Coastal processes Flashcards
Waves
Most waves are formed by wind blowing across the surface of the sea or other large body of water. The friction between the wind and the surface of the water causes the water to move in a circular motion. Although the wave moves forward, the water does not move with it. As the wave moves into shallow water, it breaks. When the depth of the sea is less than the height of the wave, friction with the bottom increases and the wave slows down. The wavelength becomes shorter and the front of the wave becomes steeper. The top of the wave then tumbles forward. When this happens, the wave is said to break.
Wave erosion
Hydraulic Action: Waves can hit the coastline with a great deal of force. The force with which waves hit the coastline is often enough to cause erosion.
Abrasion/ corrasion: The material carried by the wave is thrown against the coast, thereby eroding it.
Attrition: Small stones and other material carried by the wave are thrown against each other. They are further broken down and worn into a round shape.
Solution: Sea water dissolves soluble minerals in the rocks on the coastline.
Cliffs/wave cut platforms
A cliff is defined as a steep rock face. Where marine erosion is powerful, the coastline is eroded to form a cliff. Erosion is concentrated at sea level. A notch is cut in the rock at the level where wave attack is concentrated. When the notch is cut too far, the area above this notch collapses forming a cliff.
Headlands and bays
headlannd- a section of rocky coastline that protrudes into the sea
bay- a pronounced indentation in the coastline usually found in between two headlands.
Long-shore drift
The transport of sand and pebbles along the coast.
Spits
These are formed when material is deposited along the coastline by longshore drift
Tombolo
This is a linear deposit of material formed by longshore drift which joins an island to the mainland.
Coral reef definition
A coral reef is an offshore ridgeoro formed from the secretions of small marine animals called coral polyps.
types of coral reefs
barrier reefs, fringing reefs and atoll
Fringing reef
is a shallow water features found close to and parallel to the shore. it forms from the gradial accumulation of coral to the coast. Over time, storms and marine erosion move the coral to form the irregular coral platforms.
barrier reef
lies in deeper water, much further to sea. develops near low living coastal plains. a rise in sea levels floods the coastal lowland, creating a wider body of water. coral continues to grow to form a large barrier feature that is now separated from the coast.
atoll reef
is an isolated ring-shaped week rising our of deep water.
conditions coral favours
Temperature- the water should be warm. most corals thrive in temperature 21 and 30 degrees celsius.
depth-coral feed on algae which need light to photosynthesize and grow, if there is not enough light there will be no algae.
salinity-corals thrive in salty water .The water should contain the right amount of salt. Coral will not grow in areas where a large amount of fresh water pours into the sea.
Benefits of coral reefs
Reefs provide a home for many species of marine life including sponges, algae, sea urchins, shellfish and fish.
Many tourists visit tropical areas to visit coral reefs.
Problems coral reefs face
overfishing
ecological damage(tourism)