Seaforth River Explained

Seaforth River
Pushpin Map:New Zealand Fiordland#New Zealand South Island#New Zealand
Pushpin Map Size:270px
Pushpin Map Caption:Mouth of the Seaforth River
Source1 Coordinates:-45.5308°N 167.099°W
Mouth Location:Supper Cove, Tamatea / Dusky Sound
Mouth Elevation:0m (00feet)
Mouth Coordinates:-45.6975°N 166.9599°W
Subdivision Type1:Country
Subdivision Name1:New Zealand
Subdivision Type2:Region
Subdivision Name2:Southland
Subdivision Type3:District
Subdivision Name3:Southland
Tributaries Left:Kintail Stream, Bessie Burn, Deadwood Creek, Jane Burn, Roa Stream
Tributaries Right:Kenneth Burn, Bishop Burn, Macfarlane Stream, Henry Burn
Waterbodies:Gair Loch

The Seaforth River is a river in New Zealand, flowing into Dusky Sound. About 9km (06miles) and 41m (135feet) up from Supper Cove in Dusky Sound is Lake Maree. The river rises about another 20km (10miles) to the north, on the slopes of the Black Giants, at about 1300m (4,300feet).[1] Like many former British Empire locations, it and its lakes have Scottish names.

The river was first mapped in 1896 by Thomas Mackenzie, who was briefly Prime Minister in 1912.[2] He described cataracts of 10feet, 25feet and 60feet between the Sound and the Loch[3] and named the river after himself. However, in 1897 E. H. Wilmot discovered that the Mackenzie and Seaforth were the same river and removed the former name.[4] The route Mackenzie followed is now part of the Dusky Track.[5] It was thought that few had followed the route until at least 1950.[6]

Carbon dating of beech tree stumps in Lake Maree indicate it was formed when a large rock fall dammed the river during the 1826 earthquake.[7] Near Kintail Hut, Gair Loch is another debris dammed lake.[8] Further debris fell, probably during the 2011 Christchurch earthquake.[9]

Mackenzie described the vegetation as mainly birch, with red-pine, rata, and some totara. He said that there were also ribbon-wood, panax, mikimiki, pepper-tree, mokomoko, tutu, ferns and mosses.[10]

A 1981 survey identified six native fish - Anguilla dieffenbachii, Prototroctes oxyrhynchus, Galaxias maculatus, Galaxias fasciatus, Galaxias brevipinnis and Gobiomorphus huttoni.[11]

Moose were liberated in the valley in 1910,[12] but it is not thought that they survived.

See also

Notes and References

  1. Web site: Seaforth River, Southland. NZ Topo Map. en. 2019-08-04.
  2. Web site: 1896 Department of Lands and Survey Annual Report. paperspast.natlib.govt.nz. 2019-08-04.
  3. Web site: 1896 Department of Lands and Survey Annual Report. paperspast.natlib.govt.nz. 2019-08-04.
  4. Web site: Department of Lands and Survey Annual Report. 1 January 1897. paperspast.natlib.govt.nz. 2019-08-04.
  5. Web site: Dusky Track. Department of Conservation.
  6. Web site: Through The Rain Forests From Manapouri To Dusky. Otago Daily Times. A. H. Reed. 4 September 1950. paperspast.natlib.govt.nz. 2019-08-05.
  7. Web site: Recent mapping and radiocarbon dating of three giant landslides in northern Fiordland, New Zealand, GNS Science Report 2012/45. Hancox, G. T.; Langridge, R. M.; Perrin, N. D.; Vandergoes, M.; Archibald, G.. Aug 2013.
  8. Web site: Southland District Plan Section 6. 27 June 2001.
  9. Web site: From Dawn to Dusky. 2017-05-01. en. 2019-08-04.
  10. Web site: 1896 Department of Lands and Survey Annual Report. paperspast.natlib.govt.nz. 2019-08-04.
  11. Web site: Freshwater fish in Fiordland National Park. R. M. MCDowall. April 1981. NIWA.
  12. Web site: Southland Times. 29 March 1910. paperspast.natlib.govt.nz. 2019-08-05.