosphorus, especially with a valence of 3 or a valence lower than that of a comparable phosphoric compound. , in a lake. When the concentrations are lowest the water is clear and is called oligotrophic ol·i·go·tro·phic adj. Lacking in plant nutrients and having a large amount of dissolved oxygen throughout. Used of a pond or lake. ol . The grades march upwards through mesotrophic, eutrophic eu·troph·ic adj. Relating to, characterized by, or promoting eutrophia. , to hypereutrophic. Slightly or moderately eutrophic water is good be cause it supports a complex web of plant and animal life. Hypereutrophic gives rise to masses of algae algae (ăl`jē) [plural of Lat. alga=seaweed], a large and diverse group of primarily aquatic plantlike organisms. These organisms were previously classified as a primitive subkingdom of the plant kingdom, the thallophytes (plants that that consume oxygen leaving the water unable to support other life; * Hydraulic retention time The Hydraulic retention time (HRT) is a measure of the average length of time that a soluble compound remains in a constructed reactor. HRT = Volume of aeration tank/influent flowrate . This is the time required for all the water in a lake to pass through its outflow. The approximate retention times for the five Great Lakes are: Lake Superior--191 years Lake Michigan--99 years Lake Huron--22 years Lake Ontario--6 years Lake Erie--2.6 years; * Lentic Adj. 1. lentic - of or relating to or living in still waters (as lakes or ponds) lake - a body of (usually fresh) water surrounded by land lotic - of or relating to or living in actively moving water . This word is applied to lakes because their waters are standing, or still, relative to rivers ("lotic lo·tic adj. Of, relating to, or living in moving water. [From Latin l " systems); * Overturn. The sinking of surface water and rise of bottom water in a lake. This usually happens because of changes in air temperature in spring and fall, but can be the result of a storm. Lakes where this happens are called dimictic. In some lakes, called meromictic, the deepest water remains stagnant and never rises to the top; * Thermal stratification. Lake water nearest the surface is the warmest (in sum met anyway); this upper layer is called the epilimnion Epilimnion is the top-most layer in a thermally stratified lake, occurring above the deeper hypolimnion. It is warmer and typically has a higher pH and dissolved oxygen concentration than the hypolimnion. and the temperature is fairly uniform. The middle layer, or thermocline ther·mo·cline n. A layer in a large body of water, such as a lake, that sharply separates regions differing in temperature, so that the temperature gradient across the layer is abrupt. , is where there is a marked drop in temperature as you go deeper. The lowest level, or hypolimnion hy·po·lim·ni·on n. The layer of water in a thermally stratified lake that lies below the thermocline, is noncirculating, and remains perpetually cold. , is the coldest and, again, the temperature is fairly uniform. There are a tonne more terms listed in a glossary at --http://www.nalms.org/ glossary/glossary.htm
Canadian provinces and territories
ranked by their freshwater surface area
Province / Total area Freshwater % of juris-
territory (land + area diction
water) ([km.sup.2]) covered
([km.sup.2]) by fresh-
water
Quebec 1,542,056 176,928 11.5
Northwest 1,346,106 163,021 12.1
Territories
Ontario 1,076,395 158,654 14.7
Nunavut 2,093,190 157,077 7.5
Manitoba 647,797 94,241 14.5
Saskat- 651,036 59,366 9.1
chewan
Newfound- 405,212 31,340 7.7
land
British 944,735 19,549 2.1
Columbia
Alberta 661,848 19,531 2.9
Yukon 482,443 8,052 1.7
Nova 55,284 1,946 3.5
Scotia
New 72,908 1,458 2.0
Brunswick
Prince Ed- 5,660 -- 0.0
ward Island
Canada 9,984,670 891,163 8.9
Province / % of total
territory Canadian
freshwater
area
Quebec 19.9
Northwest 18.3
Territories
Ontario 17.8
Nunavut 17.5
Manitoba 10.6
Saskat- 6.7
chewan
Newfound- 3.5
land
British 2.2
Columbia
Alberta 2.2
Yukon 0.9
Nova 0.2
Scotia
New 0.2
Brunswick
Prince Ed- <0.1
ward Island
Canada 100.0
Source: Canada. Natural Resources Canada. The Atlas of Canada.
Facts About Canada: Land and Freshwater Areas, Ottawa,
1999.
FACT FILE Freshwater lakes, rivers, and underground aquifers hold only 2,5% of the world's water, By comparison, saltwater oceans and seas contain 97.5% of the world's water supply. FACT FILE The most popular name for a lake in Canada is "Long"--there are 204 of them. |
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