Obabika River
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Obabika River
The Obabika River is located in central Ontario, Canada. It is south of Lady Evelyn-Smoothwater Provincial Park and west of Lake Temagami, within Sudbury District. It flows from Obabika Lake in a south-westerly direction and drains into the Sturgeon River. The Obabika River is remote and surrounded by undeveloped wilderness. The river is characterized by long meandering sections through clay and sand valleys alternated by sections through eroded bedrock and marshes. The lower Obabika River is rather wide with several oxbow ponds, and obstructed by occasional log jams. Although the current is strong, the only noteworthy rapids occur immediately before its confluence with the Sturgeon River. With its steady current and few portages, the Obabika River is a popular canoe route within the Temagami region, linking Lake Temagami and Lady Evelyn Lake via Obabika Lake to the Sturgeon River. It is part of the traditional indigenous travel network called "nastawgan", which has changed lit ...
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Provinces And Territories Of Canada
Within the geographical areas of Canada, the ten provinces and three territories are sub-national administrative divisions under the jurisdiction of the Canadian Constitution. In the 1867 Canadian Confederation, three provinces of British North America—New Brunswick, Nova Scotia, and the Province of Canada (which upon Confederation was divided into Ontario and Quebec)—united to form a federation, becoming a fully independent country over the next century. Over its history, Canada's international borders have changed several times as it has added territories and provinces, making it the world's second-largest country by area. The major difference between a Canadian province and a territory is that provinces receive their power and authority from the ''Constitution Act, 1867'' (formerly called the ''British North America Act, 1867''), whereas territorial governments are creatures of statute with powers delegated to them by the Parliament of Canada. The powers flowing from t ...
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Log Jam
A log jam is a naturally occurring phenomenon characterized by a dense accumulation of tree trunks and pieces of large wood across a vast section of a river, stream, or lake. ("Large wood" is commonly defined as pieces of wood more than in diameter and more than long) Log jams in rivers and streams often span the entirety of the water's surface from Bank (geography), bank to bank. Log jams form when trees floating in the water become entangled with other trees floating in the water, or become snagged on rocks, large woody debris, or other objects anchored underwater. They can build up slowly over months or years, or they can happen instantaneously when large numbers of trees are swept into the water after natural disasters. A notable example caused by a natural disaster is the log jam that occurred in Spirit Lake (Washington)#Mount St. Helens eruption, Spirit Lake following a landslide triggered by the 1980 eruption of Mount St. Helens, eruption of Mount St. Helens. Until they ar ...
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Rivers Of Sudbury District
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as Stream#Creek, creek, Stream#Brook, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to Geographical feature, geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "Burn (landform), burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from Precipitation (meteorology), precipitation through a ...
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List Of Rivers Of Ontario
This is the list of rivers which are in and flow through Ontario. The watershed list includes tributaries as well. Dee River, flows between Three Mile Lake and Lake Rosseau. List of rivers arranged by watershed Hudson Bay Atlantic Ocean Alphabetical list of rivers See also * List of rivers of Canada *List of rivers of the Americas *Hudson Bay drainage basin *List of lakes of Ontario * Geography of Ontario References {{Canada topic, List of rivers of Ontario * Rivers A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of wate ...
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Timiskaming District
Timiskaming is a district and census division in Northeastern Ontario in the Canadian province of Ontario. The district was created in 1912 from parts of Algoma, Nipissing, and Sudbury districts. In 1921, Cochrane District was created from parts of this district and parts of Thunder Bay District. The division had a population of 32,251 in the Canada 2016 Census. The land area is ; the population density was . It is just west of the similarly named Témiscamingue county in Québec, which is also informally called a region, but is administratively part of a greater region named Abitibi-Témiscamingue. Temiskaming District is home to several provincial parks. History The ''coureurs de bois'' explored and traded fur in what is now the Timiskaming District, in the 17th century. Subdivisions City * Temiskaming Shores (Haileybury, New Liskeard, Dymond Township, North Cobalt) Towns * Cobalt * Englehart * Kirkland Lake (Chaput Hughes, Swastika) * Latchford Townships * Arms ...
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Nipissing District
Nipissing District is a district in Northeastern Ontario in the Canadian province of Ontario. It was created in 1858. The district seat is North Bay. In 2016, the population was 83,150. The land area is ; the population density was , making it one of the most densely populated districts in northern Ontario. History The Sudbury District was created in 1894 from townships of eastern Algoma District and west Nipissing District. The Timiskaming District was created in 1912 from parts of Algoma, Nipissing, and Sudbury Districts. Subdivisions City * North Bay Towns * Mattawa * Temagami *West Nipissing In addition, the eastern part of the town of Kearney is within Nipissing District, but the entire town is enumerated with the Parry Sound District. Townships * Bonfield * Calvin * Chisholm * East Ferris * Mattawan * Papineau-Cameron * South Algonquin Unorganized areas * North Part * South Part Local services boards in these unorganized areas include: * Redbridge * Thorne ...
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Obabika Old-Growth Forest
Obabika old-growth forest is an Eastern White Pine and Red Pine dominated old-growth forest at the north end of Obabika Lake, just west of the Temagami region of Ontario, Canada. At in size, it is commonly considered to be the largest remaining white pine dominated old-growth forest in the world. It is also sometimes called Chee-Skon Lake old-growth forest, or Wakimika Triangle old-growth forest. This area was slated for logging in 1989 and was protected largely as a result of a blockade on Red Squirrel Road in which 344 protestors were arrested, including future Ontario premier Bob Rae. The oldest trees in the Obabika old-growth forest are confirmed to be at least 375 years old, but a diversity of age classes occur in this forest. Another important feature of the area is the spirit rock, a column of rock on the shore of Chee-Skon Lake that is of spiritual significance to the Teme-Augama Anishnabai people. The Obabika old-growth forest is protected within the Obabika River Provinc ...
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Lady Evelyn Lake
Lady Evelyn Lake is a lake on the Lady Evelyn River in Timiskaming District, Northeastern Ontario, Canada. The highly irregularly shaped lake consists of two parts, about equal in size, separated by the Obisaga Narrows. The southern part is within the Obabika River Provincial Park, directly east of the Lady Evelyn-Smoothwater Provincial Park. Lady Evelyn River is a tributary of the Montreal River (Timiskaming District), Montreal River, which is a tributary of the Ottawa River. See also *List of lakes in Ontario References National Resources Canada
Lakes of Timiskaming District {{Ontario-geo-stub ...
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Canoe Camping
Canoe camping, also known as touring, tripping or expedition canoeing, is a combination of canoeing and camping. Like backpacking, canoe campers carry enough with them to travel and camp for several days, but do so via a canoe or kayak. Description A canoeist can transport significantly heavier and bulkier loads than a backpacker or even a kayaker can. Portaging by foot is sometimes necessary to pass between water bodies or around hazardous obstacles such as rapids or waterfalls, but most of the time canoe campers travel on water. Because they usually don't continuously carry their gear on their backs, canoe campers can bring more food and gear and undertake longer trips. This is especially the case with food which, unlike gear where the weight is essentially fixed regardless of the trip duration, increases in weight for each additional day of provision. On rivers, high water levels after storms can make river travel hazardous, while on lakes, winds and thunderstorms can produc ...
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Portage
Portage or portaging (Canada: ; ) is the practice of carrying water craft or cargo over land, either around an obstacle in a river, or between two bodies of water. A path where items are regularly carried between bodies of water is also called a ''portage.'' The term comes from French, where means "to carry," as in "portable". In Canada, the term "carrying-place" was sometimes used. Early French explorers in New France and French Louisiana encountered many rapids and cascades. The Native Americans carried their canoes over land to avoid river obstacles. Over time, important portages were sometimes provided with canals with locks, and even portage railways. Primitive portaging generally involves carrying the vessel and its contents across the portage in multiple trips. Small canoes can be portaged by carrying them inverted over one's shoulders and the center strut may be designed in the style of a yoke to facilitate this. Historically, voyageurs often employed tump lines on t ...
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Rapid
Rapids are sections of a river where the river bed has a relatively steep gradient, causing an increase in water velocity and turbulence. Rapids are hydrological features between a ''run'' (a smoothly flowing part of a stream) and a ''cascade''. Rapids are characterized by the river becoming shallower with some rocks exposed above the flow surface. As flowing water splashes over and around the rocks, air bubbles become mixed in with it and portions of the surface acquire a white color, forming what is called "whitewater". Rapids occur where the bed material is highly resistant to the erosive power of the stream in comparison with the bed downstream of the rapids. Very young streams flowing across solid rock may be rapids for much of their length. Rapids cause water aeration of the stream or river, resulting in better water quality. Rapids are categorized in classes, generally running from I to VI. A Class 5 rapid may be categorized as Class 5.1-5.9. While Class I rapids are eas ...
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Oxbow Lake
An oxbow lake is a U-shaped lake or pool that forms when a wide meander of a river is cut off, creating a free-standing body of water. In South Texas, oxbows left by the Rio Grande are called '' resacas''. In Australia, oxbow lakes are called billabongs. The word "oxbow" can also refer to a U-shaped bend in a river or stream, whether or not it is cut off from the main stream. Geology An oxbow lake forms when a meandering river erodes through the neck of one of its meanders. This takes place because meanders tend to grow and become more curved over time. The river then follows a shorter course that bypasses the meander. The entrances to the abandoned meander eventually silt up, forming an oxbow lake. Because oxbow lakes are stillwater lakes, with no current flowing through them, the entire lake gradually silts up, becoming a bog or swamp and then evaporating completely. When a river reaches a low-lying plain, often in its final course to the sea or a lake, it meanders wi ...
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