In Greymouth I found some accommodation and drove 40kms to Punakaiki to visit the pancake rocks and blowholes. The Pancake Rocks are a heavily eroded limestone. The sea bursts though a number of vertical blowholes during high tides. The 'pancake'-layering of the limestone was created by immense pressure on alternating hard and soft layers of marine creatures and plant sediments formed 30 million years ago.
Saturday, April 14, 2012
Greymouth and Punakaiki
I travelled from Hanmer Springs through the Lewis Pass to Greymouth.

In Greymouth I found some accommodation and drove 40kms to Punakaiki to visit the pancake rocks and blowholes. The Pancake Rocks are a heavily eroded limestone. The sea bursts though a number of vertical blowholes during high tides. The 'pancake'-layering of the limestone was created by immense pressure on alternating hard and soft layers of marine creatures and plant sediments formed 30 million years ago.


In Greymouth I found some accommodation and drove 40kms to Punakaiki to visit the pancake rocks and blowholes. The Pancake Rocks are a heavily eroded limestone. The sea bursts though a number of vertical blowholes during high tides. The 'pancake'-layering of the limestone was created by immense pressure on alternating hard and soft layers of marine creatures and plant sediments formed 30 million years ago.
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