C l i f f s
  
 
 
 
Christmas Island is the uplifted peak of a huge underwater volcanic mountain, rising steeply some 5000 m from the ocean floor. The highest point on the island is 361 m above sea level. Over the eons, the island has been raised above sea level in stages allowing the wave action to cut new cliffs at each stage, resulting in a series of picturesque terraces and dramatic coastal and inland cliffs rising to a central plateau at about 250-300 m. Coral formed over the volcanic core at each stage of the island’s development, providing a thick crust of limestone that now covers the island.
 
     
 
Centuries of erosion from the harshest punishment of nature... relentless waves, ocean swells, cyclones, and monsoon rains has sculpted a uniquely picturesque but mostly inaccessible coastline around the island.
 
     
     
 
  
 
 
 
The Blowholes
 
 
Martin Point
 
 
 
  
 
 
 
Margeret Knoll
 
 
Low Point
 
 
 
  
 
 
 
North-East Coastline
 
 
North-West Chasm
 
 
 
  
 
 
 
 
 
     
 

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