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Report 2014-2015

exploration site located on Rimutauteka Road at Waitui, in the Waitara catchment. The site is called Mangahewa-D wellsite. This report covers the period from August 2014 to December 2015. During this period, four wells (MHW-21, 22, 23, and 24) were drilled and tested. The hydraulic fracturing programme is ongoing. This report describes the monitoring programme implemented by the Taranaki Regional Council (the Council) to assess the Company’s environmental performance in relation to drilling

Interim Review of the Regional Policy Statement for Taranaki 2010

page page (THIS PAGE IS INTENTIONALLY BLANK) page Final report on Interim review of the Regional Policy Statement for Taranaki 2010 Evaluation of appropriateness, efficiency and effectiveness Taranaki Regional Council Private Bag 713 Stratford June 2017 Document number: 1847085 page (THIS

Todd Energy McKee production station consent monitoring 2017-2018

page Todd Energy Ltd McKee Production Station Monitoring Programme Annual Report 2017-2018 Technical Report 2018-71 Taranaki Regional Council ISSN: 1178-1467 (Online) Private Bag 713 Document: 2149930 (Word) STRATFORD Document: 2180894 (Pdf) March 2019 page page Executive summary Todd Energy Ltd operates a petroleum

Greymouth Petroleum northern sites consent monitoring 2017-2018

June 2033 1.3.1 Water discharge permits Section 15(1)(a) of the RMA stipulates that no person may discharge any contaminant into water, unless the activity is expressly allowed for by a resource consent or a rule in a regional plan, or by national regulations. GPL holds water discharge permit 6498-1 for the northern section of the site, to discharge treated stormwater and treated produced water from hydrocarbon exploration and production operations at the Turangi Production Station

TAG Oil (NZ) Ltd groundwater monitoring report 2013

effects from hydraulic fracturing or other hydrocarbon exploration and extraction activities, upon shallow groundwater or surface water in the vicinity. The investigation indicated that the Company demonstrated a high level of environmental performance and compliance with the resource consents and with the provisions of the Council’s Regional Fresh Water Plan for Taranaki (2001), in respect of the matters under investigation. This report includes recommendations concerning the nature of

Report 2011-2014

further hydrocarbon exploration located on Brookes Road, within the Stratford district, in the Waingongoro catchment. The site is called Cheal-C wellsite. This report covers the period from April 2011 to July 2014. During this period, four wells were drilled and tested (C1, C2, C3 and C4), and one well drilled, tested, and hydraulically fractured (Cardiff-3). This report for TAG Oil (NZ) Limited describes the monitoring programme implemented by the Taranaki Regional Council (the Council) to

May 2025 climate summary

average air temperature for the region (excluding Te Maunga sites) was 12.7°C, which is 0.4°C warmer than long-term May averages. The maximum air temperature recorded in May was 21.7°C at Waitōtara at Hawken Rd on 14 May. May average wind speeds were 12.6km/hr, with average gust strength of 41.7km/hr, these were 0.2km/hr lighter, and 0.7km/hr gustier than the long-term average. The maximum wind gust recorded in May was 91.9km/hr at Taungatara at Eltham Rd on 18 May. TRC Climate Summary May 2025 May

Taranaki Regional Council Biosecurity Strategy

page Taranaki Regional Council Biosecurity Strategy 2018 – 2038 Taranaki Regional Council Private Bag 713 Stratford February 2018 Document number: 1908587 page (THIS PAGE IS INTENTIONALLY BLANK) page i At a glance Our vision Taranaki has a high performing,

Annual report 2012-2013

explored and commercially successful hydrocarbon producing area in New Zealand. Oil and gas exploration and development has been on-going in the region for nearly 150 years. Since the first well in 1865, over 600 exploration and production wells have been drilled. While the majority of the basin is offshore, the majority of the producing wells are onshore. The geology of the basin is derived from diverse episodes of tectonic activity. The Cretaceous to Quaternary basin fill is up to 9,000 m