Image
Mud and sand from Kaikōura and Cook Strait canyons are carried by fast, muddy flows called turbidity currents. Most turbidity currents spill out of a gap 1,400 kilometres along the channel, where the current known as the Ocean Conveyor spreads the sediment into a fan. Some currents continue up to 600 kilometres further across the deep ocean floor.
Using this item
Te Ara - The Encyclopedia of New Zealand
Source: NIWA – National Institute of Water and Atmospheric Research
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.