chapter 3:the dynamic earth

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Chapter 3:The Dynamic Earth 31. The Geosphere 3.2 The Atmosphere 3.3 The Hydrosphere and Biosphere p.58-83

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Chapter 3:The Dynamic Earth. 31. The Geosphere 3.2 The Atmosphere 3.3 The Hydrosphere and Biosphere p.58-83. Key Terms. Geosphere Crust Mantle Core Lithosphere Asthenosphere Tectonic plate Erosion Atmosphere Troposphere Stratosphere Ozone. Radiation Conduction Convention - PowerPoint PPT Presentation

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Page 1: Chapter 3:The Dynamic Earth

Chapter 3:The Dynamic Earth

31. The Geosphere3.2 The Atmosphere

3.3 The Hydrosphere and Biospherep.58-83

Page 2: Chapter 3:The Dynamic Earth

Key Terms• Geosphere• Crust• Mantle• Core• Lithosphere• Asthenosphere• Tectonic plate• Erosion• Atmosphere• Troposphere• Stratosphere• Ozone

• Radiation• Conduction • Convention• Greenhouse effect• Water cycle• Evaporation• Condensation• Precipitation• Salinity• Fresh water• Biosphere• Closed system• Open system

Page 3: Chapter 3:The Dynamic Earth

3.1 The Geosphere• Describe the composition and structure of the

Earth• Describe the Earth’s tectonic plates• Explain the main cause of earthquakes and their

effects• Identify the relationship between volcanic

eruptions and climate change• Describe how wind and water alter the Earth’s

surface

Page 4: Chapter 3:The Dynamic Earth

The Earth as a SystemWhat are the conditions that allow us to survive

on a constantly changing planet?The earth is divide into 4 parts

1. Geosphere (rock)2. Atmosphere (air)3. Hydrosphere (water)4. Biosphere (living things)http://www.youtube.com/watch?v=uG3ql0vLioU

Page 5: Chapter 3:The Dynamic Earth

Geosphere• The solid part of the Earth that consists of all

rock, soils and sediments on Earth’s Surface• Most is located in interior • http://volcano.oregonstate.edu/vwdocs/vwlessons/lessons/Earths_layers/Earths_layers1.html

Page 6: Chapter 3:The Dynamic Earth

Discovering Earth’s Interior• Very difficult to study – we have only looked at 12km deep • Seismic waves to study Earth’s Interior (waves travel differently in physical

layers)Composition of Earth-

http://www.youtube.com/watch?v=_iUfi8XqEos&feature=related1. Crust- think outer layer, light elements, less than 1% of planet’s mass2. Mantle 64% mass of Earth, 2,900km thick, rock medium density, iron

rich layer3. Core densest element radius of 3,400km, hot nickel and iron center of

EarthBill Nye-

http://www.youtube.com/watch?v=MucQmSIKElU&feature=endscreen&NR=1 (23mins)

Page 7: Chapter 3:The Dynamic Earth

Composition of Earth-3 layers1. Crust- think outer layer, light elements, less

than 1% of planet’s mass, 5-8km thick beneath the oceans and 20-70km beneath the continents

2. Mantle- layer under crust, makes up 64% of mass, 2,900km thick, made of rock, medium dense

3. Core- innermost layer, densest elements, radius of 3,400 km

Page 8: Chapter 3:The Dynamic Earth

The Structure of the Earth

5 layers- http://video.about.com/geography/The-Four-Earth-Spheres.htm

1. Lithosphere2. Asthenosphere3. Mesosphere4. Outer Core5. Inner Core

Page 9: Chapter 3:The Dynamic Earth

Lithosphere- stone• 15-300 km thick• Cool rigid• Outermost layer of Earth• Crust and uppermost part of mantle• Divided into huge pieces called plate tectonic • Both continental and oceanic crust

Page 10: Chapter 3:The Dynamic Earth

Asthenosphere• 250 km thick• Solid plastic layer of mantle between the

mesosphere and the lithospehre• Made of mantle rock that flows very slowly,

allows for plates to move on top of it

Page 11: Chapter 3:The Dynamic Earth

Mesosphere• 2,550 km thick• Middle sphere• Lower layer of the mantle between the

asthenosphere and the outer core

Page 12: Chapter 3:The Dynamic Earth

Outer core• 2,200 km thick• Outer shell of Earth’s core• Made of liquid nickel and iron

Page 13: Chapter 3:The Dynamic Earth

Inner Core• 1,228 km radius• Spere of solid nickel and iron at the center of

the Earth

Page 14: Chapter 3:The Dynamic Earth

Thicknesses and density

Page 15: Chapter 3:The Dynamic Earth

Plate Tectonics• Glide across the underlying asthenosphere like ice on a pond• Continents are located on them and move with them• Pacific, North American, South American, African, Eurasian, and Antarctic

plates• Plate boundaries- this movement may cause mountains, earthquakes,

volcanoes erupt• Plate Tectonics and Mountain Building- Himalaya Mountains (Asia and

India plates collided 50mya)

• http://www.ucmp.berkeley.edu/geology/tectonics.htm• http://www.youtube.com/watch?v=1-HwPR_4mP4 (7mins)• NGO- 50minshttp://www.youtube.com/watch?v=KCSJNBMOjJs&feature=relatedBill- 23mins

https://www.youtube.com/watch?v=2hKssFQdZ0k&feature=related

Page 16: Chapter 3:The Dynamic Earth
Page 17: Chapter 3:The Dynamic Earth

Earthquakes• Fault- break in Earth’s crust preventing it from

sliding• When it breaks and creates vibrations in crusts

creates earthquakes• Occur all the time most are too small to feel• Richter scale- quantify the amount of energy

reassessed by an earthquake or its magnitude• Smallest magnitude that can be felt is 2.0• Largest recorded 9.5• Earthquakes of 7 or greater cause widespread damage

Page 18: Chapter 3:The Dynamic Earth
Page 19: Chapter 3:The Dynamic Earth

Where do they occur?• Take place at the boundaries due to the stress level• San Andreas Fault along California (N. American

plate and Pacific plate are slipping)• We cannot predict when they will occur but rather

the likely hood of where they can occur• High risk areas we build bridges and buildings

slightly flexible so they can sway when the ground moves

• http://earthquakestoday.info/

Page 20: Chapter 3:The Dynamic Earth
Page 21: Chapter 3:The Dynamic Earth

Japan's Tsunami - How it Happened 2011

• http://www.youtube.com/watch?v=24A8UwpYSs8&feature=related

Page 22: Chapter 3:The Dynamic Earth

Volcanoes• Mountains/ islands built from magma, melted

rock, that comes from the Earth’s core• Can occur on land or under the sea• Most active areas is around the pacific Ocean

plate boundaries• https://www.youtube.com/watch?v=NBPwwt0HuVo

Page 23: Chapter 3:The Dynamic Earth
Page 24: Chapter 3:The Dynamic Earth

Local Effects of Volcanic Eruptions• Loss of human life• Clouds of hot ash, dust, gases travel down at

speed of 200km/hr killing everything in its path

• Can mix with water can create a mudslide• Destroy buildings, bury crops, damage engines

of vehicles• Breathing difficulties

Page 25: Chapter 3:The Dynamic Earth

Global Effects of Volcanic EruptionsGlobal impact: https://www.youtube.com/watch?v=TghGWlVN31chttps://www.youtube.com/watch?v=k8mAtY-7n-o

• Mt St Helen- change Earth’s climate for several years• Ash and gases travel into the atmosphere reducing

sunlight decreasing global temperatures for several years

• Top 10- https://www.youtube.com/watch?v=4aYQixhdWY4&feature=fvwrel• Billl Nye• https://www.youtube.com/watch?v=gOc04z8jHaM• https://www.youtube.com/watch?v=MucQmSIKElU&feature=related (23mins)

Page 26: Chapter 3:The Dynamic Earth
Page 27: Chapter 3:The Dynamic Earth

Erosion• The removal and transport of surface material • Water Erosion- rivers create deep gorges or

oceans waves erode coastlines• Wind Erosion- area where plants are limited

(beaches and deserts) sandstone vs granite can erode more quickly

https://www.youtube.com/watch?v=G5Rp9MJJGCUBill- https://www.youtube.com/watch?v=HjVSiuj7Lxk&feature=related

Page 28: Chapter 3:The Dynamic Earth

3.2 Atmosphere• Describe the composition of the Earth’s

Atmosphere• Describe the layers of the Earth’s atmosphere• Explain 3 mechanisms of heat transfer in

Earth’s atmosphere• Explain the greenhouse effect

Page 29: Chapter 3:The Dynamic Earth

Atmosphere• Mixture of gases found in first 30km above the

Earth’s surface

Page 30: Chapter 3:The Dynamic Earth

Composition of the Atmosphere• Nitrogen 78%• Oxygen – 21%• Other -1 % (argon, carbon dioxide, methane, water

vapor)• Tiny solid particles or dust (soil, salt, ash, skin, hair

clothing, pollen, bacteria, viruses, aerosols)• Air pressure- due to the gravity, more dense closer

to earth, difficult to breath at higher elevations• http://www.youtube.com/watch?v=jmQ8FWnM0fA

Page 31: Chapter 3:The Dynamic Earth

Layers of the Atmosphere1. Troposphere2. Stratosphere3. Mesosphere4. Thermosphere

Page 32: Chapter 3:The Dynamic Earth

Troposphere-a. layer closes to the Earth’s surface to 18km aboveb. weather occurs in this layerc. densest layerd. temperature decreases as altitude increases

Page 33: Chapter 3:The Dynamic Earth

Stratosphere-• Above the troposphere• Extends from 18km to altitude of 50km• Temperatures rise as altitude increases in the

stratosphere, because the ozone absorbs the suns UV energy and warms the air

• Ozone- O3- molecule that is made up of 3 oxygen atoms

• Reduced the amount of UV that reaches the Earth

Page 34: Chapter 3:The Dynamic Earth

Mesosphere• Layer above the stratosphere• Extended to an altitude of 80km• Coldest layer as low as -93’C

Page 35: Chapter 3:The Dynamic Earth

Thermosphere• Farthest from the Earth• Nitrogen and oxygen absorb solar radiation-

temperatures have been measured above 2,000’C• Would not feel hot to us because this layer is so thin

that air particles rarely collide – little heat is transferred

• Lower level is called ionosphere – it absorbs X and gamma rays, causing the atoms to be electrically charged (ions)

• Ions can radiate energy as light- Aurora Borealis or Northern Lights (North and South poles)

Page 36: Chapter 3:The Dynamic Earth

Energy in the Atmosphere• Energy is neither created or destroyed

transferred and transformed1. Radiation- transfer of energy across a space (fire,

sunlight)2. Conduction- flow of heat from one object to

another3. Convection- air currents (hot air rises)

Page 37: Chapter 3:The Dynamic Earth

Heating of the Atmosphere• Solar energy reaches the Earth as electromagnetic

radiation, visible light, infrared radiation, UV light• Only ½ actually reaches the Earth• Most is absorbed or reflected by clouds, gases and dust• Ocean/ lakes and land radiate the energy back into the

atmosphere• 50% absorbed by Earth’s Surface• 25% scattered and reflected by clouds and air• 20% absorbed by ozone, clouds and gases• 5% reflected by Earth surface

Page 38: Chapter 3:The Dynamic Earth

The Movement of Energy in the Atmosphere

• Convection Currents- movement of the air in a circular pattern that are caused by the unequal heating of the Atmosphere

• Cold air sinks and hot air rises

Page 39: Chapter 3:The Dynamic Earth

The Greenhouse Effect• Gases trap heat near the Earth• Like heat being trapped into a car on a hot

day, the glass window would be the atmosphere

• This allows for the Earth to be warm, if it did not occur Earth would be too cold for life

3 mins- http://www.youtube.com/watch?v=ZzCA60WnoMkDiscovery Channel - Global Warming, What You Need To Know, with Tom Brokaw80mins- http://www.youtube.com/watch?v=xcVwLrAavyA&feature=related

Page 40: Chapter 3:The Dynamic Earth

3.1The Hydrosphere and Biosphere

• Name 3 major processes in the water cycle• Describe the properties of ocean water• Describe the 2 types of ocean currents• Explain how the ocean regulates Earth’s

Temperature• Discuss the factors that confine life to the

biosphere• Explain the difference between open and closed

systems

Page 41: Chapter 3:The Dynamic Earth

Hydrosphere• Makes up all of the water on the Earth’s

surface• Most is found in the oceans (3/4 globe)• Atmosphere, land and in soil

Page 42: Chapter 3:The Dynamic Earth

Hydrosphere and Water Cycle

• Water cycle- Continuous movement into ht air, land back to water– Evaporation- liquid water is heated by sun and goes

into the atmosphere– Condensation- water vapor cools and forms water

droplets– Precipitation- larger droplets fall from clouds (snow,

sleet, or hail)Bill Nye- (3mins)http://www.youtube.com/watch?v=hehXEYkDq_YRap- http://www.youtube.com/watch?v=i3NeMVBcXXU&feature=fvwrelMagic School Bus- http://www.youtube.com/watch?v=yfLTBJKnEQA

Page 43: Chapter 3:The Dynamic Earth
Page 44: Chapter 3:The Dynamic Earth

Earth’s Oceans• World Oceans- Arctic, Pacific, Atlantic, Indian• 70% of earth surface• Regulates Planet’s environment• High salt concentrations (salinity)( lower where

freshwater or rain runs into it, high in areas where evaporation is high)

• Temperature zones- surface warmed by sun, deep clod no sunlight (surface zone, thermocline- warm and cold weather)

Page 45: Chapter 3:The Dynamic Earth

Global Temperature Regulator

• Absorb and store energy from sunlight regulates temperatures in Earth’s Atmosphere

• Ocean absorbs and release more slowly than land does

• If it did not regulate temps conditions would be too extreme for life today

• Can warm land masses near by

Page 46: Chapter 3:The Dynamic Earth

Ocean Currents• Surface currents- stream like movements of

water that occur at or near the surface, wind driven and a result from global wind patterns

http://www.youtube.com/watch?v=YCorkyBe66o

• Deep currents- streamlike movements of water that flow very slowly along the ocean floor (Antarctic Bottom Water)

http://www.youtube.com/watch?v=XVZujRMGZzs

Bill Nye- http://www.youtube.com/watch?v=4_wLatK7sXghttp://www.youtube.com/watch?v=w_8mw-1HYFg

Page 47: Chapter 3:The Dynamic Earth
Page 48: Chapter 3:The Dynamic Earth
Page 49: Chapter 3:The Dynamic Earth

Fresh water• 3% of Earth’s water• Most is locked in icecaps and glaciers• Lakes, rivers, streams, ground water, wetlands,

and atmosphere• River systems- network of streams that drains

an area of land including its tributaries (small that flow into large ones)

• Mississippi River system 40%

Page 50: Chapter 3:The Dynamic Earth

Ground water• Rain and melting snow run off the land

collected into the ground• 1% of all of Earth’s Water• Aquifers- rock layer that stores and allows the

flow of ground water• Recharge zone- where water enters an aquifer

Page 51: Chapter 3:The Dynamic Earth
Page 52: Chapter 3:The Dynamic Earth

Biosphere• Part of Earth were life exists • Think layer at Earth’s surface down to the

bottom of the oceanhttp://www.youtube.com/watch?v=RmifaYcLPik&feature=related

Page 53: Chapter 3:The Dynamic Earth

Biosphere• If the Earth was an apple- it would be the skin• Uppermost part of the geosphere, most of

hydrosphere, lower part of atmosphere• 11km into the ocean and 9km into the

atmosphereLife requires:

• liquid water• Temps between 10-40’c • Source of energy

Page 54: Chapter 3:The Dynamic Earth

Energy Flow in the Biosphere• Sun light main source of energy• 4 biogeochemical cycle ( recycling of once

living organisms to be put back into the Earth’s resources)– Closed system- Earth mostly closed with respect

to matter, Eden Project– Open system- sun/ energy, energy comes in from

the sun and lost as heat