Hokitika River Explained

Hokitika River
Source1 Location:Southern Alps
Mouth Location:Tasman Sea
Subdivision Type1:Country
Subdivision Name1:New Zealand
Length:64km (40miles)

The Hokitika River is in the West Coast of the South Island of New Zealand. It is about 64km (40miles) long, beginning in the Southern Alps, emerging from the narrow Hokitika Gorge after merging with the Whitcombe River, and flowing into the Tasman Sea just south of the town of Hokitika. The river then feeds into the offshore Hokitika Canyon, which merges with the Cook Canyon to form the Cook Channel. The canyons extend to about 650km (400miles) and are important spawning areas for hoki, hake[1] and orange roughy.[2]

The Hokitika River, and its eastern tributary, the Kokatahi River, have formed the Kowhitirangi-Kokatahi alluvial plain; a fertile and productive land extensively used for dairy farming.

The entrance to the Hokitika River was once used as a harbour during the West Coast gold rush; however, the sand bar at the river mouth created a treacherous and often fatal obstacle - resulting in many shipwrecks. After the gold-rush subsided, the use of the river as a harbour declined and is now no longer used.

References

-42.7167°N 227°W

Notes and References

  1. Web site: 2005-12-18 . Vast underwater canyons revealed . 2022-11-21 . NIWA . en.
  2. Web site: B.R. Moore, C. Ó Maolagáin, K. Spong, A. Dutilloy, R.J. Saunders . December 2021 . Age composition of orange roughy from Cook Canyon (ORH 7B) in 2019 and 2020 . NIWA.