PHYSIOGRAPHIC REGIONS CANADIAN SHIELD: (4 billion years old) Formed through extreme volcanic activity, left igneous rocks rich in minerals Shaped through billions of years of erosion and glaciers Put minerals within reach Left behind 1000’s of lakes Climate – northern winters are long, cold with shorter cooler summers Population –based on resource towns GREAT LAKES-ST.LAWRENCE LOWLANDS Formed as glaciers receded, creating rolling landscapes and carving out great lakes The lowlands were formed by faulting (tension caused plates to pull apart, creating valley As glaciers melted left behind rich soil Humid continental climate influenced by Great Lakes Home to half of Canada’s population APPALACHIAN Formed as N.American and Eurasian plate movements caused folding of sedimentary rock on ocean floor Shaped by erosion – flattened mountains, created plains between, oceans flooded lowlands creating jagged coastline Maritime climate; cooler than BC because of winds blowing off of continent and cooler Atlantic O. Communities developed along coast near ports and in valleys near rich farmland INTERIOR PLAINS Formed when inland seas filled with sediment Shaped by erosion, glaciers Thick soil layers Sea life changes to oil/natural gas Climate: continental, more extreme, hot summers, cold winters Many farming and ranch communities; cities developed on the banks of rivers WESTERN CORDILLERA Formed as the movement of the Pacific and North American plates folded earth’s crust, volcanic eruptions, lava formed interior plateau Shaped by glaciers, erosion Rich in minerals, forests, orchards Maritime, temperate climate; northern regions have a cooler climate Major cities developed in the southern region along Fraser River ARCTIC Formed as plate movements folded sedimentary rock upwards (Innutians), and islands also formed from sedimentary rock Shaped by glaciers, rising sea levels Left behind barren surface, some oil and natural gas deposits Very severe climate; very little precipitation Low population; mainly Inuit