Napier-Hastings

Napier map

Geological Summary

The geology of the Napier-Hastings area is dominated by Late Quaternary alluvial and marine sediments forming the Heretaunga Plains. These overlie older Quaternary sediments that are exposed in lower hills and these in turn overlie Pliocene alternating mudstone, sandstone and limestone.

Maps and Information

The Napier-Hastings urban and urban fringe areas are part of a current geological mapping initiative that has completed a new geological map, and will complete a geomorphological map and a 3D geological model in late 2020.

Urban Maps

2020: Geology of the Napier-Hastings urban area

This 1:75 000 scale map provides updated geological mapping for the Napier-Hastings urban areas. New information includes detailed mapping of Pliocene–Quaternary-age rocks in the hills northwest of Napier and the Ngaruroro River, new formations introduced to encompass Holocene river and marine deposits, and revision of surficial and sub-surface traces of potentially active faults.  The map provides geological context for the landscape features within this dynamic part of North Island’s east coast.

Rocks present in the map area record the development of the Hikurangi subduction margin and deformation associated with it.  The oldest rocks present are Eocene to Miocene-age deep-marine mudstone and sandstone, distributed in fault-controlled northeast–southwest-trending strips east of Havelock North.  Pliocene- to Quaternary-age shallow-marine limestone, mudstone, and sandstone overlie the Miocene rocks and form the hill country that immediately surrounds the Napier-Hastings urban areas.  Conglomerate, pumiceous sandstone, carbonaceous mudstone, and volcaniclastic deposits of early to middle Quaternary age, are preserved at Cape Kidnappers, south of Havelock North, and as isolated remnants on hilltops west of Napier. Middle to late Quaternary alluvial fan and marginal-marine sediments were deposited by rivers and coastal processes. The Awanui and Tukituki faults are steeply-dipping reverse faults with surface traces exposed in the south of the map area but are buried beneath the plains farther north.

A pdf version of the geological map can be downloaded for free from the Online Shop. The digital geological data also can be accessed via ArcGIS Server web services. GIS layerfiles that reference and symbolise the web service layers are available for use in ArcGIS (ArcMap and ArcGIS Pro) and QGISMetadata describing the various geological data are also available.

To view the Napier-Hastings geological map in more detail use this link or click on the image above.

  • Lee JM, Begg, JG, Bland KJ. 2020. Geological map of the Napier-Hastings urban area. GNS Science geological map 7a. GNS Science, Lower Hutt, NZ.

Other Information

2011/2018: QMAP 1:250 000 geological map

For wider and more generalised geological context of the Napier-Hastings area, a 1:250 000 geological map was printed with accompanying explanatory text. Digital GIS and image versions of the map are available on DVD. The digital version has since been updated in a national GIS dataset at that nominal scale. The underlying GIS datasets have rich feature attributes.

  • Lee, J.M.; Bland, K.; Townsend, D.B.; Kamp, P.J.J. (compilers) 2011. Geology of the Hawke’s Bay area. Institute of Geological & Nuclear Sciences 1:250 000 geological map 8. Lower Hutt, New Zealand. Institute of Geological & Nuclear Sciences Limited.  93 p. + 1 sheet.
  • Heron, D.W. (custodian) 2018. Geological Map of New Zealand 1:250 000. GNS Science geological map 1 (2nd edition). Lower Hutt, New Zealand. GNS Science.
Napier

For more information on the 1:250 000 Geological Map of New Zealand visit its web page.

1970: 1:63 360 Napier and Hastings-Kidnappers geological map

The city area of Napier-Hastings is covered by a 1:63,360 geological map published in 1970 (Kingma 1970). This is a printed map with limited accompanying text and no digital equivalent.