DISTRIBUTION, BREEDING AND FEEDING Banded kokopu are primarily a lowland species but can penetrate up to 180km inland, and to elevations of 550m. This has allowed them to establish some landlocked populations in lakes in central New Zealand. They are exceptional climbers and can scale steep falls to reach higher catchments. Preferred habitats for adult banded kokopu are small tributaries with plenty of forest cover. Unlike other kokopu, they don’t seem
range of specific resource consent compliance programmes. We have also committed to permanent iwi representation on the Council’s two main standing committees. This is currently being progressed through Treaty of Waitangi settlement legislation. There are eight iwi whose rohe or tribal area falls either wholly or partially within the Taranaki region.
memory Limited discordant elements disrupt the distinctive pattern of boulders along the river bed channel Transient values Hangatahua (Stony) River catchment is exposed to some of the heaviest rain in New Zealand with rocks rolling down the river in accelerated river flows frequently changing its course At other times the river is recognised for having waters so clear that it appears that it isn’t there, however this has declined in more recent years due to natural erosion
the distinctive pattern of boulders along the river bed channel Transient values Hangatahua (Stony) River catchment is exposed to some of the heaviest rain in New Zealand with rocks rolling down the river in accelerated river flows frequently changing its course At other times the river is recognised for having waters so clear that it appears that it isn’t there, however this has declined in more recent years due to natural erosion higher up the catchment in Egmont National
the distinctive pattern of boulders along the river bed channel Transient values Hangatahua (Stony) River catchment is exposed to some of the heaviest rain in New Zealand with rocks rolling down the river in accelerated river flows frequently changing its course At other times the river is recognised for having waters so clear that it appears that it isn’t there, however this has declined in more recent years due to natural erosion higher up the catchment in Egmont National
managed. Minimal flaring was being undertaken with no resulting smoke or odours. No discharge was occurring from the skimmer pits but recent rain had elevated suspended solids content in the stormwater which may have required the pits to be cleaned out. 29 October 2012 No drilling was being undertaken at the time of inspection. Most of the exploration equipment had been moved to Cheal-B and C wellsites. The production facilities were neat and tidy. There was no discharge off site. Some silt
bubbling, though not odorous. A concrete apron had been constructed beside the first pond for easier wash-down and odour control. The storm drain pond beside the bio- filter was emitting a slight sulphurous odour. More trees had been removed along the front fence of the house opposite, which was now plainly visible. 12 July 2012 A routine inspection was carried out on 12 July 2012. Gentle very light rain stopped during the inspection. There was a light NE wind. An odour survey along Hursthouse
requirement of consent 9608, held by DR Wilson for abstraction of groundwater at a location across the Waitotara River for irrigation of pasture land. Consent 9608 requires that abstraction ceases if the water levels in the Silver Fern Farms supply bores GND0585 and GND1195 fall below 104 and 109 m respectively. Consent 2261-3.1 requires that the Company record continuous water level data, to an accuracy of ±10 mm in a dedicated monitoring bore and any operational abstraction bores. The
management area within which it falls, except as follows: (i) rules referenced with a `G' apply to the entire coastal marine area except as otherwise stated; and (ii) rules for activities that fall within more than one coastal management area are dealt with as described in Section 4.2.4. 4.1.2 Planning Maps The following maps show the location of all coastal management areas. The location of the coastal marine area boundary at rivers with non-standard "mouths" is also shown where those rivers
water level and flow of the Ngatoro Stream at SH3. By using a correlation between these two sites, a calculated flow can be estimated for the ‘Bushline. Based on this correlation, as shown in Figure 4 the flow did not fall below the 134 L/s limit, so no restrictions were required to be put in place. Figure 4 Calculated flow for Ngatoro Stream at Bushline during 2022-2023 Jul-2022 Sep-2022 Nov-2022 Jan-2023 Mar-2023 May-2023 0 1 2 3 4 5 6 7 8 9 10 11 12