incised nature of ring plain streams means that flooding is not a major problem. However, occasional intense rainfall events can lead to rapid rises in river levels and flooding in hill country valleys and elsewhere. Figure 2: The Taranaki Region page 16 2017/2018 Annual Report THE PEOPLE Figures from the 2013 census show the total population of Taranaki stands at 109,608, an increase of 5.3% over the 2006 census figure. In the previous
are few areas of sheltered water beyond the major estuaries such as the Tongaporutu, Waitara and Patea rivers, and the confines of Port Taranaki. The Taranaki region has a temperate climate with generally abundant rainfall. The incised nature of ring plain streams means that flooding is not a major problem. However, occasional intense rainfall events can lead to rapid rises in river levels and flooding in hill country valleys and elsewhere. Figure 2: The
Tongaporutu, Waitara and Patea rivers, and the confines of Port Taranaki. The Taranaki region has a temperate climate with generally abundant rainfall. The incised nature of ring plain streams means that flooding is not a major problem. However, occasional intense rainfall events can lead to rapid rises in river levels and flooding in hill country valleys and elsewhere. Figure 2: The Taranaki Region page 18 2016/2017 Annual Report THE PEOPLE
Tongaporutu, Waitara and Patea rivers, and the confines of Port Taranaki. The Taranaki region has a temperate climate with generally abundant rainfall. The incised nature of ring plain streams means that flooding is not a major problem. However, occasional intense rainfall events can lead to rapid rises in river levels and flooding in hill country valleys and elsewhere. THE PEOPLE Figures from the 2013 census show the total population of Taranaki stands at
NPDC Colson Road Landfil consent monitoring report 2016-2017. l
rainfall events can lead to rapid rises in river levels and flooding in hill country valleys and elsewhere. THE PEOPLE Figures from the 2013 census show the total population of Taranaki stands at 109,608, an increase of 5.3% over the 2006 census figure. In the previous census period (2001-2006) the population of the region increased by 1.2%. Taranaki’s population accounts for 2.6% of New Zealand’s total population. Population changes have also varied
sulphide (H2S) was detected but the source could not be located. No odours were detected at the downwind boundary of the site. The cap on the closed areas of the landfill (stages 1 & 2) was in good condition and no issues were noted. The following action was to be undertaken: Continue with litter collection 8 September 2015 This site inspection was carried out in dry weather with light, variable wind conditions. There had been only 2.5 mm of rainfall within the previous two days.
Taranaki By-Products Ltd consent monitoring report - Taranaki Regional Council.
rainfall preceding sampling. Figure 3 Ammoniacal nitrogen concentration of the Inglewood landfill stormwater/leachate (RTP002005) for monitoring to date 2.2.3 Results of receiving environment monitoring Chemical analysis Receiving water sampling was undertaken at sites AWY00103, AWY100105, AWY000100, AWY000107 and AWY000115 on two occasions (23 November 2020 and 2 February 2021). The locations of these monitoring sites are shown in Figure 2 and the results of the chemical
a relatively shallow water table. Test bores were augured to 10 m in the pit area, revealing extensive compacted, low permeable clays underlying coastal dune sands. Pit construction revealed mostly tightly packed sand at the pit bases (approximately 4-5 m below surface). Average annual rainfall for the site is 1,023 mm (taken from the nearby ‘Duffy’ monitoring station). As with the other South Taranaki coastal sites, this site is subject to strong winds. Photo 3 Landfarming area M2110