Earthquake Hazard GIS Modelling in the Greater Vancouver Regional District |
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The slope instability
cartographic model is broken down into 3 smaller models:
The above two models are then overlayed to produce the final Slope Instability cartographic model as shown below. Note: You can click on slope.rdc and slopedegreeinstability.rdc to see the corresponding maps. The clicked map will pop up in another window. Note: You can click on aspect.rdc and aspectinstability.rdc to see the corresponding maps. The clicked map will pop up in another window. Note: You can click on bedrocktype.rdc and bedrockinstability.rdc to see the corresponding maps. The clicked map will pop up in another window. Note: You can click on slopeinstability.rdc, bedrockinstability.rdc, slopedegreeinstability.rdc, slopeinstability.pdf, slopeinstability.rdc, notdeveloped.rdc and highland.rdc to see the corresponding maps and table. The clicked map/table will pop up in another window.
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NOTE: This web is created on Nov 19, 2002 by Carol Cheuk (Student #: 973003525) for course GEOG355 Project. It is optimized for resolutions of 1024x768 and above and requires the use of Microsoft Internet Explorer or Javascript enable browser for best results. |