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explain how the sediment cell concept contributes to the understanding of coastal systems
AO1 - inputs, outputs and processes and examples. 11 in UK
equilibrium - positive and negative feedback
explain the role of geology in the formation of contrasting cliff profiles
definition
faulting - tectonic activity forming anticlynes and synclines ie lulworth cove
sedimentary - diff strata and bedding planes, lead to caves etc ie hold harry
explain the role of sea level change in the formation of emergent and submergent coastlines
emergent - ice age, creates raised beaches and fossil cliffs
submergent - ice age, global warming, thermal expansion. creates rias and fjords
explain the importance of vegetation in stabilising coastal landscapes
sand dunes - sea rocket pioneer. increase size, reduce friction, roots hold together and enables dune succession
salt marshes - eel grass. roots, wave velocity allows further deposition
explain why sustainable management of coastlines may lead to conflicts
knock on effects - hard engineering like groynes ie hornsea and mappleton
managed realignment - agricultural land vs high value land ie medmerry
explain why a range of approaches is needed to manage coastal landscapes
land value - managed realignment at medmerry vs thames barrier
engineering feasibility - some cannot work ie mobile depostional features ie spurn point, chale
explain the role of sediment transport in creating distinctive landforms
longshore drift, spits - process
longshore drift, cuspate forelands - both directions
explain why hard engineering approaches are still used to protect some coastal environments
high economic value - thames barrier
more effective than soft - sea walls, groynes
referring to examples, explain the problems of classifying coastlines
high vs low - could be low but if humans install hard engieneernig the energy and erosion patterns are changes ie terminal groyne syndrome
ST vs LT - may be emergent due to LT isostatic rebound but in ST may be submergent due to rapid sea level rise from climate change ie scotland
explain how physical factors affect recession rates
fetch - more energy if travels longer ie holderness
geology - sedimentary vs igneous vs metamorphic vs boulder clay ie holderness
explain how beach characteristics can change over the year
summer - berm, constructive waves and swash percolates
winter - berm eroded so offshore bar, may be storm ridges
explain why the use of soft engineering often leads to conflict
managed realignment - medmerry farmers vs leisure centre
no active intervention - happisburgh
explain how human activity can affect recession rates
dredging - process and reasons ie hallsands
building dams - process ie aswan dam
groynes - terminal groyne syndrome ie hornsea and mappleton
explain how concordant and discordant coastlines lead to different coastal landforms
discordant - headlands and bays, caves and arches etc
concordant - dalmation coastlines, haffs
explain why low lying coastal areas are increasingly at risk from flooding
sea level change - thermal expansion, melting ice
storm surges - more significant and higher
explain factors that determine the coastal management plan
engineering feasibility - mobile depositional features ie chale with sand dunes
CBA - forecasted both tangible/intangible ie thames barrier
explain social and economic consequences of coastal flooding
economic - from storm surges ST and LT ie north se storm surge
social - displacement and health
explain the role of geology in affecting coastal recession rates
difference between igneous, metamorphic, sedimentary and unconsolidated
explain how concordant and discordant coastlines lead to different coastal landforms
discordant - headlands and bays
concordant - haffs, dalmation coastlines, coves
explain why low lying coastal areas are increasingly at risk from flooding
rising sea levels - thermal expansion, and storm surges
isostatic changes - sedminent accretion and compaction on estu
explain the factors that determine the coastal management plan
engineering feasibility
CBA
community action
EIA
explain the role of inputs and outputs in maintaining the dynamic equilibrium of a coastal sediment cell
inputs - provide the material ie marine with tides and waves bringing in offshore sediment like from the seabed, terrestrial inputs like sub aerial process
outputs - prevent coastline from prograding (growing seaward). ie deposition causes sediment to be locked away, dredging removes material permanently
explain how human activities can disrupt the sediment budget of a coastal cell
hard engineering - groynes stop sediment transfer down drift causing terminal groyne syndrome where up drift area has sediment surplus but down drift deficit
dregding - direct output removing sediment. reasons why and effect it has
river dams
explain the concept of a sediment cell
closed system - what happens in one cell remains within the cell
operates through inputs (cliff erosion, river discharge), transfers (LSD, currents) and outputs (depositional landforms)
dynamic EQ and sediment budget - positive vs negative