Council meeting agenda June 2021
Council meeting agenda June 2021
Council meeting agenda June 2021
noted that seven intakes were now in place along the roofline of shed 3, that these included fittings for shed air recirculation as at Midhirst, and that the boilers had been installed and hot water radiators were being piped up inside each shed. 27. Osflo arrived about 10.45 am, and were to begin by emptying shed 4. With rain setting in, I considered there would be little gain in continuing to monitor odour, and left the site about 11 am. 28. My observations on this occasion:-
Ordinary Council Agenda October 2024
Centre city for a coffee and then home again. This is my usual route with my 2 year old daughter who sits comfortably (she falls asleep sometimes) in the chair on the back. It's an e-bike and I travel about 25 - 35 km Comments noted. While the comments are not particularly related to the Plan we will pass the submitters comments on to NPDC as they are more relevant to the activities they manage. We would also encourage the submitter to raise their concerns/ideas …
occasions during 2019-2020 Date Lake level (m asl) Weather Wind Lake appearance L2 L3 L2 L3 17 October 2019 75.7 Broken cloud, fine Light NW Moderate NW Turbid, brown; surface rippled Slightly turbid, dark green; surface rippled 19 February 2020 77.3 Overcast, drizzle; heavy rain preceding Calm Calm Clear, dark green; surface flat Clear, dark green; surface rippled 19 March 2020 76.8 Overcast, light rain Light NW breeze Calm …
extended-duration nuisance blooms reflecting high nutrient enrichment and/or significant alteration of the natural flow regime or habitat. * The productive class is defined by River Environment Classification (REC) types, with a combination of dry climate categories and soft-sedimentary, volcanic acidic and volcanic basic geology. All sites that do not fall in these categories are in the default class. 1.3 Periphyton Periphyton is the ‘slime’ and algae found on the beds of lakes and rivers. This
page 25 Discussion 4. The chemical composition of groundwater is determined by a number of influences. These include the mineralogy of the soil and rock types forming catchments or aquifers, aquifer structure, the source and volumes of recharge water, aquifer residence times, overlying landuses and biochemical process. Groundwater aquifers in Taranaki are predominantly recharged by rainfall falling on the land surface, but recharge can also occur via infiltration from
we are conservatively forecasting port dividend returns of $8m a year over the life of the LTP. Our biggest financial risk is port dividends falling below forecast levels. Any circumstance that reduces the level of dividend will result in a commensurate increase in the level of general rates. We intend utilising our Dividend Equalisation Reserve, built up from years when dividends exceeded forecasts. This fund will be drawn upon to help minimise rates increases in the first few
29 7.7 Ngatoro 3 0.8 Waiwakaiho Audrey Gale Park 25 6.6 Puketapu 3 0.8 Lake Rotokare 23 6.1 Puniho 3 0.8 Lake Rotorangi 21 5.6 Dawson Falls 3 0.8 Wai-iti 20 5.3 Waiaua 3 0.8 Onaero 20 5.3 Kaweroa 2 0.8 Tongaporutu River 18 4.8 Kapuni Stream 2 0.5 Waiwhakaiho Meeting of the waters 17 4.5 Whenuakura River 2 0.5 Lake Opunake 17 4.5 Egmont National Park 2 0.5 Waitara beach 16 4.3 Greenwood Rd 2 0.5 Huatoki 16 4.3 Makatawa River 2 0.5 Oakura
Dow AgroSciences consent monitoring Annual report 2016-2017