Groundwater probe $100.00 per day Rain gauge calibration $300.00 per deployment Automatic water quality samplers $50.00 per day Hydrological gauging equipment (wading) $60.00 per gauging Hydrological gauging equipment (M9) $120.00 per gauging Datalogger $160.00 per year GPRS telemetry $30 per month Radio telemetry $10 per month Repair Parts (battery/fuse/cable) $50 per deployment Bertrand Rd hydrology equipment $750.00 per year Lake Rotorangi telemetry $1,752.00
Recount in 1990. 100-year flood protection and takes into account the effects of climate change. The aim has been to make the scheme as resilient as possible. A one-in-100-year flow at Waitara is estimated at around 3,800 cubic metres per second, which is more than twice the highest flow measured at 1,640 cubic metres during the heavy rain event on 20 June 2015 (picture). A one-in-100-year flood would be about three metres higher, with a substantially higher
highest 24-hour rainfalls in New Zealand. A combination of intense rainfall and small catchments with hilly topography means the region’s rivers can rise very rapidly. New Zealand has a relatively high number of landslides compared with other countries. Fortunately, the country’s low population density and settlement patterns mean there are few landslide deaths and comparatively limited damage. Heavy rain causes erosion and bank collapse in Mākāhu in the Stratford District.
Trustpower Mangorei hydro scheme consent monitoring report - Taranaki Regional Council.
approximately 2.1 ha in size and is comprised of a cutover lowland tawa dominant forest remnant on hill slopes and stream terraces. The remnant is of a native forest type that is classified as 'Chronically Threatened' in Taranaki and falls within 'Acutely Threatened' Land Environment (LENZ) F5.2a. Remnants such as this provide important habitat for rare and threatened species. Gillett Family Bush also offers good connectivity to other nearby habitats, private QEII covenants and Key Native Ecosystems in
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
Council meeting agenda June 2021
suitable for classes of up to 35 students unless otherwise stated. Activities available at both the Tupare Riverside School and the Hollard Gardens Woodlands School. In addition to activities 1-4, the following activities are available at the Hollard Gardens Woodlands School. page S ITE 20 ISSUE NO.MAY 16 77 Autumn leaf fall (30-40 minutes, only during autumn) This lesson outlines the importance of this natural process to the Tupare garden landscape.
to say that a well-managed composting operation should produce little or no leachate and the only liquids leaving the composting pads should be stormwater runoff from the composting piles and the operating area including tracks and the truck wash. 19. Both Pads 1 & 3 and the operational areas are engineered so that all stormwater that falls on these areas is captured and diverted into the irrigation pond. 20. As described in the previous paragraph all the contaminated
page Policy and Planning Committee Tuesday 17 July 2018 10.30am Taranaki Regional Council, Stratford page Agenda for the meeting of the Policy and Planning Committee to be held in the Taranaki Regional Council chambers, 47 Cloten Road, Stratford, on Tuesday 17 July 2018 commencing at 10.30am. Members Councillor M P Joyce Councillor B K Raine Councillor C S Williamson Councillor D L Lean (ex officio) Representative Mr J