UniServe Science

Virtual Field Trip - Pheasant Point, Kiama, NSW


Inlet caused by differential weathering of dyke Differential weathering between the sediemnts and the dyke Close up of the chilled margin

[Inlet and associated dyke]
[Dyke has weathered at different rate to the surrounding sediments]
[Chilled margin on the dyke]


[Pheasant Point]
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Last Update: Monday, 30-Apr-2012 15:08:50 AEST
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