Coastal Processes and Landforms
Coastal Processes and Landforms Coastal Processes and Landforms
3. Coral Coastal Features• Atoll
3. Coral Coastal Features• Atoll• Hypothesis 1: Coral grows atopunderwater volcano Coral C• Hypothesis 2: Coral grows upwardson a sinking volcanic island, or as sealevel rises
- Page 34: • Abrasion: weathering byrock fra
- Page 37 and 38: • Coastal Landslide: Alternate we
- Page 39 and 40: • Chemical weathering:Salt weathe
- Page 46 and 47: Sea level rise in the lower mainlan
- Page 48 and 49: 1. Depositional Features2. Rock Coa
- Page 50 and 51: 1. Depositional Featuresb) Beach be
- Page 52 and 53: 1. Depositional Featuresc) Beach cu
- Page 54 and 55: 1. Depositional Featuresd) (Sand) b
- Page 56 and 57: 1. Depositional Featuresd) (Sand) b
- Page 58 and 59: 1. Depositional Featurese) Sand spi
- Page 60 and 61: 1. Depositional Featurese) Barrier
- Page 62 and 63: 1. Depositional Featurese) Spits an
- Page 64 and 65: 1. Depositional Featurese) Tombolo,
- Page 66 and 67: 1. Depositional Featuresf) Estuarie
- Page 68 and 69: 2. Rock Coast Features
- Page 70 and 71: 2. Rock Coast Features
- Page 72 and 73: The force of the waves hitting a cl
- Page 74 and 75: Rock fragments which have becomedet
- Page 76: Formation of a Sea arch and stack
- Page 79 and 80: • Eventually the cliff becomesuns
- Page 81 and 82: Erosive waves may blast theirway ve
- Page 83 and 84: 3. Coral Coastal FeaturesCoral land
- Page 88 and 89: 2. Rock Coast Features• Coral ato
- Page 90 and 91: 2. Rock Coast Features• Coral ato
- Page 92 and 93: Tuvalu, only 4 m above sea level an
- Page 94 and 95: 3. Coral Coastal Features• Barrie
- Page 96: Shallow lagoons formed close to the
3. Coral <strong>Coastal</strong> Features• Atoll