CAS BI 260 Lecture Notes - Lecture 2: Georges Bank, Continental Margin, Thermocline

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A hypothesis of sea floorspreading and plate tectonics. A structure is a product of plate tectonics and major features are similar around world. 890 of ocean"s surface area i continental shelf biologicallyrich area shelfends at shelf break depth 120 400in. Ii continentalslope thought of as edge of continent shelf that begins at shelf break and goes to seafloor. Steep iii continental rise formed by sediments that have been pushed down from shelf iv continental margin can be active or passive thought of continental he shelfbreak continental slope continental sediment. 1 margin like underwater abyssal plain river delta a activemargins sites of more intensegeologicactivity incl earthquakes and volcanoes characterized by steeprocky shorelines narrow shelf and steepslope. 1 ex west coast usa passivemargins relatively inactive geologically characterized by flat wide coastal plains wide shelf and gradual sloping slope. 1 ex east coast usa v example georges bank off ma. Iii chemical and physical properties of sea water.

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