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Our Physical World Cluster One – Unit Two

Our Physical World

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Our Physical World. Cluster One – Unit Two. The Northern Hemisphere is from the equator to the North Pole. The Southern Hemisphere is from the equator to the South Pole. The western hemisphere is from the Prime Meridian west to the International Date Line. - PowerPoint PPT Presentation

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Page 1: Our Physical World

Our Physical WorldCluster One – Unit Two

Page 2: Our Physical World

The Northern Hemisphere is from the equator to the North Pole.

The Southern Hemisphere is from the equator to the South Pole.

Page 3: Our Physical World

The western hemisphere is from the Prime Meridian west to the International Date Line.

The eastern hemisphere is from the Prime Meridian east to the International Date Line.

Page 4: Our Physical World

The Atmosphere Is a gaseous layer that surrounds the

earth.

Critical for the survival of all life.

Made up of nitrogen and oxygen. It is the air that we breathe.

Page 5: Our Physical World

The Lithosphere The outer rocky shell of the earth.

In some areas this surface is exposed, in others it is under water.

We live on the exposed lithosphere.

Page 6: Our Physical World

The Hydrosphere The water surface of the earth.

Includes oceans and seas.

The Cryosphere is the area that is frozen and includes frozen seas and glaciers.

Page 7: Our Physical World

The Biosphere The thin layer of earth containing all

living organisms.

These life forms depend on the other spheres.

Page 8: Our Physical World

The Spheres Atmos – means air

Litho - means rock

Hydro – means water

Cryo – means frozen

Bio - means likfe

Page 9: Our Physical World

Atmosphere

BiosphereHydrosphere

Lithosphere

The spheres are all

interconnected

Page 10: Our Physical World

The Natural Environment

Refers to the 4 spheres except for the human part of the biosphere.

Made up of land surface, soils, atmosphere, oceans, plants, and animals.

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Land and Water Most of the water of the earth is found

in the 4 major oceans.

71% of the earth is covered with water.

29% of the earth is land.

Page 12: Our Physical World

Oceans Pacific Ocean is the largest. It covers

31% of the earths surface.

The Atlantic Ocean is the next largest. It covers 15% of the earth’s surface.

There are more islands in the Pacific than the Atlantic.

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The Indian Ocean is slightly smaller than the Atlantic and covers 13% of the earth.

The Arctic Ocean is the smallest and much of this ocean has a frozen surface.

Page 14: Our Physical World

Continents 29% of the earth’s surface is land.

There are 6 major landmasses.

They are: North America, South America, Africa, Eurasia, Antarctica, Australia.

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LandForms There are 4 major types of landforms.

1) Mountains2) Hills3) Plateaus4) Plains

The earth’s surface is always shifting and changing.

Page 16: Our Physical World

Mountains Irregular surfaces at high elevations.

Mountains in humid regions are usually rounded.

Those is arid regions are more pointy.

Page 17: Our Physical World

Hills Similar to, but, lower than mountains.

Page 18: Our Physical World

Plateaus Are large, flat areas at higher

elevations than the surrounding land.

Usually located within montainous or hilly regions and are often drained by rivers and run through deep canyons.

Page 19: Our Physical World

Plains Extensive regions that are flat and

often treeless.

They are drained by rivers that run through shallow valleys.

Page 20: Our Physical World

Landforms by Continent

Eurasia

Mountain ranges including the Himalayas, Alps and Pyrenees.

Northern Eurasia has the largest continuous lowland which includes the Siberian Lowland.

Page 21: Our Physical World

Africa Much of Africa is a plateau at 1,000

meters above sea level.

The principal mountain range runs north-south on the eastern side of the continent.

Also is largely desert. (Sahara)

Page 22: Our Physical World

North America Mountains in the west (Rocky

Mountains)

Mountains in the east (Appalacians)

Between them is lowland plains.

Page 23: Our Physical World

South America Mountains in the west (The Andes)

Brazilian Highlands in the east.

Between them are a series of plateaus, plains and river valleys.

Page 24: Our Physical World

Antarctica Completely covered in ice.

Has mountain ranges.

Page 25: Our Physical World

Australia Mountain Range = Great Dividing

Range

Most of continent is a series of dry plains and plateaus.

Page 26: Our Physical World

Rivers People almost always live by rivers.

There are 6 reasons people are attracted to rivers...

Page 27: Our Physical World

1) Rivers provide protein-rich food (fish)

2) River valleys provide soils suitable for farming.

3) Rivers provide easy movement of people and goods.

4) Rivers provide opportunities to generate power from hydroelectric dams.

5) Rivers are often favored as locations for recreational activities.

6) Rivers and their valleys provide the best route through wooded areas.

Page 28: Our Physical World

Climate Climate is the long term balance of

temperature, precipitation, wind and cloud cover.

Page 29: Our Physical World

Weather The short term condition of the

atmosphere and can change in a couple of minutes and from one day to the next.

Page 30: Our Physical World

Climate of an Area 3 main factors combine to determine

the climate of an area:

1) Latitude2) Air Masses3) Low and High Pressure Zones

Page 31: Our Physical World

Climate Zones A climate zone is a combination of the

3 main factors that contribute to an areas climate.

Page 32: Our Physical World

Climate Zones There are 5 climate zones in the world.

1) Humid-equatorial2) Dry3) Humid-Temperate4) Humid-Cold5) Cold-Polar

Page 33: Our Physical World

In each climate zone, there are 5 factors that affect it:

Page 34: Our Physical World

Ocean Currents Currents distribute heat throughout the

earth.

Page 35: Our Physical World

Prevailing Winds Wind moves moisture and temperature

from one place to another.

Prevailing winds are general wind patterns, much the same as ocean currents.

Page 36: Our Physical World

Mountain Barriers Mountains block prevailing winds.

Moisture in the air hits the mountain slope, and, because cool air cannot hold as much water, the moisture falls as precipitation.

This leaves the other side of the mountain very dry because it always rains on the other side of the mountain.

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Page 38: Our Physical World

Altitude The altitude of mountains has an effect

on climate because air that is high up is cooler and dryer than air that is closer to sea level.

Page 39: Our Physical World

Distribution of Land and Sea

Water absorbs heat more slowly than land, so, the climate of land close to water is moderated by the water.

The water keeps the land cooler during the summer and warmer in the winter.

Page 40: Our Physical World

Environmental Regions Climate determines soils and

vegetation.

Geographers combine climate, soils, and vegetation physical characteristics to identify environmental regions.

Page 41: Our Physical World

Temperate Forests- Located in Europe and eastern North America.

-Naturally forested and have fertile soil.

- Today, these are agricultural or urban with high population density.

Page 42: Our Physical World

Temperate Grasslands

-Located in continental interiors.

-Examples include: Canadian Prairies, Russian steppes and Argentinean pampas.

-There is too little precipitation for trees, but, the soil is good for growing grain and there are clearly defined seasons.

-These regions have medium population density.

Page 43: Our Physical World

Mediterranean Forests-Located on the western side of a continent in a temperate latitude.

-Summers are hot and dry, and winters are warm and moist.

-Naturally forested, these areas are usually agricultural and have medium population density.

Page 44: Our Physical World

Tropical Rainforests-Close to the equator.

-High rainfall, and dense vegetation.

-The soil is poor for agriculture and the population density is low.

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Boreal Forests-Only found in the Northern Hemisphere.

-Long cold winters, and short, warm summers.

-Low precipitation, little agriculture, and low population density.

-Good source of forest products and minerals.

Page 46: Our Physical World