BIO211H5 Lecture Notes - Eurasian Plate, Convergent Boundary, North American Plate

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Earth"s lithosphere upper lithosphere crust o o oceanic mafic: rich in mg and fe; more dense continental felsic: rich in silica; less dense lower lithosphere uppermost part of mantle. Moho discontinuity boundary between crust and mantle, occurs within the lithosphere lithosphere divided into plates; sits on top of asthenosphere (upper part of mantle) Continents fit together geological similarities floral (plant life) and faunal (animal life) similarities biostratigraphy: correlation between fossils: much work done by du toit o o. Hawaiian hot spot: area is stationary but the plates above it move thermal plume creates volcano plate moves away from plume stranded volcanoes cool, leaving an island chain chain indicated direction and rate of plate motion. Mid ocean ridges: ex. red sea (three armed rift, one arm may die out east african rift. Valley), mid atlantic ridge transform plate boundaries o transform faults enormous strike-slip faults seismically active o o o o o often occur at offset continental rift zones or mors.

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