ENV234H1 : NotesENV234.doc
Document Summary
Patterns of climate change and climate variation, and is focused mostly on the surrounding area in ontario, for relevancy to the course. September 10th: deep geology ice ages- consequences of ice ages on canada and ontario"s geomorphology. The canadian shield is dated back to the precambrian time and before organisms appear. It is the world"s largest area of precambrian bedrock. It"s continuous and stayed together as an un- encroached landmass even when continents shifted. The canadian shield is also called the laurntien shield. The shield is low in altitude- 300m to 600m in elevation and around 1500m in baffin and. Labrador: nutrients are low because it"s old and many have been leached away from plants, and eroded away from glaciers. The soils derived from this rock are very poor. The round mountains of the georgian bay prove how glaciers affect the earth, they are very erosive.