Harrow and Hillingdon Geological Society
The Volcanic History of Taranaki
Mount Taranaki /Egmont and the volcanoes to the north have been built by two million years of volcanic activity that has lasted from the early Pleistocene almost to the present day.
Prior to this, Taranaki was covered by a shallow sea, as evidenced by the seashell deposits of Eastern Taranaki, beneath which a sequence of sediments was deposited during the Tertiary. Oil and gas within these sediments gradually flowed upwards into structural traps where they could not escape to the surface; they have been subsequently drilled and commercially developed, e.g., at Kapuni and offshore Maui.
The lavas which have been extruded from the Taranaki volcanoes (Egmont, Pouakai, Kaitake and Paritutu) cover a comparatively small area, mostly at high altitudes. Below the 900m contour they merge into the ring plain. This has been constructed from collapses of pre-existing volcanic cones at each site. These
The outskirts of the Taranaki ring plains are bounded to the west by the coast and to the east by uplifted Tertiary mudstone and sandstone country. Over time, volcanic activity has moved from NNW to SSE in Taranaki, along an apparent major linear fracture in the Earth's crust. From north to south, the Taranaki volcanoes comprise:
• Paritutu Volcano – the spine of Paritutu on the New Plymouth foreshore and the nearby Sugar Loaf Islands, positioned slightly to the northeast of the principal volcanic line.
All these cones are composed of andesite lava flows . The Egmont andesite has feldspar and augite or hornblende crystals within a glassy matrix. In the central part of Kaitake volcano are diorites. Besides lava, each of the volcanoes also produced large thicknesses of tephra.