1: Structure of Better Travel Choices for Taranaki ........................................................................................................ 5 Figure 2: New Plymouth Citylink urban route map ................................................................................................................. 11 Figure 3: Connector service and timetable
page page page page page page page page page page page page page page page page Table of contents Map features Source & reliability of data Comparisons with national levels and contaminated site guidelines Chromium map Copper map Lead map Nickel map Vanadium map Zinc map
NPDC New Plymouth WWTP Annual Report 2022-2023
clearly highlights there was an urgency to activate the process, then quickly recommended by Colin McLellan on the 7/1/19. Under Question 3 of the process “Statutory Acknowledgements “The Iwi impacted on is not acknowledged, Ngaati Mutunga, this is in breach of Treaty Principles of “Partnership“, ”Protection of Taaonga” and being accorded the appropriate rights to the Mana Whenua of this area. No level of contamination is and ever will be acceptable into these waterways. These awa present
Commentary Sites of significance to Māori within the CMA Values associated with sites Map reference TRC Number Description Tāngāhoe River The Tāngāhoe River has been a major supply of food and water resources to its people both prior to and since the arrival of the Aotea Waka. The valley like the rest of the southern lands was a fertile paradise and because of the mild temperatures, promoted lush vegetation that was checked only by the occasional equinoctial weather
...........................................................................................................6 8.0 REFERENCES .............................................................................................................6 FIGURES Figure 1. A map of the seismographs used to locate earthquakes in Taranaki. ................................................8 Figure 2. A map of all earthquakes located in Taranaki between July 2009 and June 2010.............................9 Figure 3. A map of earthquakes less than 50 km deep located in Taranaki between July 2009 and June 2010.
........................................................................................................... 6 FIGURES Figure 1. A map of the seismographs used to locate earthquakes in Taranaki. ................................................ 8 Figure 2. A map of all earthquakes located in Taranaki between July 2010 and June 2011. ............................ 9 Figure 3. A map of earthquakes less than 50 km deep located in Taranaki between July 2010 and June 2011.
........................................................................................................... 6 FIGURES Figure 1. A map of the seismographs used to locate earthquakes in Taranaki. ................................................ 8 Figure 2. A map of all earthquakes located in Taranaki between July 2011 and June 2012. ............................ 9 Figure 3. A map of earthquakes less than 50 km deep located in Taranaki between July 2011 and June 2012..
Taranaki Rivers black disc visibility (the field procedure used to measure visual clarity) were calculated for each river segment in the region. Table 7 below shows the percentage of stream length of each FMU within each attribute band using modelling data with a map of the results presented in Figure 4. Table 7: Percentage of stream length within each FMU with each suspended sediment attribute band based on modelled results from Fraser (2022). Attribute band Southern
Agenda for Ordinary Council meeting May 2017.