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2/3 of Earth’s surface  covered by ocean Exist on Earth for more than 3 billion yrs. 5 major oceans: Pacific, Atlantic, Indian, Southern, Artic Control.

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Presentation on theme: "2/3 of Earth’s surface  covered by ocean Exist on Earth for more than 3 billion yrs. 5 major oceans: Pacific, Atlantic, Indian, Southern, Artic Control."— Presentation transcript:

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2 2/3 of Earth’s surface  covered by ocean Exist on Earth for more than 3 billion yrs. 5 major oceans: Pacific, Atlantic, Indian, Southern, Artic Control Earth’s temperature Create weather patterns Water source - Support all life form

3 Ocean Basins =low points on the Earth’s surface Water flows into basin =create ocean Hundreds of millions of years for oceans to fill up to present levels from water that ran off the continents

4 Planet first formed  hot ball of molten rock Outside of Earth cooled down Heat released from deep within the planet through volcanoes Water inside volcanic materials also released into the atmosphere  form of water vapour Water vapour cooled & condensed = fall on to Earth’s surface as rain Gravity causes water to fall downhill  water that fell collected in the lowest parts of Earth’s surface- the ocean basins Original water on planet came from ice in comets that hit the young Earth

5 Has interesting & varied landscape like Earth’s continents Features found on land: mountain ranges, valleys, flat plains, canyons, and volcanoes  also exist on ocean floor 2 distinct parts -Largest: middle part (general ocean basin) -Rising outside edges (continental margins)

6 Tectonic plates =large sections of rock that the entire surface of Earth is made up of Sections of rock are solid but float over a layer of molten rock (magma) Magma heats up =molten rock rises Pressure =force 2 plates apart 2 types of tectonic plates -Continental: lie under continents -Oceanic plate: lie under oceans, dense

7 Plates pushed apart  magma oozes up into the empty space Under ocean =mid-ocean ridge Magma cools at mid-ocean ridges  becomes newest rock on planet Rising & hardening of magma forces plates to continually move apart  ocean floors grow wider & wider Plates moving apart from mid-ocean ridge must come in contact with other plates.

8 Subduction =process where oceanic plate collides with continental plate  the denser oceanic plate forced to slip underneath continental plate When subduction occurs  ocean trench is formed Trench =long V-shaped groove that marks boundary between oceanic plate & continental plate Ridges =develop usually in middle of ocean basin Trenches = tend to develop near outer edges Trench

9 Abyssal plains =wide, flat areas that are stretching between areas of trenches & mid-ocean ridges Make up 30% of Atlantic ocean floor & more than 75% of Pacific ocean floor These flat areas  broken by occasional underwater peak called a seamount Seamount = an old inactive volcano that once developed near a mid-ocean ridge

10 Continental margins = regions of the ocean floor that lie underwater along the edge of the continents These margins are made up of: - continental shelf =flat area that extends from continent’s shoreline to ocean basin - continental slope =steep area that drops off rapidly to the ocean basin from edge of the continental shelf During last ice age  continental shelves in northern hemisphere =not under water More ocean water became locked up as ice  water level fell leaving the shelves exposed

11 Sediments  carried into the ocean by rivers flowing off the continents Sediments build up along the steep continental slope Build-up becomes too big =gravity suddenly causes slope to give way Resulting collapse =turbidity current Turbidity current =underwater landslide that can travel hundreds of km down the continental slope & out along ocean floor Turbidity currents  deposit piles of sediment that form the continental rise Continental rise =between continental slope & abyssal plain.

12 Some turbidity currents  powerful enough to carve out large sections of continental shelf & continental slope =creates submarine canyons Result =underwater landscape Submarine canyons  also found in regions where large rivers reach ocean

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