Introduction:
Canada is a great place to live. Winnipeg… is good enough. Winnipeg is known for its diverse population, festive multiculturalism, beautiful architecture, vast prairie land and The Jets. One thing Winnipeg is definitely not known for, being a geological hazards hot spot. These hazards are geological events that take place, which have an impact on civilization. Canada is impacted by a wide scope of events ranging from earthquakes to fires. However, Winnipeg is lucky to be conveniently located away from any seismic activity, any threat of coastal dangers, any mountain risks and lastly it is absent of even the slightest volcano. Therefore, what Winnipeg lacks in attraction it makes up for in safety. In spite of its perceived security this major Canadian city is unfortunately prone to some very serious dangers. It is home to very cold, lengthy winters, dreadful storms that lead to wet springs. Scientifically speaking “geohazards are any geological or hydrological process that poses a threat to people and/or their property” (Bilderback, 2013). Thus, the geological hazards that will be discussed in this paper are flooding, landslides, and severe weather including tornadoes and storms.
Winnipeg follows settlement trends, and happens to be amidst two very large-scale rivers. Having been quite convenient for transportation and trading purposes, it seemed like a great location for a city. Fast-forward to the year 1950, the people canoeing to work on top of water reaching 4.5 meters deep in lower areas of the city (Passfield, 2001), resentful feelings began to arise.
Ultimately leading to the proposals and implementation of the Red River Floodway. Floods the biggest geological challenge that Winnipeg faces and ...
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Service Canada. 2013. Severe Storms. Get Prepared. Government of Canada. www.getprepared.gc.ca/cnt/hzd/svrstrms-eng.aspx
Case study: the flooding that occurred in Minden Hills in the spring of 2013, flooded the downtown core. The picturesque cottage town has the Gull River flowing through it. The river overflowed in April because of many reasons: a couple of days of rain, the third largest amount in over a century, but it also happened because the frost in the ground stopped the water from going into the Earth, the lakes and rivers being full from the spring thaw, and the rapid
Gregory Wigmore’s article Before the Railroad: From Slavery to Freedom in the Canadian-American Borderland covers the main theme of local history during the 19th century in Detroit and Windsor. In particular, Wigmore looks at how the Detroit River served as an escape route between the transnational borders for slaves living on both sides of the river. Wigmore explores how the border was the godsend for the slaves because a simple cross across the river would allow them their freedom. Wigmore’s main focus is the many factors and laws that happened between the 1810’s and the 1820’s that played an important role in this freedom.
This is a report based on three days of observations and testing in the region known as the Peterborough drumlin field. It will address a variety of regional elements, such as climate, soil, vegetation, hydrology, geomorphology, and geology. A variety of sites located on the Canadian Shield, the zone of thick glacial deposits to the south, and the transition between them will be the focus of the report. It is supplemented with previous research on the region. September 8, 1999, day one of the field study involved an area of largely granite bedrock that is part of the Canadian Shield and is the most northern point of study (see Map 2). September 9, 1999, day two, involved three main areas of study: the Bridgenorth esker (Map 3), Mark S. Burnham Park (Map 4), and the Rice Lake drumlin (Map 6). These sites are in areas of thick glacial deposits. September 10, 1999, day three, involved studying the Warsaw Caves (see Map 5) as a transition zone between Precambrian Shield rock to the north and Paleozoic rock to the south. A general map of the entire study region is provided by Map 1.
A major flood on any river is both a long-term and a short-term event, particularly any river basin where human influence has exerted "control" over the ri...
The one feature common to the Hoover Dam, The Mississippi river and the three gorges dam is that they all tried to control nature’s swings, specifically in the form of flooding. Before the Hoover dam was built, the Colorado river “used to flood spectacularly…but after 1900 the Colorado provoked a vehement response” (Pg 177). The response was simple, but large. The U.S. built several large dams, including the Hoover dam, on the Colorado to decrease its flooding and increase power and irrigation. Unfortunately, just as human control of the Colorado’s flooding increased, its organisms and habitats were detrimentally influenced, and the water became more and more salinated.
“Clearing the Plains” begins set in the time period of 1100 C.E before Europeans ever settle into Canada. It depicts the laid back lifestyle that Indgienous people became accustomed to where everyone had a role and the community worked together to survive. However, as time goes on the Indigenous populations becomes thrust into a disease stricken society where there is no hope for survival due to minimal resources. The author, James Daschuk goes on to argue the reasons for this
The South Fork Dam collapsed and unleashed 20 million tons of water from its reservoir. A wall of water, reaching up to 70 feet high, swept 14 miles down the Little Conemaugh River Valley, carrying away steel mills, houses, livestock and people. At 4:07 p.m., the floodwaters rushed into the industrial city of Johnstown, crushing houses and downtown businesses in a whirlpool that lasted 10 minutes. (New York Times, 1889).
Tapas Biswas, A. K. a. J. A., 2012. Recent Floods and Salinity of the Murray River. [Online]
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New Orleans flooding risks originated from its location characteristics in proximity of Mississippi River. Since its foundation up to 1927, New Orleans water and flooding threats originated from Mississippi River but human activities had contained this by 1930s. Regrettably, this led to additional water problems. Accordingly, the critical changes to the New Orleans environment originating from the human development worsened the water problems in area caused by the floods. In particular, the growth in ...
The Red River Colony was changing, but it wasn’t the only one, all of Canada were changing, because in the late 1860s Canada entered a new era and the changes and events that occurred in the Red River was only the beginning of many more conflicts and circumstances to come that would help shape and define this age Canada has entered. Although the Red River Rebellion had ostensibly achieved most of its major objectives, the Metis would soon find themselves at a disadvantage. They would rise yet again for another rebellion called The North-West Rebellion of 1885 to assert their nationality once more.
One of the largest geographic physical structures in the United States is the Colorado River. Human activity and its interaction with this great river have an interesting history. The resources provided by the river have been used by humans, and caused conflict for human populations as well. One of these conflicts is water distribution, and the effects drought conditions have played in this distribution throughout the southwestern region. Major cities such as Las Vegas, Los Angeles, San Diego, and other communities in the southwest depend on the river. It provides water for over 20 million people, irrigation for 2 million acres of land, four thousand megawatts of hydroelectric energy, and over twenty million annual visitors for recreation purposes. Also, once in Mexico, the river provides water to irrigate half a million acres of farmland, and municipal and industrial water for 2 million people living in this delta region. The river distributes its flow from lakes and canals along its journey as well. Due to climate change, human demand, natural forces like evaporation and human-induced climate change this water supply is in conflict. Also, a recent change that began in March of 2014 will bring a temporary water surge to the delta of the Colorado River for the first time in many years to help restore this region, and it’s possible it could reach the Sea of Cortez once again.
The Old River control structures were to be operated so as to maintain the distribution of flow and sediments between the lower Mississippi River and the Atchafalaya River in approximately the same proportions as occurred naturally in 1950. That distribution was determined to be approximately 30 percent of the total latitude flow (combined flow in the Red River and Mississippi above the control structures) passing down the Atchafalaya River on an annual basis.
Flooding of settled areas within Australia has become such an inherent event, it is expected yearly during the rainy season. This is due to a mixture of fact that the severe wet season, running from March-April, and October-November, Features cyclones and heavy monsoon rains(Govt, 2013), as well as the composition of the majority of Australia’s coasts being developed due to their great property poten...