Ministry of Economic Development Home| Contact MED|


 
 
 

Links to this page were:

Section Subnavigation Links:

Existing and Potential Geothermal Resource for Electricity Generation


[ Last Updated 17 January 2006 ]
Short Description This note provides information on New Zealand's existing and potential geothermal resource for electricity generation. This information is intended to supplement the Ministry's project to identify waterbodies of national importance in relation...

Author Matthew Hall, Policy Analyst, Resources and Networks Branch

1 April 2004

Contents

1. This note provides information on New Zealand's existing and potential geothermal resource for electricity generation. This information is intended to supplement the Ministry's project to identify waterbodies of national importance in relation to existing and potential hydro generation.

Existing Geothermal Electricity Generation

2. The majority of New Zealand's geothermal generating capacity is situated in the Taupo Volcanic Zone in the upper North Island. In this region over 400MW of plant has been installed. Another 9MW has been installed at the top of the North Island with plans to expand this plant further. Geothermal generation accounts for approximately 7% of New Zealand's total electricity generation.

3. Figure 1 shows the location of high temperature geothermal fields in the North Island of New Zealand. Table 1 shows a summary of existing electricity generation by geothermal field.

Figure 1: High Temperature Geothermal Fields in New Zealand

Figure 1: High Temperature Geothermal Fields in New Zealand

Source: CAE: New Zealand's Energy Future, August 2003.

Table 1: Existing Electricity Generation by Geothermal Field
RankGeothermal field nameTotal installed capacity (MW) Annual electricity production1 (GWh)Number of power plants% of GWhp.a.Nationally important at a threshold of 230GWh?
1Wairākei2201,734251.0%Yes
2Ohaaki104820124.1%Yes
3Mōkai55434112.8%Yes
4Rotokawa2822116.5%No
5Kawerau1511823.5%No
6Ngāwhā97112.1%No
TOTAL 4313,3988100% 

4. At a threshold of 230GWh per annum, the Wairākei, Ohaaki and Mōkai geothermal fields are considered nationally important in terms of existing electricity generation.

Potential Geothermal Energy Generation

5. Geothermal energy could make a significant additional contribution to New Zealand's generating capacity. Delays and uncertainties in the resource consent process and subsequent compliance costs have been identified as the biggest obstacles to investment.

6. Table 2 shows a summary of potential electricity generation by geothermal field. The table is based on opportunities deemed to have a high to medium probability of progressing by 2025. It is derived from information collected by East Harbour Management Services in their 2002 report Availabilities and Costs of Renewable Sources of Energy for Generating Electricity and Heat.

Table 2: Potential Electricity Generation (with a High to Medium Probability of Proceeding by 2025) by Geothermal Field
RankGeothermal field namePotential additional capacity (MW) Potential electricity production (GWhp.a.)% of GWhp.a.Nationally important at a threshold of 230GWh?
1Kawerau3572,81026.8%Yes
2Rotokawa3032,39022.8%Yes
3Wairākei1821,43013.6%Yes
4Ngātamariki21401,10410.5%Yes
5Mōkai977707.3%Yes
6Tauhara705505.2%Yes
7Mangakino3655124.9%Yes
8Ngāwhā645004.8%Yes
9Rotomā352802.7%Yes
10Tikitere-Tāheke10800.7%No
11Horohoro9700.7%No
TOTAL 1,33210,496100% 

7. At a threshold of 230GWh per annum, the Kawerau, Rotokawa, Wairākei, Ngātamariki, Mōkai, Tauhara, Mangakino, Ngāwhā and Rotomā geothermal fields are considered nationally important in terms of potential electricity generation. Note that the Wairākei field is considered nationally important in terms of both existing and potential electricity generation.


1In calculating annual electricity production, a load factor of 90% has been used.

2The East Harbour report gave ranges of electricity generation potential for the Ngātamariki and Mangakino geothermal fields. The lower thresholds of these ranges have been used in Table 2.

3See Note 2.





Back to Top