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Water and Weather. Chapter Seven: Oceans. 7.1 Introduction to Oceans 7.2 Waves 7.3 Shallow Marine Environments 7.4 The Ocean Floor. 7.3 Shallow marine environment. A beach is an area of coastal sand between the low tide line and the line of permanent vegetation. - PowerPoint PPT Presentation

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Page 1: Water and Weather
Page 2: Water and Weather

Water and Weather

Page 3: Water and Weather

Chapter Seven: Oceans

• 7.1 Introduction to Oceans

• 7.2 Waves

• 7.3 Shallow Marine Environments

• 7.4 The Ocean Floor

Page 4: Water and Weather

7.3 Shallow marine environment• A beach is an area of

coastal sand between the low tide line and the line of permanent vegetation.

• The backshore is the part of the beach above the high tide line which is only submerged during storms.

• The foreshore of a beach lies between the high and low tide lines.

Page 5: Water and Weather

7.3 Shallow marine environments

• Sea level is the average ocean height between the high and low tide levels.

Page 6: Water and Weather
Page 7: Water and Weather

7.3 Sandy beaches and tidal flats

• Sand is the most obvious feature of a beach.

• The light-colored, rounded grains slip easily through your hands.

Page 8: Water and Weather

7.3 Sandy beaches and tidal flats

• Tidal flats commonly have sandy areas, but most of a tidal flat is dark, sticky mud.

Page 9: Water and Weather

7.3 Sandy beaches and tidal flats

• Tidal flats and beaches are both covered by sediment.

• Streams and rivers carry the sediment down from the mountains and other high places.

Page 10: Water and Weather

7.3 Sandy beaches and tidal flats• Waves are the key difference

between tidal flats and beaches.

• Beaches are affected by strong wave action.

• Tidal flats are not.• Waves change the size of

sediment particles.

Scientists use special cameras to measure particles and wave action.

Page 11: Water and Weather

7.3 Waves and sand

• The largest particles of sediment are heavy enough to settle to the ocean floor.

• The smallest particles and broken grains are carried out to sea with the waves and ocean currents.

Page 12: Water and Weather

7.3 Beaches in winter and summer• Gentle summer

waves carry sand from deeper water onto the beaches.

• The stronger winter waves carry the sand back to deeper water.

Page 13: Water and Weather

7.3 Moving sand• Beaches never

completely wear away because rivers and streams bring new sand from the mountains to the beaches.

• This sand doesn’t stay in one location.

• In some places the shore resists wearing away.

Page 14: Water and Weather

7.3 Moving sand• A coast is the boundary between land and

a body of water like the ocean.

• This movement of sand along a coast is called longshore drift.

Page 15: Water and Weather

7.3 How does longshore drift work?• Longshore drift occurs because waves

approach the beach at an angle.

Page 16: Water and Weather

7.3 How does longshore drift work?• The waves come in at one direction (the upwash)

and then leave the beach at a different angle (the backwash).

Page 17: Water and Weather

7.3 Barriers and breakwaters• A breakwater is a

barrier to longshore drift that protects harbors.

• Excess sand builds up near a breakwater and must be removed regularly.

Page 18: Water and Weather

7.3 The continental shelf• Sand drifting down the steep face of a

continental shelf cuts into the shelf just like streams cut into valleys.