PAL Coasts

Cards (150)

  • What is the littoral zone?
    Coastal zone in which sediments are moved around between the land, beach and sea
  • What does the littoral zone contain?
    Coastal sediments (pebbles and sand particles) that are moved by waves, currents and tides, which is from highest sea level line (linked to high tides and storm waves) to shallow offshore waters (where the base of a wave first encounters friction with the sea bed)
  • What is the backshore?
    Area sitting above high tide level. Coastal processes only affect the backshore when there is an extreme weather event, such as a storm
  • What is the foreshore?
    Marks the zone between the high and low tide marks. Many wave processes take place here
  • What is the nearshore?
    An area just off the coastline, consisting of shallow sea water
  • What is the offshore?
    Open sea
  • What is the effect of geology?
    Can create rocky, sandy and estuarine coasts, as well as concordant and discordant coasts
  • What is the effect of energy?
    Levels of energy can create high or low energy coastlines
  • What is the effect of balance?
    Between erosion and deposition, creating either erosional or depositional coasts
  • What is the effect of sea level change?
    Creates either emergent or submergent coastlines. More broadly, we can classify coastlines into rocky and coastal plains
  • What are rocky coastlines?
    Vary in height, formed from hard rock, dominated by marine and sub-aerial processes
  • What are coastal plains?
    Low-lying, low-relief, contain wetland and marshlands, poor drainage, flatter landscapes
  • What are concordant coastlines?
    Generated when rock strata run parallel to the coastline
  • What are discordant coastlines?
    Form when different rock strata intersect the coast at an angle, so geology varies along the coastline
  • What type of coasts are bays and headlands associated with?
    Discordant
  • What are bays and headlands?
    When alternate bands of hard and soft rock erode at right angles. Softer rock erodes more rapidly, forming a bay. Harder rock is more resistant and juts out as a headland. Headlands are vulnerable to wave refraction. Coves form on concordant coastlines. Once waves erode through harder out rock, softer rock begins to erode
  • What is wave refraction?
    The bending of a wave as it spreads over different depths along a coast
  • How is a dalmatian coastline formed?
    Where geology creates valleys parallel to the coast so that when the sea level rises, a series of elongated island remain offshore
  • What is a haff coastline?
    Where sand dunes and spits run parallel to the coastline
  • What is lithology?
    Refers to physical characteristics of particular rocks
  • What are the 3 main types of rocks?
    Igneous, sedimentary, and metamorphic, as well as unconsolidated (loose) material such as clau
  • What does the type of rock influence?
    Permeability which affects rates of erosion, affecting features formed
  • What are igneous rocks?
    Granite, diorite, basalt
    Crystalline, resistant, impermeable
  • What are sedimentary rocks?
    Limestone, chalk, sandstone, shale
    Formed in strata
    Jointed sedimentary rocks (limestone and sandstone) are permeable
    Other sedimentary rocks (chalks) have air spaces between their particles so are porous
    Shale is fine and compacted making it impermeable
  • What are metamorphic rocks?
    Marble, schist, slate
    Very hard and resistant
    Impermeable
  • What are unconsolidated materials?
    Glacial till or boulder clay e.g on Holderness coast
    Loose and easily eroded
    If compacted, particles can stick together and form an impermeable layer within a cliff strata
  • What is coastal morphology?
    Refers to the shape and form of coastal landscapes and their features
  • What is coastal morphology determined by?
    Lithology or physical characteristics of the rock
    Relief and slope (cliff profiles)
    Rock type and its permeability
    How resistant to erosion the rock is
  • What characteristics contribute to geological structure?
    • Strata - layers of rocks and their positioning, often with many different types
    • Bedding planes - splits in rocks, creating horizontal blocks
    • Joints - splits in rocks, creating vertical blocks
    • Folds and dips - deformations in rock due to tectonic activity; susceptible to pressure
    • Faults - weaknesses in rock geology that is susceptible to erosion
  • What is a cliff profile?
    Cross section of a cliff from a low water mark to top of cliff
  • What causes different structures to emerge on coastlines?
    Interactions between geological structures and lithology
  • What is a horizontal dip?
    Uniform horizontal layers and bedding planes can produce steep sided cliffs. Notches will appear in the cliff face
  • What is a seaward dip, high angle?
    Where dipping is steep, rockslides become common due to large slabs of rock sliding down
  • What is a seaward dip, low angle?
    Joints opened by weathering and pressure releases slabs to form cliffs that dip seaward
  • What is a landward dip?
    Bedding planes dipping inland, producing steep and stable cliffs
  • What affects coastal recession?
    Geology and lithology affect rates of erosion and speed at which coastline recedes and retreats
    Weathering and mass movement processes also affect rate of erosion
    Most cliffs are formed of more than one rock type and will produce complex cliff profiles
  • What is the role of vegetation?
    Stabilise sediment
  • How plants stabilise sediment?
    Plants growing in sediment provide an extra layer of protection, so the surface of sediment is not as exposed
    Plants protect sediment from aeolian (wind) erosion by reducing wind speed due to friction with vegetation and binding sediment together
  • What do plants growing in coastal and estuarine environments tend to be?
    Halophytic (salt tolerant) and xerophytic (drought tolerant)
  • Outline salt marshes
    Form in sheltered, low energy estuarine environments. Rivers and tides deposit silt and mud, causing mudflats to develop. These are colonised by vegetation that are halophytic. Vegetation growth and deposition of silt and mud over time causes a salt marsh to emerge