This diagram is a reconstruction of how Torlesse greywacke and associated sediments formed at the edge of the Gondwana supercontinent. Rivers carried sediment from land out to sea on the continental shelf, where it was then transported down channels as turbidity currents onto huge submarine fans on the deep ocean floor.
Te whakamahi i tēnei tūemi
Te Ara - The Encyclopedia of New Zealand
by Bruce Mahalski
Source: Glen Coates, The rise and fall of the Southern Alps. Christchurch: Canterbury University Press, 2002
This item has been provided for private study purposes (such as school projects, family and local history research) and any published reproduction (print or electronic) may infringe copyright law. It is the responsibility of the user of any material to obtain clearance from the copyright holder.