spring 2006, pflugerville isd © spring 2006, pflugerville isd, 6th grade 6th grade science

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Spring 2006, Pflugerville ISD Spring 2006, Pflugerville ISD, 6th Grade 6th Grade Science

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Spring 2006, Pflugerville ISD© Spring 2006, Pflugerville ISD, 6th Grade

6th Grade Science

Spring 2006, Pflugerville ISD

Unit 6Earth Systems and Structure

Chapter 17: The Restless EarthSection 1: Inside the EarthSection 2: Continents on the Move – Review only.Section 3: Tectonic ForcesSection 4: Building MountainsChapter 18: The Flow of Fresh WaterSection 1: The Active RiverSection 2: Stream and River DepositsSection 3: Water UndergroundChapter 19: The Earth’s AtmosphereSection 1: Characteristics of the AtmosphereSection 3: Atmospheric Pressure and Winds

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

Inside the Earth

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

How do we know what the inside of the Earth looks like?

What Do You Think?

Inside the Earth

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

Inside the Earth

The outer layer of the Earth in less dense than the inner layer.Three main layers of the Earth: crust, mantle, core. Cite: http://www.kidscosmos.org/kid-stuff/mars-trip-graphics/earth-interior-diagram.gif

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

The crust ranges from 5-100 km .Continental crust is made of light and less dense materials: silicon, oxygen and aluminum.

Oceanic crust is made of heavy and more dense materials: iron, calcium, and magnesium.

Inside the Earth

Cite: http://binky.thinkquest.nl/~ll125/images/struct.jpg

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

The mantle is between the crust and the core. It is very thick and has the most mass.

We infer what the mantle looks like by looking at the surface of the Earth. The mantle is made of iron and magnesium.

Inside the Earth

Cite: http://www.greatbasinnaturalhistory.org/Geology/Images/Mantle%20Convection.gif

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

The core begins at the bottom of the mantle and ends at the center.The core is made of iron, nickel , sulfur and oxygen.

Inside the Earth

Cite: http://www.oup.co.uk/images/oxed/children/yoes/earth/earthcore.jpg

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

When we study the Earth we look at the physical properties of its layers:

Temperature, density and ability to flow( viscosity)

Inside the Earth

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

– Lithosphere

– Asthenosphere

– Mesosphere

– Outer core

– Inner core

Inside the Earth

Cite: http://jersey.uoregon.edu/~mstrick/AskGeoMan/AskGeoImages/Earth.layers.image.gif

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

The lithosphere is the crust and the rigid upper part of the mantle.It is divided into pieces called plates.

Inside the Earth

Cite:http://www.craigtutoring.com/earthscienceimages/lithosphere.gif

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

Inside the Earth

The asthenosphere is the soft layer on which the plates move.

It is solid rock, flow very slowly.

Cite: http://www.ucmp.berkeley.edu/geology/curr2.JPG

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

Inside the Earth

The mesosphere is the strong lower part of the mantle.

Cite: http://courses.eas.ualberta.ca/eas421/images/diagrams/0108earth.gif

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

Inside the Earth

The outer core is the liquid layer that slowly circulates.

Electrical currents within it generate the Earth’s magnetic field.

Every 100,000years or so, the magnetic field reverses itself.

Cite: http://news-service.stanford.edu/news/2002/april24/gifs/earth_350.jpg

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

Inside the Earth

The inner core is a solid, dense center.

Temperature is around 4300 degrees Celsius.

Scientist know this by recreating pressures like that of the core.

Cite: http://www.phschool.com/atschool/science_activity_library/images/earths_interior.jpg

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

Earthquakes give us the answers about the earth interior through seismic waves or vibrations. They travel through the Earth at different speeds. For examples- Seismic wave through rock travels faster than through liquid.Seismographs measure the times at which different waves arrive, and record the speed.

Inside the Earth

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

Inside the Earth

Cite: http://www.thetech.org/exhibits_events/online/quakes/seismo/images/seismograph.gif

Seismograph in action

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

Click here to view the interior of the earth.

Inside the Earth

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

Build a model of the Earth using peanut butter, jelly, chocolate chips, dried milk and honey. Relate each substance to each layer of the Earth.

Inside the Earth

Activity

See speaker notes for lab.

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

Take a journey to the center of the Earth by creating a scale model of the Earth. Along the way, explore each layer and examine the characteristics of each layer.

Pre-AP Extension

See speaker notes for lab.

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

1. Explain why seismic waves travel more rapidly through the mesosphere than through the

outer core.

Let’s Review

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

Seismic waves travel more rapidly through the mesosphere because

the mesosphere is solid and densely packed, while the outer

core is liquid.

Answer

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

2. What is the difference between continental and oceanic crust?

Let’s Review

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

Oceanic crust is thinner and denser than continental crust.

Continental crust is mostly silicon, oxygen, and aluminum. Oceanic crust is rich in magnesium, iron

and calcium.

Answer

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

3. How is the lithosphere different from the asthenosphere?

Let’s Review

Chapter 17 Section 1 Spring 2006, Pflugerville ISD

The lithosphere is rigid and is divided into tectonic plates. The

asthenosphere is a layer of mantle material that flows very

slowly.

Answer

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

Tectonic Forces

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

What causes mountains to form?

What Do You Think?

Tectonic Forces

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

Stress is the amount of force per unit area put on a given object.

Deformation is the rock changing due to stress.

Three things determine how much stress a rock can handle: composition, temperature and amount of pressure.

Tectonic Forces

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

Tectonic Forces

Compression is when two plates collide. (squeezing)

Tension is when two plates pulling away from each other. (stretching)

Cite: http://www.solaster-mb.org/mb/images/dyrynda-tectonics-1-wl.GIF

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

Folding is the bending of rock

Anticline are arch-shaped folds.

Syncline are trough-shaped folds.

Monocline are rocks that have vertical stress and the ends are still horizontal.

Anticline

Tectonic Forces

Cite:http://www.salem.k12.va.us/staff/flester/lester/foldsandfaults/anticline.gif

Syncline

Cite: http://www.salem.k12.va.us/staff/flester/lester/syncline.gif

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

Monocline

Tectonic Forces

Cite: http://www.nps.gov/brca/Geodetect/Photo%20book/LF%20pix/images/Monocline%20Cross%20Section%20_TIF.jpg

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

Tectonic Forces

Cite: http://www.geosci.unc.edu/faculty/glazner/Images/Structure/Monocline.jpg

Monocline in the Mojave Desert, California

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

• Cite: http://www-class.unl.edu/geol101i/images/structure%20images/anticline%20from%20Wind%20Rivers.jpg

Anticline in Wind Rivers, Wyoming

Tectonic Forces

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

Tectonic Forces

Cite: http://users.ipfw.edu/isiorho/Syncline.JPG

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

Faulting is breaking of rocks

Footwall is one side of the rock.

Hanging wall is the other side of the rock.

A normal fault is when the rocks pull away from each other, the hanging wall moves down.

A reverse fault is when rocks are pushed together, the hanging wall is pushed up.

Tectonic Forces

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

Normal Fault

Tectonic Forces

Cite: http://www.calstatela.edu/faculty/acolvil/struct/normal_animation.gif

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

Reverse Fault

Tectonic Forces

Cite: http://www.earthsci.org/struct/fault/reverse.gif

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

Strike-slip Fault is when the rock breaks and move horizontally.

Tectonic Forces

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

Tectonic Forces

Strike Slip Fault

Cite: http://darkwing.uoregon.edu/~nfay/home/right_lateral_fault.gif

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

Using play dough, model the layers of the Earth and see what happens when the plates move.

Tectonic Forces

Activity

See speaker notes for lab.

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

1. Name tow types of stress, and describe how they affect the

Earth’s surface.

Let’s Review

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

Compression squeezes the crust together and forms folds and

reverse faults. Tension pulls the crust apart and forms mid-ocean

ridges and normal faults.

Answer

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

2. What is the difference between a normal fault and a reverse fault?

Let’s Review

Chapter 17 Section 3 Spring 2006, Pflugerville ISD

A normal fault forms as a result of tensional stress and the hanging wall moves down relative to the footwall. A reverse fault forms as a result of

compressional stress, and the hanging wall moves up relative to the

footwall.

Answer

Chapter 17 Section 4 Spring 2006, Pflugerville ISD

Building Mountains

Chapter 17 Section 4 Spring 2006, Pflugerville ISD

Why are the Appalachian Mountains in the middle of the North American

plate?

What Do You Think?

Building Mountains

Chapter 17 Section 4 Spring 2006, Pflugerville ISD

Most mountain ranges form where plates collide- convergent boundary.

Uplift is the process by which regions of the crust are raised to a higher elevation.

Building Mountains

Chapter 17 Section 4 Spring 2006, Pflugerville ISD

Building Mountains

Cite: http://www.calstatela.edu/faculty/acolvil/plates/subduction.jpg

Chapter 17 Section 4 Spring 2006, Pflugerville ISD

Folded Mountains are formed when rock layers are squeezed together. Appalachians

Fault - Block Mountains are formed when faulting causes large blocks of the crust to drop down. Tetons

Volcanic Mountains are formed when molten rocks erupts onto the Earth’s surface. Divergent boundary.

Building Mountains

Chapter 17 Section 4 Spring 2006, Pflugerville ISD

Building Mountains

Fault Block Mountains

Citehttp://cse.cosm.sc.edu/erth_sci/Metamorf/ue3588.jpg:

Chapter 17 Section 4 Spring 2006, Pflugerville ISD

Cite: http://cse.cosm.sc.edu/erth_sci/Metamorf/ue1868.jpg

Building Mountains

Folded Mountains in Canada

Chapter 17 Section 4 Spring 2006, Pflugerville ISD

Volcanic Mountain

Building Mountains

Cithttp://cse.cosm.sc.edu/erth_sci/Metamorf/ss5_3.jpge:

Chapter 17 Section 4 Spring 2006, Pflugerville ISD

You are going to research a mountain and find a photograph of the mountain. We will place all the different mountains around the room and you will tour the museum.

Building Mountains

Activity

See speaker notes for lab.

Chapter 17 Section 4 Spring 2006, Pflugerville ISD

It can takes millions of years for a mountain to form or sometimes just a few years. Research a mountain and create a timeline on the formation of the mountain.

Pre-AP Extension

See speaker notes for lab.

Chapter 17 Section 4 Spring 2006, Pflugerville ISD

1. Name and describe the type of tectonic stress that forms folded

mountains.

Let’s Review

Chapter 17 Section 4 Spring 2006, Pflugerville ISD

Folded mountains form when compression pushes layers of

rock into huge folds.

Answer

Chapter 17 Section 4 Spring 2006, Pflugerville ISD

2. Name and describe the type of tectonic stress that forms fault-

block mountains.

Let’s Review

Chapter 17 Section 4 Spring 2006, Pflugerville ISD

Fault-block mountains form when tension pulls rock apart and

causes a large number of normal faults to form.

Answer

Chapter 17 Section 4 Spring 2006, Pflugerville ISD

3. Explain how volcanic mountains change the surface of the Earth.

Let’s Review

Chapter 17 Section 4 Spring 2006, Pflugerville ISD

Volcanic mountains change the surface of the Earth by adding

material to it.

Answer

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

The Active River

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

What are the parts to the water cycle?

What Do You Think?

The Active River

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

The Active River

Erosion is the removal and transport of rock and soil by the flow of water and by the action of wind , ice and gravity.

Cite:http://www.fotos-und-grafik.de/fichtel/natur/erosion/erosion.jpg

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

The water cycle is a continuous movement of water.Parts of the water cycle are:1. Condensation is when water vapors cool and change into liquid water droplets that form clouds.2. Precipitation is rain, snow, sleet or hail that falls from the clouds to the Earth’s surface.

The Active River

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

3. Evaporation takes place when liquid water from the Earth’s surface changes into water vapor. Energy from the sun causes evaporation.

4. Water vapor is also added to the air by plants (transpiration).

Water gains energy during evaporation- endothermic.

Water loses energy during condensation- exothermic.

The Active River

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

Cite: http://www.tkp.edu.hk/~lscn/6a/hydrologic_cycle.gif

Hydrological Cycle

The Active River

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

Runoff is water that flows across the land and enters rivers and streams. It eventually flows into lakes and oceans.Percolation is the downward movement of water through soil and rock due to gravity.Tributaries are smaller streams or rivers that flow into larger ones.

The Active River

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

A watershed is the region of land drained by a river system. Mississippi Watershed is the largest in U.S.

Divides separated the watersheds.

A channel is the path that a stream follows.

Gradient is the measure of the change in elevation over a certain distance.

The Active River

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

The Active River

Click here to watch a short video on watersheds.

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

The Active River

Discharge is the amount of water that a stream or river carries in a given amount of time.

Load is the materials carried by a river or stream.

Cite: http://www.ecy.wa.gov/programs/wq/images/yak_wq_images/dirty_ri.jpg

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

Young- erodes channels deep, river flows quickly and is straight.Mature- erodes wider, meanders, gradient not as steep as young river and has more tributaries and discharge.Old- has little gradient and little erosion. Oxbow lakes and large amount of meanders.Rejuvenated- land is raised due to plate tectonics and river becomes steeper.

The Active River

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

Get some pictures of different rivers and see if the students can figure out the age of the rivers based on the characteristics of each river.

The Active River

Activity

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

The Active River

Explore a river system by clicking here.

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

You will make a model of the water cycle, and you will watch water as it moves through the model.

The Active River

Activity

See speaker notes for lab.

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

1. Explain the interactions between matter and energy in the water

cycle.

Let’s Review

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

Liquid water gains energy form the sun and evaporates. As water

evaporates, it changes into water vapor. Water vapor rises and

condenses to form clouds. As the water vapor condenses, it loses

energy, and water falls back to the Earth as precipitation.

Answer

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

2. Describe the differences between a river system and a

watershed.

Let’s Review

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

A river system is a network of streams and rivers. A watershed is the region of land drained by a river system. River systems are

mad up of smaller systems of streams and tributaries.

Answer

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

3. Describe the ways that youthful, mature, old, and rejuvenated

rivers shape the Earth’s surface.

Let’s Review

Chapter 18 Section 1 Spring 2006, Pflugerville ISD

Youthful rivers erode deep channels. Mature rivers erode wide channels. Old rivers deposit sediment in their channels and along their banks.

Rejuvenated rivers form terraces in the river valley.

Answer

Chapter 18 Section 2 Spring 2006, Pflugerville ISD

Stream and River Deposits

Chapter 18 Section 2 Spring 2006, Pflugerville ISD

Why are some farms located near a river?

What Do You Think?

Stream and River Deposits

Chapter 18 Section 2 Spring 2006, Pflugerville ISD

Rivers erode and carry enormous amounts of sediment.

When the river’s current slows down the sediment is deposited.

Deposition is the process by which material is dropped.

Stream and River Deposits

Chapter 18 Section 2 Spring 2006, Pflugerville ISD

Stream and River Deposits

Cite:http://www.rcgroups.com/gallery/data/512/10591CO_River_1-19-03__4_.jpg

Deposition happens along the insideof the bank , where the current is slower.

Erosion happens on the outsidebank, where the current is faster.

Chapter 18 Section 2 Spring 2006, Pflugerville ISD

A delta is formed where a river’s current slows down and sediment is deposited in a fan- shaped pattern. New land is built.An alluvial fan is created when fast moving water flows onto a flat plain and sediment is deposited in a fan-shaped pattern. A flood plain is when a river overflows its banks.

Stream and River Deposits

Chapter 18 Section 2 Spring 2006, Pflugerville ISD

Stream and River Deposits

Delta

Alluvial Fan

Flood Plains

Cite: http://www.windows.ucar.edu/earth/geology/images/alluvial_fan_lg.jpeg

Cite: http://www.lizander.com/workforsale/images/patterns_river_delta.jpg

Cite: http://www.wildlife-art.co.uk/new_site/graphics/earth_science/flood_plain.jpg

Chapter 18 Section 2 Spring 2006, Pflugerville ISD

1. Describe how river deposition forms deltas, alluvial fans, and

flood plains.

Let’s Review

Chapter 18 Section 2 Spring 2006, Pflugerville ISD

Answer

A delta is formed where a river’s current slows down and sediment is deposited in a fan- shaped pattern. New land is built.An alluvial fan is created when fast moving water flows onto a flat plain and sediment is deposited in a fan-shaped pattern. A flood plain is when a river overflows its banks.

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Water Underground

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Where does the water go after it rains?

What Do You Think?

Water Underground

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Ground water is water that is beneath the Earth’s surface.

97% of the world’s liquid fresh water is stored here.

There are two zones underground:

1. Zone of aeration

2. Zone of saturation.

Water Underground

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Zone of Aeration is the upper zone where rain water passes.

Zone of Saturation is where water collects.

Where these two zones meet is at the water table.

Water table rises during wet years and lowers during dry years.

Water Underground

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Water Underground

Citehttp://www.geo.sunysb.edu/classes/oldclasses/cei542/notes/watertable.jpg:

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

An aquifer is a rock layer that stores ground water and allows it to flow.

Porosity is the amount of space between the particles that make up a rock.

Aquifers allow water to pass freely from one pore to another.

Permeability is a rock’s ability to allow water to pass through it.

Water Underground

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Water Underground

Cite: http://www.dac.neu.edu/Earth/m.wizevich/GEO200/Week11/Porosity1.gif

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Cite:http://www.rw.ttu.edu/2302_butler/images/permeability.jpg

Water Underground

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Which substance has more permeability sand or soil? Find out how long it takes for water to travel through each of these substances.

Water Underground

Activity

See speaker notes for lab.

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Best aquifers usually form in permeable materials such as sandstone, limestone, and layers of sand and gravel.

Recharge zone is the ground surface where water enters an aquifer. (marked by signs).

The size of the recharge zone depends on the layer of rock.

Water Underground

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Water Underground

Cite: http://pasture.ecn.purdue.edu/~epados/ground/images/recharge.gif

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Ground water movement depends on the slope of the water table.

If the water table reaches the Earth’s surface, water will flow out from the ground and form a spring.

A well is a human-made hole that is deeper than the level of the water table. Water is filtered and purified as it travels through an aquifer.

Water Underground

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Water Underground

Cite: http://www.artesianwater.com/kids/Aquifer.jpg

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Most caves are formed as ground water dissolves the limestone.

Stalactites are sharp- icicle shaped features that are from deposits of calcium carbonate.( Hang from the ceiling)

Stalagmites form when water falls to the cave floor adds to cone- shaped features.

Drip stone column are stalagmites and stalactites connected.

Water Underground

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Stalagmites

Stalactites

Dripstone Column

Water Underground

Cite: http://www.epidauros.freeserve.co.uk/slovenia/4stalagmites.jpg

Cite: http://www.sisutcliffe.co.uk/pix/spain_dec_03/stalagtites.jpg

Cite:http://www.suite101.com/files/articles/93000/93687/carlsbad_column1.jpg

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

View maps of major and minor aquifers of Texas by clicking here.

Water Underground

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Porosity and permeability are related terms used to describe any rock or loose sediment. Both of these properties are essential to the formation of an aquifer. Describe the porosity and permeability in sand, gravel and clay.

Pre-AP Extension

See speaker notes for lab.

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

1. What is the source of the water in an aquifer?

Let’s Review

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Surface water percolates down through the recharge zone to

supply water to an aquifer.

Answer

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

2. What are some of the features formed by underground erosion

and deposition?

Let’s Review

Chapter 18 Section 3 Spring 2006, Pflugerville ISD

Caves form by ground-water erosion. Stalagmites, stalactites, and dripstone columns form by

underground deposition.

Answer

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

Characteristics of the Atmosphere

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

Why is the atmosphere so important to the Earth?

What Do You Think?

Characteristics of the Atmosphere

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

Atmosphere is a mixture of gases that surround the Earth.

Protects you from the sun and

has oxygen.

Characteristics of the Atmosphere

Cite: http://www.wsd1.org/PC_Science/Weather/atmosphere.jpg

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

Characteristics of the Atmosphere

The atmosphere is made up of gases, solids and liquids.

Water is most common liquid in the atmosphere.

Cite: http://www.birdlife.org.za/resources/sustainable/Air/atmosphere_bird.jpg

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

Air pressure is the measurement of the force with which air particles push on a surface.

Characteristics of the Atmosphere

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

The atmosphere is held around the Earth by gravity.The gas particles are pulled towards the surface.There are fewer particles as you move away from the surface.

Characteristics of the Atmosphere

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

Altitude is the height of an object above the Earth’s surface.

As altitude increases, air pressure decreases.

Characteristics of the Atmosphere

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

Temperature changes as you move through the atmosphere due to the amount of sun’s energy that is absorbed by gases.

Characteristics of the Atmosphere

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

Characteristics of the Atmosphere

Cite:http://www.noaanews.noaa.gov/stories/images/atmosphere-regions.jpg

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

Characteristics of the Atmosphere

Troposphere makes up 90% of the mass of atmosphere.

It is the densest layer and the layer in which you live.

Cite: http://www.weatherquestions.com/troposphere.jpg

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

Characteristics of the Atmosphere

Stratosphere is above the troposphere

The air is very thin here and there is very little moisture.

The ozone is here that absorbs some of the sun’s harmful rays.

Temperature increases with altitude here.

Cite: http://www.policyalmanac.org/graphics/chartsn.gif

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

The mesosphere is above the stratosphere

It is the coldest layer and protects us from meteoroids. It burns up any substance that enters our atmosphere.

Characteristics of the Atmosphere

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

Thermosphere is a hot layer yet is doesn’t feel hot-because the particles move fast but are far apart.

Characteristics of the Atmosphere

Cite: http://www.spaceflightnow.com/delta/d289/images/timed.jpg

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

Characteristics of the Atmosphere

Ionosphere is the upper part of mesosphere and lower part of Ionosphere. This layer absorbs the sun rays, and the gas particles become electrically charged.

Cite:http://www.oma.be/BIRA-IASB/Public/Images/aurora2.gif

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

Use a scale to find the mass of a ball. Record the mass of the empty ball. Pump up the ball. Use a scale to find the mass of the ball filled with air. Compare the two masses. Does air have mass.

Characteristics of the Atmosphere

Activity

See speaker notes for lab.

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

Review the layers of the atmosphere by clicking here.

Characteristics of the Atmosphere

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

Some scientist believe the Earth is warming up due to the greenhouse effect.

Measure temperatures in a model greenhouse and in a control as they are heated. Calculate the resulting temperature changes.

Pre-AP Extension

See speaker notes for lab.

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

1. What cause air pressure?

Let’s Review

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

Air pressure is caused by gravity pulling molecules in the atmosphere

toward the Earth.

Answer

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

2. How can the thermosphere have high temperature but not feel hot?

Let’s Review

Chapter 19 Section 1 Spring 2006, Pflugerville ISD

In the thermosphere, particles are moving quickly, but because they are

few and far apart, they cannot transfer much energy.

Answer

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

Atmospheric Pressure and Winds

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

What causes the wind to blow?

What Do You Think?

Atmospheric Pressure and Winds

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

Wind is the movement of air as a result of different air pressures.

The greater the pressure difference, the stronger the wind.

Wind is caused by unequal heating of the Earth.

Atmospheric Pressure and Winds

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

The unequal heating of the Earth makes pressure belts. The air rises or sinks making circular patterns on the Earth. These patterns are called convection cells.

Atmospheric Pressure and Winds

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

Cite: http://www.eeb.uconn.edu/courses/eeb244/EEB244S02/Aphys4.gif

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

The way the wind blows depends on the rotation of the Earth.

The wind blows in a curved path due to the rotation of the Earth called the coriolis effect.

Atmospheric Pressure and Winds

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

Cite: http://www.students.i.csbsju.edu/ijflenner/coriolis_effect.gif

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

Winds in the Northern Hemisphere curve to the right.

Winds in the Southern Hemisphere curve to the left.

Atmospheric Pressure and Winds

Cite: http://www-nsidc.colorado.edu/arcticmet/images/factors/coriolis.gif

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

Cyclones are areas of low pressure. There is warm, less dense air at the center that rises.

Anticyclones are areas of high pressure. There is colder, denser air at the center that sinks.

Atmospheric Pressure and Winds

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

Atmospheric Pressure and Winds

Cite: http://rst.gsfc.nasa.gov/Sect14/3_cyclones.jpg

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

Local winds generally move short distances and can blow from any direction.Global winds are part of a pattern of air flow that moves across the Earth.

Atmospheric Pressure and Winds

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

Trade winds blow at 30* latitude to the equator. (early sailors used the winds to sail from Europe to America).

Doldrums are around the equator where there is very little wind. (means foolish)

Horse Latitudes- are at 30*North and 30* south latitudes. Air sinks and there is very little air.

Atmospheric Pressure and Winds

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

Westerlies are between 30* and 60* latitude. Flows towards the poles and helped ships return to Europe.

Polar Easterlies are between the poles and 60* latitude and is where cold air sinks.

Atmospheric Pressure and Winds

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

Atmospheric Pressure and Winds

Cite: http://www.esys.org/wetter/doldrums6.jpg

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

Jet stream is a narrow belt of high-speed winds that blow in the upper troposphere and lower stratosphere. The jet stream controls how storms move.

Atmospheric Pressure and Winds

Cite: http://www.fishusa.com/FishErie/Captain/images/adams-jet-stream.jpg

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

Fill a large, clear plastic container with cold water. Tie the end of a string around the neck of a small bottle.Fill the small bottle with hot water. Add a few drops of red food coloring until the water has changed color.Without tipping the small bottle, lower it into the plastic container until it touches the bottom of the container. Observe what happens.

Activity

See speaker notes for lab.

Atmospheric Pressure and Winds

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

Explore the movement of the jet stream by

clicking here.

Atmospheric Pressure and Winds

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

1. How does the Coriolis effect affect the way wind moves?

Let’s Review

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

The Coriolis effect prevents winds from blowing in a straight path. Because of the Coriolis effect,

winds in the Northern Hemisphere curve to the right and winds in the

Southern Hemisphere curve to the left.

Answer

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

2. How do winds affect the weather?

Let’s Review

Chapter 19 Section 3 Spring 2006, Pflugerville ISD

The warm, rising air in a low pressure area brings clouds and rain. The cool, sinking air in a high pressure area brings dry,

clear weather.

Answer