Reduction of greywacke sediments on the Canterbury Bight Coast, South Island, New Zealand
The coastline of the Canterbury Bight between Timaru and the southern end of Kaitorete Barrier is in long term erosion. Paradoxically, alluvial cliffs and several large, braided rivers drain from the rapidly eroding Southern Alps into the Canterbury Bight, transporting indurated sandstone of the Tor...
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| Language: | en |
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University of Canterbury. Geography
2010
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| Online Access: | http://hdl.handle.net/10092/4377 |