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Processes Shaping our Earth

Processes Shaping our Earth

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Processes Shaping our Earth. Four components of our Planet. Lithosphere Hydrosphere Atmosphere Biosphere. LITHOSPHERE. Lithosphere. Consists of the Earth’s crust and the top section of solid mantle . Brittle uppermost shell of the Earth is broken into a number of tectonic plates . - PowerPoint PPT Presentation

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Page 1: Processes Shaping our Earth

Processes Shaping our Earth

Page 2: Processes Shaping our Earth

Four components of our Planet

Lithosphere HydrosphereAtmosphere

Biosphere

Page 3: Processes Shaping our Earth

LITHOSPHERE

Page 4: Processes Shaping our Earth

Lithosphere

• Consists of the Earth’s crust and the top section of solid mantle.

• Brittle uppermost shell of the Earth is broken into a number of tectonic plates.

• The movement of the plates shape the Earth’s surface.

Page 5: Processes Shaping our Earth

Plate Tectonic Motion

• The belief is that the Earth’s lithosphere is divided into large slabs of rock known as tectonic plates.

• Earth’s continents are attached to these plates.• Scientists believe that these plates move as

solid chunks floating on top of the more plastic part of the mantle. They only move a few centimeters each year.

Page 6: Processes Shaping our Earth

PANGAEA

Page 7: Processes Shaping our Earth

What causes plate movement?

• Convection – the spread of heat through the movement of fluid substance.

• Gravity – contributes to plate movement.

• Brain Pop video over plate tectonicshttp://www.brainpop.com/science/earthsystem/platetectonics/

Page 8: Processes Shaping our Earth

Effects of Plate Tectonics

Mountain buildingSeafloor Spreading and Rift

ValleysEarthquakes and Tsunamis

Volcanoes

Page 9: Processes Shaping our Earth

Mountain Building

• When two plates, known as continental plates, slowly push into each they fold upwards, creating mountain chains.

• This process has created the Himalayan mountains.

http://www.geocraft.com/WVFossils/collision.html

Page 10: Processes Shaping our Earth

Seafloor Spreading and Rift Valleys

• As the tectonic plates move apart they cause the seafloor to spread and magma will rise up and create a ridge of mountains.

• The separation of tectonic plates can also create rift valleys – long valleys between parallel ridges of mountains.

Page 11: Processes Shaping our Earth

Earthquakes and Tsunamis• Plate movement can cause a break in the Earth’s crust

called a fault. • Plate movements can also cause vibrations known as

earthquakes. • When the rocky crust breaks it will create a fault and

sending vibrations known as seismic waves. The seismic waves are what scientist measure with a seismograph.

• When an earthquake occurs under or near the ocean it creates huge, destructive ocean waves known as tsunamis.– http://www.pep.bc.ca/tsunamis/causes_2.htm

Page 12: Processes Shaping our Earth

TSUNAMIS

Page 13: Processes Shaping our Earth

EARTHQUAKES

Page 14: Processes Shaping our Earth

Volcanoes

• A place in which tectonic plates go in different directions and sometimes one plate will dive under another and cause pressure in the Earth’s mantle.

• A volcano can create lava when the magma reaches the Earth’s surface.

• Most volcanoes and earthquakes locations match up with the plate boundaries.

Page 15: Processes Shaping our Earth
Page 16: Processes Shaping our Earth

RING OF FIRE

An area where large numbers of earthquakes and volcanic eruptions occur in the basin of the Pacific

Ocean

Page 17: Processes Shaping our Earth

Weathering, Erosion, and Deposition also affect the lithosphere.

• Weathering – the wearing down of rocks at the Earth’s surface by the actions of wind, water, ice and living things

• Erosion – process by which rock, sand, and soil are broken down and carried away. • Erosion can cut a canyon like the Grand Canyon

or carve away a region leaving valleys and lakes behind like the Great Lakes.

• Deposition – particles and sediment can be deposited and build up by the same forces that erode. For example, ocean waves can bring sand to a beach.

Page 18: Processes Shaping our Earth

Soil• Soil is a mixture of several

materials: sand, clay, rocks, water, fungi, bacteria, and decayed plants and animals.

• The type of soil affects the plant life.

• The deserts sands cannot support many forms of life.

• The soil in rainforests often lack nutrients because they are washed away.

• Soils in grassland areas and steppes or the best for farming.

Page 19: Processes Shaping our Earth

Earth’s Landforms

• Mountains – formed by collision of tectonic plates can be thousands of feet in elevation.

• Plateau – flat highland whose sides drop suddenly.

• Valleys – long, low areas between ranges of mountains, hills, or uplands. Often created by erosion, and may have a river or stream running along the bottom.

• Canyon – deep gorge or ravine between cliffs, often carved from the landscape by a river.

Page 20: Processes Shaping our Earth

HYDROSPHERE

Page 21: Processes Shaping our Earth

Hydrosphere More than 70% of the Earth’s surface is covered by water.

Water Cycle• The sun heats the surface

causing some of the surface water to evaporate.

• Water vapor condenses into clouds.

• Water returns to the oceans and land as precipitation.

• Water on land and in the ground runs off into the oceans.

• And the process repeats.

Page 22: Processes Shaping our Earth

Tides and CurrentsTIDES• Tides are caused by the gravitational pull of the moon

on Earth’s ocean waters. • High tide – a time when sea levels are at their highest.

http://www.brainpop.com/science/earthsystem/tides/

CURRENTS• The movement of the ocean’s waters. • They occur at the ocean’s surface and below. • Surface currents are caused by the spinning of the Earth

and winds.

Page 23: Processes Shaping our Earth

ATMOSPHERE AND CLIMATE

Page 24: Processes Shaping our Earth

ATMOSPHERE• The envelope of gases around the Earth• It is made up of 78% nitrogen and 21% oxygen.• It absorbs solar radiation, moderates temperatures, and

distributes water.

WEATHER• The conditions in the atmosphere closest to Earth, including

humidity, winds, and precipitation (rain, snow, or hail).

CLIMATE• The average weather conditions of a place over a long period

of time.

Page 25: Processes Shaping our Earth

Geography of Weather

• Weather is affected by latitude, elevation, wind patterns, ocean currents, and mountain barriers.

• Temperatures are usually warmer closer to the Equator.

• Temperatures are cooler in higher elevations. • Winds are based on the Earth’s spin. Depending on

the location winds can bring moist air and rain like monsoons or they can leave an area dry.

• Tropical hurricanes occur because the warm ocean water evaporates so quickly that it causes an area of low pressure.

Page 26: Processes Shaping our Earth

Seasons• The Earth tilts on its axis as it

revolves around the sun. • The tilt causes the sun’s rays to hit

the Northern hemisphere longer and more directly in summer than in winter.

• When it is summer in the northern hemisphere it is winter in the Southern hemisphere because the Southern hemisphere is tilting away from the sun and receives less direct solar rays.

• The two pole areas are very different. In the summer each pole has 24 hours of sunlight while in the winter the sun never rises in certain areas around the North and South pole.

Page 27: Processes Shaping our Earth

BIOSPHERE

Page 28: Processes Shaping our Earth

Biosphere

• Refers to all life on Earth. • Biomes – distinct geographic regions with

their own types of plant and animal life.

Page 29: Processes Shaping our Earth

Types of Biomes• Temperate Deciduous Forest

– Develop in areas with ample rain and moderate temperatures with cool winters.

– Trees change color in the fall and lose their leaves in winter.

• Tropical Rain Forest– Develop in tropical areas near

the Equator where there is ample rainfall and warm temperatures year round.

– Large trees form a canopy. – Great abundance of animal and

plant life.

Page 30: Processes Shaping our Earth

Types of Biomes• Grassland and Savanna

or Steppes– Grassland exists where

the climate is drier and there is not enough rainfall to support large amounts of trees.

– Savannas are grasslands with a few trees.

• Deserts– Regions that receive

less than 10 inches of rainfall a year.

Page 31: Processes Shaping our Earth

Types of Biomes

• Tundra– Found closer to the polar regions. The ground is

frozen most of the year.