BIO211H5 Study Guide - Final Guide: Radiocarbon Dating, Schist, North American Plate

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Origin of earth o o o: mantle (40-2890 km) o o crust (0-40 km) liquid iron core (2890-5150 km) solid iron core (5150-6370 km) Meteorite impacts increased concentrations of some elements in upper earth. Mafic: high in magnesium and iron oceanic crust: denser and heaver, more mafic continental: lighter, less dense, felsic oldest rocks on earth are small archean fragments high heat flow limited continental thickness zircon crystals: 4. 1-4. 2 billion years old. 2 continental collide: mountains o o o o. Mohorovicic: boundary between the mantle and the crust. 40-0km deep (0 at volcanoes) continental: thicker, less dense oceanic: thinner, more dense together with the uppermost mantle, makes up the lithosphere. Earth is an archive geologic record archives earth"s history results from the interaction of complex systems within the planet the lithosphere (specifically the sedimentary rocks of the crust) contains the record of life on earth.

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