The Ocean Floor and Margins Chapter 14
The vast world ocean Earth is often referred to as the blue planet Seventy-one percent of Earth’s surface is represented by oceans and marginal seas Continents and islands comprise the remaining 29
Views of the Northern and Southern hemispheres
The vast world ocean Four main ocean basins Pacific Ocean - the LARGEST and has the GREATEST DEPTH. Atlantic Ocean – about HALF the size of the Pacific and not quite as deep. Indian Ocean – SLIGHTLY SMALLER THAN the ATLANTIC. Arctic Ocean – about 7 PERCENT the SIZE OF the PACIFIC.
The oceans of Earth
Mapping the ocean floor Bathymetry – measurement of ocean depths and the charting of the shape or topography of the ocean floor Echo sounder (also referred to as SONAR) Primary instrument for measuring depth Reflects sound from ocean floor
EXAMPLES: LeadlineSingle Beam Multibeam 1-2 K soundings per survey K soundings per survey 400,000 – 1,000,000 K soundings per survey Image courtesy of NOAA & UNH
Echo sounder
Multibeam sonar
Careful coverge to map the seafloor
Mapping the ocean floor Three major topographic units of the ocean floor Continental margins Ocean basin floor Mid-ocean ridge
Major topographic divisions of the North Atlantic Ocean
Seafloor Features: Continental Margins Continental shelf - extends from shore to a point marked by great increase in slope Continental slope - steep slope beyond the continental shelf break Submarine canyons Deep, steep-sided valleys cut into the continental slope. eroded by turbidity currents (dense mudflows) or seaward extensions of river valleys.
Continental rise (thick accumulation of sediment at base of continental slope) found in regions where trenches are absent
Continental Margin CONTINENTAL SHELF CONTINENTAL SLOPE CONTINENTAL RISE
Turbidity currents (currents of mud and water) flow down the continental margin
Features of continental margins
Seafloor Features: Deep Ocean Basin Abyssal plain - the most level place on Earth Sites of thick accumulations of sediment Found in all oceans Seamounts - underwater volcanoes 500 m to 1000 m high flat-topped ones are called guyots Mid-Ocean Ridges – divergent boundaries on the seafloor Trenches – at subduction zones
TRENCH ABYSSAL PLAIN GUYOT SEAMOUNT
Continental margins Passive continental margins No subduction
Passive Continental Margin
Features of a passive continental margin
Passive Continental Margin PASSIVE CONTINENTAL MARGIN
Continental margins Active continental margins Subduction
An active continental margin
Active Continental Margin
ACTIVE CONTINENTAL MARGIN
Label the Diagrams on the Seafloor Worksheet
Seafloor sediments Mud is the most common sediment on the deep-ocean floor
Carbonate Compensation Depth
Distribution of marine sediments
Ocean Water and Ocean Life Chapter 15
Composition of seawater Seawater consists of about 3.5% (by weight) dissolved minerals. Salinity Total amt. of solid material dissolved in water Average salinity is 3.5% Major constituent is sodium chloride would = Layer of salt 200 ft thick over entire ocean floor
Relative proportions of water and dissolved components in seawater
Where do the Dissolved Minerals come from? Chemical weathering of rocks on the continents carried by rivers (adds sodium+) Volcanic outgassing (adds chlorine and sulfur+)
Destination of Dissolved Mineral Solids Salinity of seawater does not change, so material must be removed as fast as it is delivered. Where does it all go? Hard parts of plants and animals, e. g. sea shells Chemical sedimentary rocks
Variations in Salinity (page 409) High salinity Areas of high evaporation Low salinity Areas of high rain (tropics) or at the mouths of rivers (Gulf of Mexico)
Ocean temperature Surface water temperature varies with the amount of solar radiation received Lower surface temperatures are found in high-latitude regions No rapid temperature change with depth Higher temperatures found in low- latitude regions Rapid decreasing temperature with depth
Variations in ocean water temperature with depth (fig on page 410) Temperature of Ocean Water #32
Ocean density Factors affecting seawater density Salinity Temperature - the greatest influence Fresh vs. saltwater density
Variations in ocean water temperature with depth (fig on page 410)
Variations in ocean water density with depth
Layering in the ocean
Ocean life Most organisms live within the sunlight surface waters (photosynthesis) Classification of marine organisms Plankton (floaters) like algae and zooplankton
Ocean life Nekton (swimmers)
Ocean life Benthos (bottom dwellers)
Marine life zones Plankton N e k t o n Benthos Continental slope Continental shelf Abyssal Plain Intertidal zone
Chapter 16 The Dynamic Ocean
Ocean water movements Surface circulation Surface currents develop from friction between the ocean and the WIND that blows across the surface
Average ocean surface currents in February-March
Ocean water movements Surface circulation Deflected by the Coriolis effect To the right in the Northern Hemisphere To the left in the Southern Hemisphere
Ocean water movements Upwelling The rising of cold water from deeper layers Caused by surface winds Brings greater concentrations of dissolved nutrients to the ocean surface
Ocean water movements Deep-ocean circulation A response to density differences (density currents) Temperature – cold water is denser Salinity – density increases with increasing salinity
Layering in the ocean
Copyright N.W. Driscoll, Woods Hole Oceanographic Institute Thermohaline Oceanic Circulation
Idealized “conveyor belt”model of ocean circulation Cold, higher salinity Warm, lower salinity
Demos Home page
Waves On The Beach As the wave travels in shallower water it slows and eventually falls forward as a breaker.
Wind or Storm Waves The most familiar waves are wind generated.
Wind or Storm Waves There are 3 things that determine how large these waves can become.
1.Wind speed 2.Wind duration - time 3.Fetch – distance over which the wind blows
Breakers
Tides Tides are caused mainly by the gravitational pull of the moon.
Idealized TIDAL BULGES on the Earth
As the earth rotates, two high tides and two low tides occur each day
Tides Monthly tidal cycle Spring tide During new and full moons Gravitational forces of the moon and the sun added together Especially high and especially low tides Large daily tidal range
Earth-Moon-Sun positions during the Spring tide (sun,moon, earth all lined up)
High tide in the Bay of Fundy along the Nova Scotia coast
Low tide in the Bay of Fundy along the Nova Scotia coast
Life in the tidal flats is exposed at low tide
Hydroelectric Power here is highly productive, but endangers the salt marshes and local habitat.
Tides Monthly tidal cycle Neap tide First and third quarters of the Moon Daily tidal range is least
Earth-Moon-Sun positions during the Neap tide (sun, moon and earth form right angle)
Label Diagrams in notes as Spring and Neap Tide