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Auckland topographic map
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Auckland
The Auckland Volcanic Field has contributed greatly to the growth and prosperity of the Auckland Region since the area was settled by humans. Initially, the maunga (scoria cones) were occupied and established as pā (fortified settlements) by Māori due to the strategic advantage their elevation provided in controlling resources and key portages between the Waitematā and Manukau harbours. The rich volcanic soils found in these areas also proved ideal for the cultivation of crops, such as kūmara. Following European arrival, many of the maunga were transformed into quarries to supply the growing city with aggregate and building materials, and as a result were severely damaged or entirely destroyed. A number of the smaller maar craters and tuff rings were also removed during earthworks. Most of the remaining volcanic centres are now preserved within recreational reserves administered by Auckland Council, the Department of Conservation, and the Tūpuna Maunga o Tāmaki Makaurau Authority.
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About this map
Name: Auckland topographic map, elevation, terrain.
Location: Auckland, New Zealand (-37.36447 173.89633 -35.69839 175.90322)
Average elevation: 30 m
Minimum elevation: -1 m
Maximum elevation: 836 m
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Other topographic maps
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Wellington
New Zealand > Wellington > Wellington City
Averaging 2,055 hours of sunshine per year, the climate of Wellington is temperate marine, (Köppen: Cfb), generally moderate all year round with warm summers and mild winters, and rarely sees temperatures above 26 °C (79 °F) or below 4 °C (39 °F). The hottest recorded temperature in the city is 31.1 °C…
Average elevation: 85 m
