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Global warming & its effects What will be the effect of global warming on glaciers and the polar icecap? What will happen to ocean levels and coastal communities in our region? Read p. 27 and discuss! The last ice age! (you think our winters are cold!) Last ice age began about 120 000 years ago, and ended only 11 000 years ago! Almost all of Canada was covered by a glacier! Read pp. 28-30 Solving problems using science Can science alone solve problems like global warming? Cultural views, societal views, etc. are very important part of solving problems. Questions 1-5, p. 28 Questions 1-8, p. 35 Pause and Reflect... p.35 Chapter 2 Exploration of ocean basins Read p. 38-46 Ocean basins The surface of the ocean floor is as varied as the land. The five major oceans, from largest to smallest, are the Pacific the Atlantic the Indian the Southern the Arctic The low points in the oceans are called basins. Oceans are vital to life, as they control temperature, create weather patterns and provide water for water cycles. Basins becoming bigger – demo (p. 41) Ocean basins (cont’d) The ocean basins contain mountains, valleys and plains. The largest changes to the ocean basin occur through the movement of tectonic plates, although there is also erosion via storms, earthquakes and icebergs. Origin of ocean water Oceans have filled over hundreds of millions of years. Scientists believe the oceans are more than 3 billion years old. Water may have originally been released from volcanic eruptions when the vapour from the eruption cooled and condensed. Some believe the water came from ice comets. Origin (cont’d) Pangea began to split up due to plate tectonics. Earth’s surface is made of large, slow-moving sections of rock called tectonic plates. http://www.ucmp.berkeley.edu/geology/anim1.html Technologies for studying ocean basins Read pp. 46-49 STSE Define the following technologies in your notebook: Sonar Satellites Core sampling Underwater photography/videography Deep sea submersibles Diving Write a paragraph explaining how these technologies have improved over time. (ex. Diving vs. Submersible and wire line depth probe vs. Sonar) Continental margins and others Abyssal plains are the pieces of oceanic crust between a spreading mid-ocean ridge and the trench it disappears into. Continental shelf is the submerged part of the continent between the coast and the edge of the basin. Continental slope is the section that slopes downward to the seafloor. Mid-ocean ridge is where the sea floor is still being formed by volcanic eruptions. Two plates are being pushed apart (magma oozes out from the core and hardens) and a mountain change forms! Draw a profile diagram include: continental shelf continental slope abyssal plain mid-ocean ridge Read Science Watch p. 52 Do questions 1-11, p. 53. Ocean Currents Read pp. 54-61 Ocean Currents There are more than 20 major currents which move large amounts of water predictably around the oceans. Currents move large quantities of water, minerals, solar energy, oxygen and carbon dioxide, plankton and fish. Currents are caused and driven by water density and salt content, the wind, the spin of Earth, coastlines and the moon. Largest current is the Antarctic Circumpolar Current in the Southern Ocean, at 24 000 km long Ocean currents are either Surface currents (0 - 200 m) Deep water currents (200 m and deeper) What makes surface currents move? Wind As air warms from solar energy, it rises, and cooler air rushes to replace it. This creates wind. As the wind passes along the surface of the water, it bumps the water molecules and moves them along in the same direction. Spin of the Earth Earth spins from West to East (counter clockwise) The Coriolis effect deflects winds and currents to the right/East in the Northern hemisphere (opposite in the Southern hemisphere) http://video.google.ca/videosearch?q=the%20physics%20of%20weather&h l=en&rlz=1T4GWYE_enCA242CA242&um=1&ie=UTF-8&sa=N&tab=wv# Shape of continents Currents move through the oceans and around the continents like rocks in a stream. What makes deep currents move? Water temperature Like air, warm water rises, and cool water falls Density current = cool, dense water moving on an ocean floor. Three layers of water dependent on temperature: Surface: 0 - 200 m, warmest Thermocline: 200 m - 1 km, rapidly cools Deep water: 1 km and deeper, just above freezing Water salinity Adding fresh water decreases salinity Evaporation and freezing increases salinity Densest ocean waters at the poles Upwelling occurs when nutrient-rich cold water finally moves up to the surface Convection current demo... P. 36 Curriculum Guide Questions 1-10, p. 63 Ocean Waves Read pp. 64-66 Ocean Waves Most waves are created by wind. In open ocean, waves are called swells. Swells “break” in shallow water, called breakers. The largest waves are tsunamis, caused by undersea earthquakes, landslides or volcanic eruptions. Tsunami - From The Discovery Channel-B (12-26-04) ◦ http://video.google.com/videoplay?docid=- 4333412395835151021&vt=lf&hl=en Newfoundland Tsunami and photos http://www.collectionscanada.gc.ca/sos/002028-1100e.html Breakers As a wave approaches the shore, its wavelength decreases and its height increases. Class project! Newfoundland Tsunami Make a poster about the 1929 Newfoundland Tsunami Include: Date Location (map) Cause Death toll Destruction Pictures Tides Read p.69-71 Tides Hopewell Rocks – Bay of Fundy Tides ◦ http://video.google.ca/videoplay?docid=3956711618129258915&ei=-1W5SNTFH4yawH96NnYDA&q=fundy+tides&vt=lf Tides are caused by gravities of Earth and the Moon. High tides occur where the Moon is closest to Earth (and opposite side) Low tides occur at 90º to the high tides. Tidal range (difference between high and low) averages 2 m in NL. The Sun’s gravity, when lined up properly, can produce extreme tides. These are called spring tides When the Sun, Moon and Earth are not lined up, the tides are called neap tides. Questions 1-4, p.71 Shoreline interactions Read pp. 66-69 Interactions at shorelines Waves erode coastal areas based on the force of the waves, and the composition of the shoreline. Headlands made up of harder rock, and erode less, but absorb most wave force. Bays occur between headlands, are generally calm. http://maps.google.ca/maps?sourceid=navclient&ie=UTF8&rlz=1T4GWYE_enCA242CA242&q=Goose%20bay&um=1&sa= N&tab=wl Sea stacks are extra-hard rock left behind from eroded headlands. Reminder from Grade 7... Weathering – breakdown of rocks into smaller particles Erosion – the movement of those weathered particles Deposition – when eroded material is left behin Shorelines Waves have the power to erode shorelines and deposit sediments on the shore. Tides work together with waves and determine the range of shoreline that can be affected by wave action. The interaction with shorelines depend on: Shape of the shoreline Slope of the shoreline (shallow means deposition of sediments, steep means erosion) Type of rock material (sandstone erodes faster than shale) Wave energy Limestone Class Activity 6 groups (4/5 per group) You are to research the processes of erosion and deposition that result from wave action and water flow on one of the following: beaches, shoal, sand bars, sea caves, sea stacks, sea arches Present your findings on a poster. Be sure to include pictures and NL location! Prevention/reduction of wave action along shorelines Breakwaters http://maps.google.ca/maps?sourceid=navclient&ie=U TF8&rlz=1T4GWYE_enCA242CA242&q=foxtrap%20mari na&um=1&sa=N&tab=wl Jetties/wharves Vegetation Questions 1-5, p.69 Read Wild, Weird, Wonderful, p. 76 (The Spout!) http://video.google.ca/videosearch?sourceid=navclient& ie=UTF8&rlz=1T4GWYE_enCA242CA242&q=the%20spout%20e ast%20coast%20trail&um=1&sa=N&tab=wv# Questions 1-13, p. 77 Foldable for review! p. 39 http://video.google.ca/videoplay?docid=669595010475 6107303&ei=pv7fSJrxFoT0gGSy4yiCw&q=the+spout+east+coast+trail&vt=lf List 10 points/key terms in your notebook shown in the video that we have discussed this chapter. Quiz! Test!