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McLennan Hills (also Te Aponga o Tainui) is one of the volcanoes in the Auckland volcanic field. It was a group of cratered scoria mounds up to 45 m high, before it was quarried away. A 1940 aerial photo (in Searle's book) shows a crater around 100 m wide, one around 50 m wide, and 2 or 3 smaller craters. McLennan Hills, alongside neighbouring Ōtāhuhu / Mount Richmond, were the sites of fortified pā in pre-European times, important due to their location between the Waitematā Harbour/ Tāmaki River and the Manukau Harbour. [1] Since the European settlement of Auckland, the scoria cone was quarried. [1] The former quarry site was used for greenhouses before being redeveloped for housing.
36°55′45″S 174°50′47″E / 36.929208°S 174.846468°E
![]() | This article includes a list of general
references, but it lacks sufficient corresponding
inline citations. (February 2018) |
McLennan Hills (also Te Aponga o Tainui) is one of the volcanoes in the Auckland volcanic field. It was a group of cratered scoria mounds up to 45 m high, before it was quarried away. A 1940 aerial photo (in Searle's book) shows a crater around 100 m wide, one around 50 m wide, and 2 or 3 smaller craters. McLennan Hills, alongside neighbouring Ōtāhuhu / Mount Richmond, were the sites of fortified pā in pre-European times, important due to their location between the Waitematā Harbour/ Tāmaki River and the Manukau Harbour. [1] Since the European settlement of Auckland, the scoria cone was quarried. [1] The former quarry site was used for greenhouses before being redeveloped for housing.
36°55′45″S 174°50′47″E / 36.929208°S 174.846468°E