Earth's surface experiences change driven by relief, sea level, hydroclimate and human activity. Extreme hydroclimatic events combined with human activity on steep slopes and/or adjacent to low-lying coasts generate natural hazards. If there is little or no human activity in an area where a natural disaster occurs, we speak of a geophysical event. For example, a flood or a LANDSLIDE in an uninhabited part of the Canadian Arctic is a geophysical event. Where geophysical events interact with society, however indirectly, they are called natural hazards. A flood or a landslide that occurs in the lower Fraser River valley of British Columbia is thus a natural hazard.
Specific geomorphological processes and natural hazards tend to be associated with specific terrain units: ROCKSLIDES are relatively common in areas of dipping stratified rocks; slumps, earthflows and debris flows tend to occur on finely textured materials (eg, lacustrine silts, clays, tills); finely textured materials also encourage surface erosion and gullying; all active fluvial areas adjacent to river channels are flood-hazard zones; piping, causing collapse and settling, is associated with lacustrine silts; sinkhole development is associated with limestone and gypsum lithologies. EARTHQUAKE hazard is not restricted to a specific terrain unit, but the severity of the effect is greatest in thick deposits of sensitive materials.
It is important to recognize a distinction between land cover and land use. Land cover includes biota (a region's flora and fauna), soils, topography, surface and groundwater, and built structures; land use is the purpose for which humans exploit land cover. Land use involves both the manner and purpose of manipulation.
Land has a finite capability to resist the natural processes of EROSION. If we compare, for example, 2 relatively pristine environments, such as the COAST MOUNTAINS of British Columbia and the BADLANDS of Alberta, the Coast Mountains are 3-4 orders of magnitude more resistant to erosion than the badlands. There exists a broad spectrum of land resistance to erosion between these 2 extremes. It is therefore important, when land managers consider disturbing the land cover by introducing new land use, that they consider the optimal use of that land and do not exceed the threshold of resistance. Examples of failure to observe the optimal use of land exist throughout Canada's expanding urban areas, with catastrophic results for individual homeowners.
There are many ways of defining sustainability, but few have improved on the original definition provided by Gro Harlem Brundtland (1987), "ensuring that the needs of the present generation and the human activity arising from those needs do not compromise the ability of future generations to meet their own needs." The availability of land of adequate quality and quantity is an obvious critical consideration in the ongoing sustainability debate. Determining and implementing the optimal use of land in the present will do much to ensure that future generations' needs can be met. Included among these sustainable land use options are both enhancing the land cover and, in some cases, simply leaving the land cover undisturbed. (See also SUSTAINABLE DEVELOPMENT.)
In the 1960s and 1970s, Canada was a leader in establishing public awareness of land use issues. The CANADA LAND INVENTORY program (1965-75), which assessed and mapped the natural capability of approximately 25% of Canada's land area, contributed to a new sensitivity to land quality problems. The underlying concepts in this program were that land has a finite capability to sustain a given type of land use, that it has a finite capability to assimilate pollutants and that it is possible to define optimal uses for a given land unit. The Environmental Assessment and Review Process (EARP), 1973, introduced the twin principles of delaying or halting development proposals that were not respectful of the finite capability of the land, and requiring a regular audit of ways in which the land was disturbed by the development initiative (see ENVIRONMENTAL IMPACT ASSESSMENT).
Since the 1970s the terms of reference of the process have moved toward a more SOCIAL IMPACT ASSESSMENT and in the first decade of the 21st century, the integrity of the process is threatened by a perceived need to speed up the decision-making. The issue has become politically polarized between land developers and those who recognize the strong relation between the health of ECOSYSTEMS and human well-being. The land, its use and its future potential are the main ingredients in the debate.
Author OLAV SLAYMAKER
W. Neil Adger and Katrina Brown, Land Use and the Causes of Global Warming (1994); J. Alan Heginbottom, co-ordinator, "A Survey of Geomorphic Processes in Canada," Quaternary Geology of Canada and Greenland (1989); Eric F. Lambin and Helmut Geist, Land Use and Land Cover Change: Local Processes and Global Impacts (2006); Wendy Simpson-Lewis, Ruth McKechnie, V.P. Neimanis, editors, Stress on Land in Canada (1983); Millennium Ecosystem Assessment, Ecosystems and Human Well-Being: A Framework for Assessment (2005); Gilbert F. White, Natural Hazards (1974).
Links to Other Sites
Glossary: Terrain Classification
Glossary of technical terms related to terrain features in the landscape. A Government of British Columbia website.
An extensive information source about "Canada Lands" as defined by the "Canada Lands Surveys Act." From Natural Resources Canada.
An illustrated overview of geological hazards in Alberta. From the Alberta Geological Survey.
Shawnadithit grew anxious waiting for her uncle, Longnon, to return to camp at the junction of Badger Brook and the Exploits River, deep in the wilds of Newfoundland...