Crowded Coasts

Loading...

Flash Player 9 (or above) is needed to view presentations.
We have detected that you do not have it on your computer. To install it, go here.

0 comments

Post a comment

    Post a comment
    Embed Video
    Edit your comment Cancel

    Favorites, Groups & Events

    Crowded Coasts - Presentation Transcript

    1. Crowded Coasts – An introduction
      • Understand that geology affects a coast’s topography and relief
      • Draw spider diagrams to show how coasts vary physically, and the variety of human uses of coasts
      • Understand that coastal populations are increasing worldwide
    2. Starter
      • Key Questions to consider:
      • Why do coasts vary so much?
      • What are they used for?
      • Why?
    3. Mangrove Coastline
    4. Mangrove Coastline
      • Low trees and shrubs with dense roots that grow in the marginal tidal zones between TROPICAL seas and land.
      • Adapted to area due to thick waxy leaves which conserve water by reducing transpiration during low tide.
      • Roots anchor into mudflats
      • Salt tolerant ‘halophytes’
      • Protects against storm surges and tsunamis
    5. Tropical Coastline
    6. Salt Marsh coasts
    7. Salt Marsh
      • Defined as the vegetation that occurs on muddy shores between mean high water neap and extreme high water spring tides, form on the shore due to a lack of wave action and the tide.
      • Incoming tide moves across the sheltered shore bringing sediment and detritus, the lack of wave action results in this material settling out at slack water
      • Accretion takes place; sediment builds up forming soil and can even raise the level of mud.
      • Abiotic Factors : (Non Living)
      • Saline Mud/Soil : Seawater deposits salts (solutes) in the sediment. Causing problems for plants growing
      • Waterlogged Soil: The air spaces within the soil are filled with water rather than air. Roots need oxygen for respiration as much as other parts of the plant. Long-term waterlogging creates an anaerobic condition of black mud. Which is toxic to plants.
      • Drag and Scour: The tidal movement across the surface causes a sideways drag on the plant. With two tides a day this will possibly uproot the plants. The water contains sediment like sand and mud particles and this will scour the plants like being buffed with sandpaper.
    8. Mudflats
    9. Polar Coastline
    10. Sand Dunes
    11. Reef Coastline
    12. Reef Coastline
      • Great Barrier Reef in Australia is 1500km long and comprises of 2900 different reefs
      • 3 types of reef: Fringe, barrier reefs and atolls. Charles Darwin first found these three
      • Helps dissipate wave energy
      • Fragile and open to exploitation
    13. Desert Coastline
    14. The British Seaside?
    15. What is a coast?
      • ‘ that part of the land most affected by its proximity to the sea and that part of the ocean most affected by its proximity to the land ’
      • It’s called the ‘ Zone of Transition ’
      • The Coast is the narrow zone where the land overlaps the sea and interacts
      • It is affected by Terrestrial, Human, marine and Atmospheric processes and their relationships.
      • It is the most varied and rapidly changing of all landforms and ecosystems.
    16. The Coastal Zone
    17. The Importance of Coastal Environments
      • The Coastal zone is an interface between the sea and the land. Where the marine and terrestrial processes combine to produce a variety of changing landforms.
      • Coasts suffer from rapid erosion and flooding thus can threaten lives and property.
      • Changes to coastlines are both short term (eg Storms) and long term (Rising sea levels)
    18. Factors influencing coasts The Nature of Coasts
      • Sea
      • Coastal (marine) ecosystems
      • Wave energy and direction
      • size and type of waves
      • Local currents and LSD
      • Tidal changes
      • Water depth
      • Offshore sediments
      • Long-term changes in sea level
      • Land
      • Shape of the coastline
      • Relief
      • Presence or lack of beach
      • Structure of the coast
      • Resistance of the rocks
      • Sub-aerial processes
      • River sediments
      • Coastal (land) ecosystems)
      • Weather and Climate
      • Wind strength and direction
      • Rainfall and temp
      • Storms and surges
      • Human activities
      • Intervention in natural ecosystems
      • Use of land for development
      • Exploitation of resources
    19. Did you know?
      • 3 billion people live within 100km of the coast
      • Two thirds of our largest cities are within 60km of the sea
      • Coastal population densities are usually 80 people/km2 – 50% more than inland areas
      • These can rise up to 1000+ in the Nile and Ganges Deltas
      • Coastal ecosystems are coming under constant pressure from human activities
      • There is constant competition for it’s natural resources.
      • Coastal management is becoming a major issue
      • Human intervention has lead to unexpected impacts
      • With human development and global warming demands will increase so need for management, particularly sustainable management strategies are needed.
    20. THE FACTORS
    21. Waves
      • Created by the transfer of energy from the wind blowing over the surface of the sea.
    22. Tsunamis
      • Are created not by the wind but by submarine shock waves generated by earthquakes or volcanic activity.
      • With waves the greater the wind the greater the frictional drag and therefore the size of wave
      • Those that travel short distances and are the result of local waves are seen as sea waves
      • Those that are formed from distant storms and travel large distances are known as swell .
    23. Wave Energy
      • Wind velocity
      • Period of time the wind has blown
      • Length of the fetch
    24. Exercise 1.
      • On a map of the UK find areas which have the biggest fetch
    25. Wave terminology
      • CREST
      • TROUGH
      • WAVE PERIOD
      • LENGTH
      • VELOCITY
      • STEEPNESS
      • ENERGY
      • SWELL
      • CREST – Highest point of the wave
      • TROUGH
      • WAVE PERIOD
      • LENGTH
      • VELOCITY
      • STEEPNESS
      • ENERGY
      • SWELL
      • CREST – Highest point of the wave
      • TROUGH – lowest point of the wave
      • WAVE PERIOD
      • LENGTH
      • VELOCITY
      • STEEPNESS
      • ENERGY
      • SWELL
      • CREST – Highest point of the wave
      • TROUGH – lowest point of the wave
      • WAVE PERIOD – Time taken for wave to travel one wave length
      • LENGTH -
      • VELOCITY
      • STEEPNESS
      • ENERGY
      • SWELL
      • CREST – Highest point of the wave
      • TROUGH – lowest point of the wave
      • WAVE PERIOD – (T) Time taken for wave to travel one wave length
      • LENGTH – (L) Distance between two successive waves
      • VELOCITY -
      • STEEPNESS
      • ENERGY
      • SWELL
      • CREST – Highest point of the wave
      • TROUGH – lowest point of the wave
      • WAVE PERIOD – (T) Time taken for wave to travel one wave length
      • LENGTH – (L) Distance between two successive waves
      • VELOCITY – (C) speed of movement of a crest in a given period of time
      • STEEPNESS -
      • ENERGY
      • SWELL
      • CREST – Highest point of the wave
      • TROUGH – lowest point of the wave
      • WAVE PERIOD – (T) Time taken for wave to travel one wave length
      • LENGTH – (L) Distance between two successive waves
      • VELOCITY – (C) speed of movement of a crest in a given period of time
      • STEEPNESS – (H/L) ratio of wave height divided by length it can not exceed 1:7 (0.14) as it will break
      • ENERGY
      • SWELL
      • CREST – Highest point of the wave
      • TROUGH – lowest point of the wave
      • WAVE PERIOD – (T) Time taken for wave to travel one wave length
      • LENGTH – (L) Distance between two successive waves
      • VELOCITY – (C) speed of movement of a crest in a given period of time
      • STEEPNESS – (H/L) ratio of wave height divided by length it can not exceed 1:7 (0.14) as it will break
      • ENERGY – (E) expressed as E~ (Is proportional to) LH2
      • SWELL –
      • CREST – Highest point of the wave
      • TROUGH – lowest point of the wave
      • WAVE PERIOD – (T) Time taken for wave to travel one wave length
      • LENGTH – (L) Distance between two successive waves
      • VELOCITY – (C) speed of movement of a crest in a given period of time
      • STEEPNESS – (H/L) ratio of wave height divided by length it can not exceed 1:7 (0.14) as it will break
      • ENERGY – (E) expressed as E~ (Is proportional to) LH2
      • SWELL – have low height, gentle steepness and long wave length
    26.  
    27. World map – coastal hotspots?
    28. Types of coasts?
      • Trade Coasts?
      • Recreation coasts?
      • Residential coasts?
      • Resource coasts?
      • Exercise 2: Complete a table with examples of each
    29. High Value coastal environments?
      • Exercise 3: Identify the features, opportunities, value and pressures for each of the following:
      Mangroves Reefs Salt Marshes
    30. Exercise 4
      • Annotate photo to identify
      • Physical features
      • Human features
      • Opportunities
      • Threats/pressure
    31. So...
      • As you can see there are many different forms of coasts and they vary enormously.
      • In groups define the benefits for differing regions in terms of geology and relief that an area may possess and see if you can think of examples from your own ideas.
    32. Finally
      • Using your textbooks look at some of the places and answer these questions below:
      • Physical features (use the words topography, geology, relief). How have these affected the coast?
      • its human activities (e.g. industry, tourism, port)/ What were the reasons for these activities developing here?
      • What are the possible futures for these areas?

    + fozziefozzie, 10 months ago

    custom

    820 views, 0 favs, 0 embeds more stats

    Introduction to AS Edexcel crowded coasts with lots more

    More info about this document

    © All Rights Reserved

    Go to text version

    • Total Views 820
      • 820 on SlideShare
      • 0 from embeds
    • Comments 0
    • Favorites 0
    • Downloads 34
    Most viewed embeds

    more

    All embeds

    less

    Flagged as inappropriate Flag as inappropriate
    Flag as inappropriate

    Select your reason for flagging this presentation as inappropriate. If needed, use the feedback form to let us know more details.

    Cancel
    File a copyright complaint
    Having problems? Go to our helpdesk?

    Categories