STOCKTON

Cards (41)

  • Contemporary Strategy - Fencing
    • Response: trampling bach uses 
    • restoration and stabilisation of dunes. 
    • The  Newcastle City Council has implemented a $31.5 million Beach Renourishment program including fences, access ways and signage
    • Made from wire & timber poles 
    • Allows wind/sand pass through undisturbed 
    • Alternate Paths: Beach Renourishment program
  • Contemporary Management Strat x2
    Enforces fencing
    Raising awareness & understanding of the stress of trampling over vegetation. 
    Dune reconstruction to occur undisturbed = stabilise dune
  • Contemporary Strat- Earthmoving Equipment
    Form an aerodynamic shape manipulating dunes to the ideal slope for ideal vegetation growth. 
    Vegetation can flourish
    Stabilise dunes = trapping and stabilising sand particles, 
    Habitats for species.
  • Human-induced changes to coastal dunes
    • Clearing
    • Grazing
    • Vehicles
    • Excessive trampling
  • Foredunes
    Densely vegetated = more complex plant communities
  • Dunes are mostly found in arid tropical climate zones as they frequently experience strong onshore winds
  • Relative location of Stockton Bight

    Between Newcastle in the south & Port Stephens in the north
  • Absolute location of Stockton Bight
    Latitude of 32°50'S
    Longitude of 151°53'E
  • Accretion Cycle (4 spheres functioning together) forms Coastal Dune Systems
    1. Eroded & transported sand by rivers are deposited onto the shore by waves
    2. Sand dries out
    3. Blown to the back of the beach → vegetation stores it
    4. Destructive waves & currents takes sand back to sea
    5. Sand stored offshore
    6. Slowly deposited back with constructive waves
  • Components of the lithosphere on coastal dunes
    • Sand
    • Calcium carbonate → shells of dead sea animals & weathered + eroded rock
  • Weathering & erosive processes that occur in lithosphere are important functions for the development of sand dunes
    1. Weathering
    2. Erosion
    3. Breaking down of the lithosphere
    4. Movement & depositing of the weathered material
  • Mechanical weathering

    Main processes: hydraulic action & abrasion
  • Hydraulic action

    Strong waves are powerful forces & bombard cliff faces with water → loosen the sand particles
  • Abrasion
    Loosed particles act as sand paper & loosen other particles
  • Fluvial (water) erosion moves weathered material from its original area

    1. River discharge
    2. Longshore drift
    3. Wave action
  • Accretion Cycle

    1. Powerful storm waves erode dunes by moving large volumes of sand away from beach & dunes
    2. Aeolian (wind) Erosion moves particles of fine dry sand AWAY from shoreline, moving whole dune systems inland
  • Hydrological Processes

    Flows & storage of water<|>Pivotal role in accretion cycle<|>Through the flow of water: rivers, currents, waves & rain<|>Help deposit & removal of sediment<|>Key mechanism in erosive processes
  • River Discharge
    Hunter River is the main source of sediment = sand
  • Longshore Drift
    Type of current
    Role: Assists transporting sediment in the accretion cycle
    in Sediment that is produced/deposited is transported by the ebb (flow back) & swash (flow on) of waves
  • Wave Action
    Crucial role in accretion cycle
    Constructive: Reconstruct eroded foredune areas by depositing sand particles
    Destructive: strong winds, storms and power remove sand off & away
  • Rainfall
    Hydrological flow → dev sand dunes<|>Infiltrates sand dunes with ease<|>Heavy downpours can produce runoff → erodes the sandy surface exposing it to wind
  • Dynamics of weather and climate
    • Key weather factors: Wind, temp & precipitation
    • Move sand particles in the accretion cycle & provide conditions for vegetation to grow
  • Wind
    Onshore prevailing winds Determines SHAPE & EXTENT
    Helps shape, dry, move & weather sand
  • Aeolian (wind) transport

    Major contributor to erosion of sand particles AND mover of sand dunes in accretion cycle<|>Sand 1cm in diameter is too big to be transported by aeolian processes
  • Temperature
    Arid tropical climate zones = exp strong onshore winds
    Affects ability + time sand dries & for vegetation to be present
    Avg daily maximum in summer 21-2°C & winter 10-15°C
    Assists in the accretion cycle: providing enough heat to dry sand
  • Precipitation
    Determines how wet sand gets & assists vegetation growth<|>Influences vegetation cover → help stabilise sand on dunes<|>Role: storage of sand in accretion cycle<|>Heavy rainfall: erode steep dune faces, role: removal of sand in accretion cycle<|>Wet sand is less prone to erosion by WIND
  • Amount of Precipitation at Stockton Bight
    Wettest Months: Jan-June
    Assists with the formation of vegetation
  • Coastal vegetation

    • Evolved adaptations for poor soils, phosphate accumulation
    • Resilience against salt, wind & dehydration
  • Primary dune

    • Supported by resilient vegetation, forms a green ridge with Spinifex, acting as a natural defence against sea invasion
  • Formation of secondary dunes

    New mini dunes continue forming while dropping sea levels transform old foredunes into highly vegetated secondary dunes
  • Formation of tertiary dunes

    With further sea level drops, tertiary dunes emerge, turning the original dune into a biodiverse coastal forest
  • Natural stress
    1. Storm damage: heavy rain, strong winds & power waves
    2. Blowouts: breaches in dunes caused by strong winds
    3. Washover: big storms bring heavy destructive waves that breach foredune area
    4. Bushfires: catastrophic
    5. Introduced species- rabbits & weeds (Bitou Bush)
  • Vegetation adaptation to natural stress
    • Propagation
    • New Growth
    • Inputs in Nutrient Cycling
    • Some species need bush fires for their seeds to open
  • Vegetation succession helps stabilise dunes again after washover events
  • Long term gradual change
    Rise and fall of sea levels<|>Variation in temperature: change type of vegetation that covers the veg zones
  • Human impacts (positive and negative)

    • Negative: Reduction in biodiversity, disruption of sediment flow, coastal development, recreation use, cattle grazing, introduction of weeds and pests, sand mining
    • Positive: Fire encourages biodiversity, vegetation stabilises dunes, recent management efforts to eradicate weeds and reduce access
  • Sea walls disrupt the accretion cycle by reducing the flow of sediment along the coast, leading to erosion of the foredune area
  • Coastal development on the hind dune area transforms it into an urban area, impacting the natural dune system
  • Recreational use, such as 4wd driving and trampling by people, causes damage to the dune vegetation
  • Sand mining is the most disruptive and controversial human impact, involving the total removal of dune vegetation and taking decades to rehabilitate