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Tessellated Pavement

Stock Photography By Rodney Garnett

The Tessellated Pavement at Eaglehawk Neck is a natural floor of volcanic tiles tempered by the ocean over the ages.

Tessellated Pavement, Eaglehawk
#525286
© Rodney Garnett
Tessellated Pavement, Eaglehawk
#525304
© Rodney Garnett
Tessellated Pavement, Eaglehawk
#525303
© Rodney Garnett
Tessellated Pavement, Eaglehawk
#525300
© Rodney Garnett
Tessellated Pavement, Eaglehawk
#525296
© Rodney Garnett
Tessellated Pavement, Eaglehawk
#525287
© Rodney Garnett
Tessellated Pavement, Eaglehawk
#525288
© Rodney Garnett
Tessellated Pavement, Eaglehawk
#525299
© Rodney Garnett
Tessellated Pavement, Eaglehawk
#525289
© Rodney Garnett
Tessellated Pavement, Eaglehawk
#525292
© Rodney Garnett
Tessellated Pavement, Eaglehawk
#525293
© Rodney Garnett
Tessellated Pavement, Eaglehawk
#525294
© Rodney Garnett
Tessellated Pavement, Eaglehawk
#525291
© Rodney Garnett
Tessellated Pavement, Eaglehawk
#525297
© Rodney Garnett
Tessellated Pavement, Eaglehawk
#525290
© Rodney Garnett

 

Photo Captions for Tessellated Pavement

Image #1. Tessellated Pavement, Eaglehawk Neck, Tasmania The coastal formation appears tiled because of sets of parallel fractures running at right angles. The pan (concave formations) are caused by salt crystals disintegrating the rock during low tide. The loaf (convex formations) have the erosion along the fracture lines.[2009 213D-001]

Image #2. Tessellated Pavement, Eaglehawk Neck, Tasmania The coastal formation appears tiled because of sets of parallel fractures running at right angles. The pan (concave formations) are caused by salt crystals disintegrating the rock during low tide. [2009 213D-024]

Image #3. Tessellated Pavement, Eaglehawk Neck, Tasmania The coastal formation appears tiled because of sets of parallel fractures running at right angles. The pan (concave formations) are caused by salt crystals disintegrating the rock during low tide. [2009 213D-022]

Image #4. Tessellated Pavement, Eaglehawk Neck, Tasmania The coastal formation appears tiled because of sets of parallel fractures running at right angles. The pan (concave formations) are caused by salt crystals disintegrating the rock during low tide. [2009 213D-018]

Image #5. Tessellated Pavement, Eaglehawk Neck, Tasmania The coastal formation appears tiled because of sets of parallel fractures running at right angles. The pan (concave formations) are caused by salt crystals disintegrating the rock during low tide. [2009 213D-019]

Image #6. Tessellated Pavement, Eaglehawk Neck, Tasmania The coastal formation appears tiled because of sets of parallel fractures running at right angles. The pan (concave formations) are caused by salt crystals disintegrating the rock during low tide. [2009 213D-002]

Image #7. Tessellated Pavement, Eaglehawk Neck, Tasmania The coastal formation appears tiled because of sets of parallel fractures running at right angles. The pan (concave formations) are caused by salt crystals disintegrating the rock during low tide. [2009 213D-003]

Image #8. Tessellated Pavement, Eaglehawk Neck, Tasmania The coastal formation appears tiled because of sets of parallel fractures running at right angles. The pan (concave formations) are caused by salt crystals disintegrating the rock during low tide. [2009 213D-015]

Image #9. Tessellated Pavement, Eaglehawk Neck, Tasmania The coastal formation appears tiled because of sets of parallel fractures running at right angles. The pan (concave formations) are caused by salt crystals disintegrating the rock during low tide. [2009 213D-004]

Image #10. Tessellated Pavement, Eaglehawk Neck, Tasmania The coastal formation appears tiled because of sets of parallel fractures running at right angles. The pan (concave formations) are caused by salt crystals disintegrating the rock during low tide. [2009 213D-007]

Image #11. Tessellated Pavement, Eaglehawk Neck, Tasmania The coastal formation appears tiled because of sets of parallel fractures running at right angles. The pan (concave formations) are caused by salt crystals disintegrating the rock during low tide. [2009 213D-009]

Image #12. Tessellated Pavement, Eaglehawk Neck, Tasmania The coastal formation appears tiled because of sets of parallel fractures running at right angles. The pan (concave formations) are caused by salt crystals disintegrating the rock during low tide. [2009 213D-014]

Image #13. Tessellated Pavement, Eaglehawk Neck, Tasmania The coastal formation appears tiled because of sets of parallel fractures running at right angles. The loaf (convex formations) have the erosion along the fracture lines. [2009 213D-006]

Image #14. Tessellated Pavement, Eaglehawk Neck, Tasmania The coastal formation appears tiled because of sets of parallel fractures running at right angles. The pan (concave formations) are caused by salt crystals disintegrating the rock during low tide. [2009 213D-021]

Image #15. Tessellated Pavement, Eaglehawk Neck, Tasmania The coastal formation appears tiled because of sets of parallel fractures running at right angles. The pan (concave formations) are caused by salt crystals disintegrating the rock during low tide. [2009 213D-005]

 

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