| Te Puke | |
|---|---|
| Te Puke monogenetic basaltic scoria cones (red marker) and lava field. Clicking on the map enlarges it, and enables panning and mouseover of volcano name/wikilink and ages before present. Key for the volcanics that are shown with panning is: basalt (shades of brown/orange), monogenetic basalts, undifferentiated basalts of the Tangihua Complex in Northland Allochthon, arc basalts, arc ring basalts, dacite, andesite (shades of red), basaltic andesite, rhyolite, (ignimbrite is lighter shades of violet), and plutonic. White shading is selected caldera features. | |
| Highest point | |
| Elevation | 136 m (446 ft) |
| Coordinates | 35°15′07″S 174°01′48″E / 35.252033°S 174.029961°E / -35.252033; 174.029961 |
| Geology | |
| Rock age | Pleistocene |
| Mountain type | Basaltic scoria cones |
| Rock type | Basalt |
| Last eruption | c. 1,300 years ago |
Te Puke is a 136 metres (446 ft) high group of basaltic scoria cones, in the Kaikohe-Bay of Islands volcanic field in Northland, New Zealand. It is the easternmost volcano of the field, being located near Waitangi. The three or four small, cratered cones are in a southwest–northeast alignment. The last eruption was 1300 to 1800 years ago.
References
- "Kaikohe-Bay of Islands". Global Volcanism Program. Retrieved 11 August 2012.
- Hayward, Bruce; Smith, Ian (2002). "Field Trip 7: A Taste of Northland Geology" (PDF). In Smith, Vicki; Grenfell, Hugh (eds.). Field Trip Guides, GSNZ Annual Conference "Northland 2002". Geological Society of NZ Miscellaneous Publication 112B. Retrieved 28 March 2012.
External links
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