Dunstan Mountains | |
---|---|
Highest point | |
Peak | Dunstan |
Elevation | 1,667 m (5,469 ft)[1] |
Coordinates | 44°52′S 169°35′E / 44.867°S 169.583°E45°02′56″S 169°22′34″E / 45.049°S 169.376°E |
Dimensions | |
Length | 51 km (32 mi) 45° |
Width | 19 km (12 mi) 135° |
Area | 826 km2 (319 sq mi) |
Naming | |
Native name | Mataki-nui, Neinei-i-kura, Tiko-umu (Māori) |
English translation | Matakanui translates as big burn on the face |
Geography | |
Otago, South Island, New Zealand | |
Country | New Zealand |
Region | Otago |
Range coordinates | 44°52′16″S 169°35′24″E / 44.871°S 169.590°E |
Parent range | Dunstan Mountains |
Topo map | NZMS260 F41 Edition 1 1991 Limited Revision 1996 |
Geology | |
Orogeny | Kaikoura Orogeny |
Age of rock | 200 Ma |
Mountain type | Fault-block mountain |
Type of rock | Schist |
The Dunstan Mountains are a mountain range in Central Otago, in the South Island of New Zealand. The mountains lie on the eastern shore of the man-made Lake Dunstan and overlook the towns of Cromwell to the west, Clyde to the south and Omakau to the east. The highest named peak on the mountain range, a rocky knoll simply called Dunstan, is 1,667 m (5,469 feet).
Together with the Cairnmuir Mountains to the south, the Dunstan Mountains form the Cromwell Gorge which was dammed to form New Zealand's third-largest hydroelectric dam,[Note 1] the Clyde Dam.
The Dunstan Mountains should not be confused with the Dunstan Range, a small mountain range which lies approximately 20 km (12 mi) north of the Dunstan Mountains near the Lindis Pass.
Cite error: There are <ref group=Note>
tags on this page, but the references will not show without a {{reflist|group=Note}}
template (see the help page).