flat; no debris noted 2.74 1.50 39 19.06.17 0920-1015 Cloudy, foggy, recent rain Calm 10.0 11.4 Turbid, brown; surface flat; no debris noted 1.90 1.45 38 L3 20.10.16 1105-1205 Overcast, fine Moderate 16.3 16.3 Clear, green; surface ripple; no debris noted 2.06 1.43 52 20.02.17 1125-1220 Overcast, fine Calm 21.6 21.6 Clear, v. dark green; surface flat; no debris noted 4.06 2.89 52 22.03.17 0940-1030 Overcast, rain Calm
of beach (at low tide only), any waters emerging from the cliff would be swiftly mixed and dispersed. Any effects on groundwater quality or coastal water quality would be negligible. In general the creation of stable interlocked layers of green waste ensures that it does not fall off or get blown off the cliffs and down onto the coastal marine area or into the sea. The effect of the sand movement from the lack of dune systems has seen the degradation in the land available for farming on
Policy and Planning Agenda 19 March 2024
protected from stock damage. 25 June 2015 A follow-up inspection of the site was carried out in fine weather with calm wind conditions, following heavy rain five days prior to the inspection. The inspecting officer walked across the cap. It was noted that the cap was moist, but intact, with no ponding observed. The stormwater diversion drain through the centre of the cap showed evidence of overland flow, but no damage to the cap was noted. The grass cover showed evidence of stock grazing, but
Inspections 7 September 2016 An inspection was conducted in overcast weather with rain showers and north westerly wind conditions. The influent screen was tidy and wastes were fully contained. The primary pond influent flow was reasonably clear with an estimated flow rate of 3 L/s. the pond was a turbid, light green brown colour with a rippled surface. page 11 The secondary pond was slightly turbid and a light green brown colour with a rippled surface. An algal sample was
staying at Konini Lodge at Dawson Falls. The Kaupokonui Stream has its source close to Dawson Falls with several sites nearby suitable for study. At a later date, many school groups study the same river at several other sites along its course. Data collected at each study is then presented in various ways showing the health of the river at its different points. Other rivers such as the Waiaua River (west Taranaki) and the Waiwhakaiho River (north Taranaki) have suitable
and subtidal habitats. Sedimentation has a major influence on the region’s estuaries, the factors behind which include rain fall and modified land use. The large number of rivers and the erosion of Mount Taranaki generally bring a lot of sediment to the coast. However, the high energy coastline means this sediment supply does not settle long enough to greatly assist with the beach building process. Active dunelands exist at some of the larger river mouths and dominate the
to the reservoir levels falling below 80%. In all of these instances CCCWSL advised Council and affected parties of this requirement, as per their consent conditions. However, one of these instances CCCWSL went over and above their 79 L/ s for 24 hours (with permission from Council) to ensure they continued to provide water to their community while they were fixing a mains pipe burst. An abatement notice was issued for this event and is discussed in Section 2.2. Figure 2 shows CCCWSL’s
Todd Petroleum Ltd Mangahewa D Hydraulic Fracturing Report 2022-2023