The Auckland Islands are an archipelago of New Zealand, lying 465 km (289 mi) south of the South Island. The main Auckland Island, occupying 460 km2 (180 sq mi), is surrounded by smaller Adams Island, Enderby Island, Disappointment Island, Ewing Island, Rose Island, Dundas Island, and Green Island, with a combined area of 570 km2 (220 sq mi). The islands have no permanent human inhabitants.
The Otago Peninsula is a long, hilly indented finger of land that forms the easternmost part of Dunedin, New Zealand. Volcanic in origin, it forms one wall of the eroded valley that now forms Otago Harbour. The peninsula lies south-east of Otago Harbour and runs parallel to the mainland for 20 km, with a maximum width of 9 km. It is joined to the mainland at the south-west end by a narrow isthmus about 1.5 km wide.
Portobello is a village beside the Otago Harbour halfway along the Otago Peninsula in Dunedin City, New Zealand. It lies at the foot of a small peninsula between Portobello Bay and Latham Bay.
Otago Harbour is the natural harbour of Dunedin, New Zealand, consisting of a long, much-indented stretch of generally navigable water separating the Otago Peninsula from the mainland. They join at its southwest end, 21 km (13 mi) from the harbour mouth. It is home to Dunedin's two port facilities, Port Chalmers and at Dunedin's wharf. The harbour has been of significant economic importance for approximately 700 years, as a sheltered harbour and fishery, then deep water port.
Dunedin is the second-largest city in the South Island of New Zealand, and the principal city of the Otago region. Its name comes from Dùn Èideann, the Scottish Gaelic name for Edinburgh, the capital of Scotland. The city has a rich Māori, Scottish, and Chinese heritage.
Port Chalmers is a town serving as the main port of the city of Dunedin, New Zealand. Port Chalmers lies ten kilometres inside Otago Harbour, some 15 kilometres northeast of Dunedin's city centre.
The Taieri Plain is an area of fertile agricultural land to the southwest of Dunedin, in Otago, New Zealand. The plain covers an area of some 300 square kilometres, with a maximum extent of 30 kilometres. It is not to be confused with Strath Taieri, a second plain of the Taieri River, 40kms to the north beyond Mount Ross.
Quarantine Island, is the largest island in Otago Harbour, close to the city of Dunedin, New Zealand. The island covers an area of 15 hectares, and is a publicly accessible recreation reserve. The buildings on the island are owned by Quarantine Island / Kamau Taurua Community Incorporated (QIKTC). Its management is shared between QIKTC and the Department of Conservation.
Macandrew Bay is located on the Otago Peninsula in the South Island of New Zealand. It is situated on the edge of Otago Harbour, and is named for pioneer Scottish settler James Macandrew who lived here during his later life. The Te Reo Māori name for the bay, Te Roto Pāteke, refers to the Brown teal formerly prevalent in the area. Early European residents of the area called the bay "The Hundreds", due to the large number of boulders which covered the foreshore.
The Portobello Marine Laboratory is located on the end of a short peninsula close to the township of Portobello, within the limits of the city of Dunedin in New Zealand's South Island. It is run as part of the University of Otago, the main campus of which is 23 kilometres to the southwest in Dunedin's main urban area.
The villages and then city that lay at the head of Otago Harbor never existed in isolation, but have always been a staging ground between inland Otago and the wider world. While Dunedin's current official city limits extend north to Waikouaiti, inland to Middlemarch and south to the Taieri River mouth, this articles focus is the history of the Dunedin urban area, only mentioning Mosgiel, the Otago Peninsula, Port Chalmers and inland Otago for context.
Flagstaff, known in Māori as Te Whanaupaki, is a prominent hill overlooking the northwest of the city of Dunedin, in New Zealand's South Island. Together with Mount Cargill, which lies to its northeast, it dominates the skyline of the city. Flagstaff lies seven kilometres to the north of Dunedin's city centre.
St Leonards is a suburb of the New Zealand city of Dunedin. It is located close to the northern shore of the Otago Harbour and on the hilly slopes above the harbour. St Leonards is 8.5 kilometres (5.3 mi) northeast of Dunedin's city centre, between the small settlement of Burkes and Sawyers Bay. St Leonards was named by early settler David Carey for the birthplace of his wife, the English town of St Leonards-on-Sea, on the Sussex coast.
Ravensbourne is a suburb of the New Zealand city of Dunedin. It is located on Otago Harbour on the steep southeastern slopes of Signal Hill. It lies on the harbour's northern shore, 4.5 kilometres (2.8 mi) east-northeast of the city centre.
State Highway 88 (SH 88) is a New Zealand State Highway connecting the city centre of Dunedin with Port Chalmers, which is the location of Dunedin's main port facilities and home of one of New Zealand's major container terminals. It is roughly 12 km long.
Papanui Inlet is the northernmost of two large inlets in the Pacific coast of Otago Peninsula, in the South Island of New Zealand.
Hoopers Inlet is one of two large inlets in the Pacific coast of Otago Peninsula, in the South Island of New Zealand.
Te Aka Ōtākou is a cycleway and shared pathway for walking and cycling in Dunedin, New Zealand, which follows the shoreline of the Otago Harbour. It also known as the Otago Harbour Cycleway, and has previously been known by various names, including The Harbour Loop, and by the names of various sections.
The Dunedin volcanic group is a volcanic group that covers over 7,800 km2 (3,000 sq mi) of Otago in the South Island of New Zealand. It is a recent reclassification of the group previously known as the Waiareka-Deborah volcanic field due to common magma melt ancestries of the Dunedin Volcano with the overlapping alkali basaltic monogenetic volcanic field. Excluded from the group are a group of volcanics of different composition and older age near Oamaru, which have been given the name previously used for the Dunedin group. The older Waiareka-Deborah volcanic field overlaps the new Dunedin volcanic group geographically; though Dunedin Volcano has been well studied from the 1880s since New Zealand's first school of geology was established at the University of Otago, detailed studies of north-central volcanoes such as the Crater near Middlemarch were done much later, and high-quality composition studies still need to be done to properly classify many volcanics near Oamaru.
