grade 8 science unit 1: water systems on earth chapter 2

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Grade 8 Science Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

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Page 1: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

Grade 8 ScienceGrade 8 ScienceUnit 1:

Water Systems on Earth

Chapter 2

Page 2: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

Oceans are Oceans are important...important...1. Primary water source

for the water cycle2. Control weather3. Support diverse life4. Provides humans

with food, minerals, and resources

Page 3: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

The Origin of the The Origin of the OceansOceans1.Tectonic Plates2.Volcanic action3.Erosion4.Glaciation

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Tectonic PlatesTectonic PlatesHas helped determine where ocean basins are located.

Tectonic plates move changing the position of the continents.

Page 5: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

Panthalassa... Oceans then

Page 6: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

Oceans now

Page 7: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

Volcanic ActionVolcanic ActionHas built ocean floor along mid-ocean ridges in areas where plates separate.

Has helped build continental divides in areas where plates have collided and mountain building occurs.

Page 8: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

Water trapped in volcanic materials were released as vapour. It cooled, condensed and fell back to the earth. This water collected in the lowest parts of the Earth’s surface... The ocean basins.

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Page 10: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

ErosionErosionHas aided the further development of continental drainage systems as material is removed and deposited into the ocean basins.

Page 11: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

GlaciationGlaciationA force of erosion in the development of continental drainage systems.

Glaciers move materials towards the oceans.

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Hudson Bay Lowlands, Ontario

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Researching the Ocean Researching the Ocean FloorFloorTechnologies include...1. Sonar2. Satellites3. Core sampling4. Underwater photography/ videography

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5. Deep sea submersibles

6. Diving

Refer to pages 46 - 49

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““UNDERSEA UNDERSEA ADVENTURE”ADVENTURE”

CORE STSE

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Underwater explorationsUnderwater explorations

ShipwrecksEx. The Titanic Discovered in 1985

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Technologies: Past & Technologies: Past & PresentPresentDiving Submersib

les

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Wire line depth probe

Sonar

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““GETTING TO GETTING TO KNOW THE KNOW THE

OCEAN FLOOR”OCEAN FLOOR”

Activity 2-2 page 50-51

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Continental MarginContinental Margin

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Continental shelf: the submerged part of the continent between the coast and the edge of the basin.

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Continental slope: continental shelves slope gradually away from the land before dropping drastically.

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Abyssal plain:Wide, open features of the sea.

Formed of thick deposits of sediments.

Where do these sediments come from?

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Mid-Ocean ridge:Long, undersea mountain chains formed from volcanic eruptions.

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Canadian Organizations Canadian Organizations involved in Ocean involved in Ocean

ResearchResearch1.Environment Canada2.Federal Fisheries3.Ocean Science Centre4.Centre for Cold Ocean

Research (C-CORE at MUN)

Page 26: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

Ocean Currents...Ocean Currents...A large amount of ocean water that moves in a particular and unchanging direction.

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2 Types of Ocean 2 Types of Ocean Currents...Currents...

1. Surface currents Flow in the top 100-

200 m

2. Deep currents Flow below 200 m

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Surface CurrentsSurface Currents

Factors that influence surface currents are:

1.Wind2.Earth rotation3.Shape of the Earth’s continents

Page 29: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

WindWindAir movement caused by uneven heating.

The energy of the moving air is transferred by friction to the water molecules causing it to move.

Page 30: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

Earth RotationEarth RotationThe Earth spins counter-clockwise.

This spinning body deflects winds and currents depending on what side the equator they are on.

Page 31: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

This alteration of direction is called the Coriolis effect.

Clockwise in the Northern Hemisphere and Counter clockwise in the Southern Hemisphere

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Shape of ContinentShape of ContinentMoving currents are forced to turn when they meet a solid surface.

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Deep Water CurrentsDeep Water Currents

The most important influences are:

1.Water temperature2.Salinity

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Water TemperatureWater TemperatureNot the same at every depth.

*Cold water is also more dense than warmer water.

Page 35: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

SalinitySalinitySeawater is less salty at the mouths of large rivers due to the fresh water entering the ocean.

Fresh water also enters where glaciers and icebergs melt and areas of high precipitation.

Page 36: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

High amounts of evaporation increases salinity as well as freezing.

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Local Ocean Currents...Local Ocean Currents...

1. Labrador Current cold water

2. Gulf Stream warm water

Refer to map p. 54

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Waves...Waves...Large ripples set in motion by steady winds.

Waves on the surface of water are the result of a transfer of energy from moving air to the water.

Page 39: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

Common Wave Common Wave Features:Features:

*As a wave approaches a shoreline, the wavelength decreases and the wave height increases.

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Page 41: Grade 8 Science Unit 1: Water Systems on Earth Chapter 2

2 Types of Waves:2 Types of Waves:1. Swells Smooth waves

caused by wind and storms far out in the ocean.

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2. BreakersThe tumble of water when a wave collapses onshore.

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TsunamisTsunamisGiant waves that can be sent in motion by earthquakes on the ocean floor, landslides or volcanic eruptions near the shoreline.

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Can be very destructive.

November 18, 1929

South Coast of NL

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Tides...Tides...The slow rise and fall of the ocean.

The upper and lower edges of a beach are determined by the high- and low- tide mark.

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Tides are connected to the motion of the moon and the spinning of the Earth.

The moon exerts a greater force of pull than the sun due to its closer proximity to Earth.

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High Tide

Low Tide

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2 Types of Tides:2 Types of Tides:

1. Spring Tide: Occur when the

Earth, Sun and Moon are in a line.

Causes extra high and low tides.

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2. Neap Tides:Occur when the Sun and the Moon are at right angles to one another.

Causes the smallest tidal movements. There is little difference between low and high tides.

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Tidal Range:The difference in level between a high and a low tide.

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Shaping Our Shaping Our Shorelines...Shorelines...

Waves have the power to erode and deposit sediments on the shore.

Tides work with waves to determine the range of shoreline that can be affected by wave action.

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Factors that affect the interaction of waves and tides on the shorelines are:

1.Slope of the shoreline2.Shape of the shoreline3.Type of rock material4.Wave energy

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Shoreline Features...Shoreline Features...

Wave energy is concentrated on headlands and spreads out as it reaches bays.

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Sand bar or Shoal

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Think-Pair-Share...

How can coastal communities minimize the damage to shoreline property due to waves and tides?

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Shorelines can change Shorelines can change quicklyquicklyExample...Intense wave action during:

winter storms hurricanes

Etc.

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Technologies to prevent/ Technologies to prevent/ reduce the effects of reduce the effects of wave action near human wave action near human development include:development include:1. Breakwaters2. Jetties/ wharves3. Vegetation4. Sea walls5. Coastal reconfiguration