Article · Wikipedia archive · Last revised Jul 20, 2026

Kakanui Range

The Kakanui Range is a range of high hills located inland from Oamaru in the South Island of New Zealand. The range forms a boundary between the valley of the Waitaki River to the north and the high plateau known as the Maniototo and the upper watershed of the Taieri River to the southwest.

Last revised
Jul 20, 2026
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Kakanui Range
The Kakanui Range dominates the eastern horizon of the Maniototo.
Highest point
PeakMount Pisgah
Elevation1,643 m (5,390 ft)
Coordinates45°04′48″S 170°23′31″E / 45.08013°S 170.39206°E / -45.08013; 170.39206
Geography
Map
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Pigroot Hill
Kattothryst
Mount Dasher
Mount Alexander
Obi
Kakanui Peak
Mount Nobbler
Mount Pisgah
Range coordinates
45°05′S 170°24′E / 45.083°S 170.400°E / -45.083; 170.400

The Kakanui Range (or Kakanui Mountains)1 is a range of high hills located inland from Oamaru in the South Island of New Zealand. The range forms a boundary between the valley of the Waitaki River to the north and the high plateau known as the Maniototo and the upper watershed of the Taieri River to the southwest.

The western Kakanui Range is crossed by road at Danseys Pass, which has a saddle at 935 m (3,068 ft). The eastern portions start to the north east of The Pigroot and Pigroot Hill to the east of the road is a foothill of the range.2

Geology

The southwestern slopes of the Kakanui Range were a major goldfield during the Otago gold rush of the 1860s. Relics from this goldrush can be found at Kyeburn and Naseby.

The Kakanui Range is composed of metamorphosed sedimentary rocks of the Rakaia Terrane. This has been described as quartzofeldspathic semischist.3: 333 

The Kakanuis continue as the Horse Range and then the Blue Mountains (there is another range called the Blue Mountains in Otago)4 to the Pacific at Shag Point.3: 330 5 Except where exposed by stream erosion or road cuttings there is no surface evidence of the rhyolitic deposits from what must have been a surface eruption at about 112 million years ago that extends this distance of 50 km (31 mi)6 and was subsequently covered by ocean sediments.

Soil

The soil in farmland near the ranges is acid and has the potential to cause aluminium toxicity in crops. Partial mitigation can be with lime, with full mitigation with gypsum unlikely to be economic.7

History

The Kakanui Mountains were mined for brown coal, limestone, and gold in the 19th century.8

Peaks

The highest point in the Kakanui Range is Mount Pisgah, at 1,643 metres (5,390 ft).9

Named Peaks in Kakanui Range
Name Height Coordinates
Mount Pisgah 1,643 metres (5,390 ft) 45°04′48″S 170°23′31″E / 45.08013°S 170.39206°E / -45.08013; 170.392069
Mount Nobbler 1,550 m (5,090 ft) 45°01′18″S 170°20′58″E / 45.02161°S 170.34944°E / -45.02161; 170.3494410
Kakanui Peak 1,528 m (5,013 ft) 45°08′01″S 170°26′22″E / 45.13371°S 170.43932°E / -45.13371; 170.4393211
Obi 1,426 m (4,678 ft) 45°10′53″S 170°28′38″E / 45.18135°S 170.47733°E / -45.18135; 170.4773312
Mount Alexander 1,357 m (4,452 ft) 44°59′22″S 170°20′50″E / 44.98956°S 170.34732°E / -44.98956; 170.3473213
Mount Dasher 1,304 m (4,278 ft) 45°08′53″S 170°29′06″E / 45.14817°S 170.48501°E / -45.14817; 170.4850114
Kattothryst 1,293 m (4,242 ft) 45°09′41″S 170°30′12″E / 45.16152°S 170.50347°E / -45.16152; 170.5034715
Pigroot Hill 758 m (2,487 ft) 45°12′28″S 170°25′51″E / 45.20789°S 170.43096°E / -45.20789; 170.430962
References

References

  1. "NZTopoMap:Kakanui Mountains". Retrieved 23 September 2024.
  2. "NZTopoMap:Pigroot Hill". Retrieved 23 September 2024.
  3. Forsyth, P.J.; Martin, G.M.; Campbell, H.J.; Simes, J.E.; Nicoll, R.S. (2006). "Carboniferous conodonts from Rakaia Terrane, East Otago, New Zealand". New Zealand Journal of Geology and Geophysics. 49 (3): 329–336. doi:10.1080/00288306.2006.9515171.
  4. "NZTopoMap:Blue Mountains". Retrieved 23 September 2024.
  5. "Bulletin". 1919.
  6. Tulloch, AJ; Ramezani, J; Mortimer, N; Mortensen; J; van den Bogaard, P; Maas, R (2009). "Cretaceous felsic volcanism in New Zealand and Lord Howe Rise (Zealandia) as a precursor to final Gondwana break-up". Geological Society, London, Special Publications. 321 (1): 89–118. doi:10.1144/SP321.5.
  7. Venter, H.J. (2017). "Soil acidity in the Kakanui ranges" (PDF). In Currie, L.D.; Hedley, M.J. (eds.). Science and policy: nutrient management challenges for the next generation Occasional Report No. 30 (Report). Palmerston North, New Zealand: Fertilizer and Lime Research Centre, Massey University. pp. 1–8.
  8. Breese, Alison (2 April 2025). Kakanui Presbyterian Church (former) (Report). Heritage New Zealand.
  9. "NZTopoMap:Mount Pisgah". Retrieved 23 September 2024.
  10. "NZTopoMap:Mount Nobbler". Retrieved 23 September 2024.
  11. "NZTopoMap:Kakanui Peak". Retrieved 23 September 2024.
  12. "NZTopoMap:Obi". Retrieved 23 September 2024.
  13. "NZTopoMap:Mount Alexander". Retrieved 23 September 2024.
  14. "NZTopoMap:Mount Dasher". Retrieved 23 September 2024.
  15. "NZTopoMap:Kattothryst". Retrieved 23 September 2024.