Wave formation
Made by friction between wind + sea surface
size depends on wave spped + fetch
Formation of a wave - Fetch
Distance of open sea that wave travels before reaching the shore
Formation of a wave - Shore
Area of beach exposed between high + low tide
Parts of a wave - Crest
Top of a wave
Parts of a wave - Trough
Bottom of a wave
Parts of a wave - Wavelenght
Distance between 2 crests
Parts of a wave -Breakin gwave
Friction slows down trougha of waves as they approach shore. Wave becomes steeper as fast crest catches up + collapses over the trough
Parts of a wave -Swash
Beach material carried up the shore by a breaking wave
Parts of a wave -Backwash
When the swash has no more energy, it drags lighter material with it as it flows back to the sea
deposititing waves are
Constructive waves
Eroding waves are called
Destructing waves
Wave Refraction - def
Waves change direction as the approach the shore due to friction
Erosion factors - List
Composition
Wave strength
Coastal shape
Shore gradient
Human activity
Rising sea levels
Climate change
Erosion factors - composition
Hard coast (sandstone cliffs) erode slowly. Soft coasts (clay + sand) erode fast
Erosion factors - Wave strength
destructive waves are strong + cause erosion - strongest in storms
Erosion factors -Coastal shape
Determines the amount of wave refraction that occurs
Erosion factors -Shore gradient
Steep slopes = more destructive waves becuase they break close to the shore
Erosion factors -Human activity
Removal of beach material material increases erosiom. Sea walls + rock armour reduce erosion
Erosion factors -Rising sea levels
Higher sea levels = higher flooding + erosion
Erosion factors - climate change
Increased storm frequency + strength - increased erosion
Compression
Coastal erosion. Waves wash over rocks. air is compressed within cracks + joints. As the waves retreat, air expands, weakening + shattering the rock
Bays and headlands eg
Dublin Bay, Co Dublin
Bays and headlands - description
Bays are curved indents on the coastline formed by destructive waves. A headland is a section of land that protrudes further into the sea than its surrounding coastline
Bays and headlands - explanation
An area of soft rock along the coast has hard rock on either side of it. Due to differential erosion from hydraulic action and compression , the soft rock erodes much faster, creating an indent called a bay with the headlands jutting out on either side. This leads to wave refraction which causes deposition in the bay leading to beach formation