wave erosion and marine geology

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Wave Erosion and Marine Geology How waves behave How the sea modifies coastlines

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Wave Erosion and Marine Geology . How waves behave How the sea modifies coastlines. Waves. Essential Points. Waves are created by the wind Water in waves oscillates but does not move with the wave What happens when waves hit the shore Storm surges can be catastrophic. Wave Fetch. - PowerPoint PPT Presentation

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Page 1: Wave Erosion and Marine Geology

Wave Erosion and Marine Geology

How waves behaveHow the sea modifies coastlines

Page 2: Wave Erosion and Marine Geology

Waves

Page 3: Wave Erosion and Marine Geology

Essential Points1. Waves are created by the wind2. Water in waves oscillates but does not

move with the wave3. What happens when waves hit the shore4. Storm surges can be catastrophic

How Waves Behave

Page 4: Wave Erosion and Marine Geology

Wave Fetch

Page 5: Wave Erosion and Marine Geology

Wave Fetch

Page 6: Wave Erosion and Marine Geology

The Highest Recorded Ocean Wave

1. Waves are created by the wind

Page 7: Wave Erosion and Marine Geology

Global Wave Heights

1. Waves are created by the wind

Page 8: Wave Erosion and Marine Geology

Freak Waves • Addition of waves of different frequencies

• Theoretically could reach 200 feet in Gulf of Alaska

• One nearly sank the Queen Mary in WWII, with 15,000 troops aboard.

1. Waves are created by the wind

Page 9: Wave Erosion and Marine Geology

Wave Motions

• Particles in a wave travel circular paths• The water in a deep-water wave does not

move forward• Below wave base, wave effects are negligible

2. Water in a wave oscillates but does not move with the wave

Page 10: Wave Erosion and Marine Geology

Wave Motions

2. Water in a wave oscillates but does not move with the wave

Page 11: Wave Erosion and Marine Geology

When Waves Meet the Shore

When the bottom interferes with wave motion, the wave steepens and the top overtakes the bottom.

3. What happens when waves hit the shore

Page 12: Wave Erosion and Marine Geology

Wave Refraction

• Waves change path when they reach shallow water• Wave energy is concentrated on headlands and

spread out in bays

3. What happens when waves hit the shore

Page 13: Wave Erosion and Marine Geology

Wave Refraction off Cape Cod

3. What happens when waves hit the shore

Page 14: Wave Erosion and Marine Geology

Rips

• When waves break parallel to a beach, rips occur

3. What happens when waves hit the shore

Page 15: Wave Erosion and Marine Geology

Rips, Lake Superior

Page 16: Wave Erosion and Marine Geology

Oblique Rips

3. What happens when waves hit the shore

Page 17: Wave Erosion and Marine Geology

Storm Waves: Galveston, Texas, September 8, 1900:

• 6000-8000 dead• 3600 houses destroyed

4. Storm surges can be catastrophic

Page 18: Wave Erosion and Marine Geology

Raising Galveston – 6 in. to 17 ft.

Page 19: Wave Erosion and Marine Geology

“A rickety maze such as Dr. Seuss might have drawn”

Page 20: Wave Erosion and Marine Geology

The Lift in Progress

Page 21: Wave Erosion and Marine Geology

Pumping in the Sand

4. Storm surges can be catastrophic

Page 22: Wave Erosion and Marine Geology

The Galveston Seawall

4. Storm surges can be catastrophic

Page 23: Wave Erosion and Marine Geology

Essential Points1. Waves are created by the wind2. Water in waves oscillates but does not

move with the wave3. What happens when waves hit the shore4. Storm surges can be catastrophic

How Waves Behave

Page 24: Wave Erosion and Marine Geology

How the sea modifies coastlines

Page 25: Wave Erosion and Marine Geology

Essential Points1. Wave Action erodes or deposits material

along coastlines2. Types of coastline3. Deltas are governed by deposition, waves,

and tides4. Reefs are a special type of coastline in

tropical regions5. Global sea level is affected by ice ages and

plate tectonics

How the sea modifies coastlines

Page 26: Wave Erosion and Marine Geology

In the long run, nothing is as futile as trying to resist shoreline

change.

Change can be resisted for a while, but when the water wants

something badly enough, it will come in and take it.

1. Wave Action erodes or deposits material along coastlines

Page 27: Wave Erosion and Marine Geology

Property Values and Shoreline Erosion

• If more than half the original lot is left, it’s Location, Location, Location

• After that, it becomes obvious there soon won’t be any location left

1. Wave Action erodes or deposits material along coastlines

Page 28: Wave Erosion and Marine Geology

Marine Erosion

• Chemical Attack • Abrasion • Wave Impact • Compressed Air • Backwash

1. Wave Action erodes or deposits material along coastlines

Page 29: Wave Erosion and Marine Geology

Water Velocity and Erosion

1. Wave Action erodes or deposits material along coastlines

Page 30: Wave Erosion and Marine Geology

Longshore and Beach

Drift

• Most Beach Sand Is Created by Weathering and Carried to Coasts by Rivers

• Beach Sand Moves along the Coast by Longshore and Beach Drift

1. Wave Action erodes or deposits material along coastlines

Page 31: Wave Erosion and Marine Geology

Beach Drift, New Jersey

Page 32: Wave Erosion and Marine Geology

Types of CoastDegree of Modification• Primary - Not Modified Much by Wave Action• Secondary - Highly Modified by Wave Action History• Emergent - Land Rises or Water Level Falls• Submergent - Land Sinks or Water Level Rises Dominant Process• Erosional• Depositional

2. Types of coastline

Page 33: Wave Erosion and Marine Geology

Effects of the Pleistocene

• Sea level has risen at least 100 meters in the last 18,000 years

• Most coastlines globally are submergent• Primary coastlines are very common

2. Types of coastline

Page 34: Wave Erosion and Marine Geology

Secondary Coasts Are Modified by Marine Erosion or Deposition

Page 35: Wave Erosion and Marine Geology

Secondary CoastsErosion• Stack • Terraces • Tombolo • Erosion rate becomes very

slow – wave energy dissipated

crossing the wave-cut terrace. – Cliffs become higher, meaning

more material to move.

Deposition• Spit • Lagoon • Baymouth Bar • Barrier Bar

2. Types of coastline

Page 36: Wave Erosion and Marine Geology

Primary Coastlines Are Very Common

• Drowned River Valleys (Estuaries)

• Drowned Glacial Valleys (Fiords)

2. Types of coastline

Page 37: Wave Erosion and Marine Geology

Estuaries, Chesapeake Bay

Page 38: Wave Erosion and Marine Geology

Tidal Marshes,

Chesapeake Bay

2. Types of coastline

Page 39: Wave Erosion and Marine Geology

Fiord Coast, Labrador

Page 40: Wave Erosion and Marine Geology

Other Ways Primary Coasts Can Form

• Deltas • Volcanic Activity • Uplift

2. Types of coastline

Page 41: Wave Erosion and Marine Geology

Primary and Secondary Coastlines

2. Types of coastline

Page 42: Wave Erosion and Marine Geology

Baymouth Bar, Michigan

Page 43: Wave Erosion and Marine Geology

Wave-Cut Platform, California

Footer

Page 44: Wave Erosion and Marine Geology

Coastal Terraces, California

Page 45: Wave Erosion and Marine Geology

Sea Stacks, Washington

Page 46: Wave Erosion and Marine Geology

Former Stack, Michigan

Page 47: Wave Erosion and Marine Geology

Sea Caves, Apostle Islands

Page 48: Wave Erosion and Marine Geology

Wave-Cut Arch, Lake Superior

Page 49: Wave Erosion and Marine Geology

Delta Coasts

• Deposition-Dominated• Wave Dominated• Tide-Dominated

3. Deltas are governed by deposition, waves, and tides

Page 50: Wave Erosion and Marine Geology

The Mississippi – A Deposition-Dominated Delta

3. Deltas are governed by deposition, waves, and tides

Page 51: Wave Erosion and Marine Geology

Yukon and Nile Deltas – Balance of Deposition and Wave Action

3. Deltas are governed by deposition, waves, and tides

Page 52: Wave Erosion and Marine Geology

Sao Francisco, Brazil – A Wave-Dominated Delta

Page 53: Wave Erosion and Marine Geology

Ganges, Bangladesh – A Tide-Dominated Delta

Page 54: Wave Erosion and Marine Geology

Reefs Are a Major Type of Coast in Tropical Areas

4. Reefs are a special type of coastline in tropical regions

Page 55: Wave Erosion and Marine Geology

Fringing Reef, Tahiti

Page 56: Wave Erosion and Marine Geology

Tarawa – A Typical Atoll

4. Reefs are a special type of coastline in tropical regions

Page 57: Wave Erosion and Marine Geology

Reefs Also Form along the Edges of Large Islands and Continents

These Are Barrier Reefs • Australia • Yucatan • Belize • West Florida and the Keys

4. Reefs are a special type of coastline in tropical regions

Page 58: Wave Erosion and Marine Geology

Sea Level and Tectonic Activity

5. Global sea level is affected by ice ages and plate tectonics

Page 59: Wave Erosion and Marine Geology

Depth of Ocean Crust

5. Global sea level is affected by ice ages and plate tectonics

Page 60: Wave Erosion and Marine Geology

Sea-Floor Spreading and Sea Level

5. Global sea level is affected by ice ages and plate tectonics

Page 61: Wave Erosion and Marine Geology

Sea Level and Tectonic Activity

5. Global sea level is affected by ice ages and plate tectonics

Page 62: Wave Erosion and Marine Geology

Essential Points1. Wave Action erodes or deposits material

along coastlines2. Types of coastline3. Deltas are governed by deposition, waves,

and tides4. Reefs are a special type of coastline in

tropical regions5. Global sea level is affected by ice ages and

plate tectonics

How the sea modifies coastlines