backwash is discharged via a large pond. The outlet from the pond is an inverted pipe located at the
opposite end of the pond from the inlet. The discharge from the pond emerges from a pipe to fall over a
small waterfall. At the base of the waterfall the discharged water runs down a natural cobbled channel
beneath native riparian vegetation for approximately 10 metres before entering the Patea River,
downstream of the intake weir.
1.2.2 Midhirst water supply
The Midhirst community WTP
Groundwater quantity monitoring report 2015-2017
opportunity arises (i.e. as
review dates in the consent fall due, if review is not possible otherwise) and, as appropriate, impose conditions
consistent with the more recent consents.
page
P A T T L E D E L A M O R E P A R T N E R S L I M I T E D 5
R E V I E W O F P E T R O L E U M W A S T E L A N D F A R M I N G
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5.1
emission from the plant are a boiler for hot water production,
the stockyards, the effluent ponds, the effluent irrigation system, and miscellaneous
plant processes.
1.3 Resource consents
1.3.1 Water abstraction permit
Section 14 of the Resource Management Act stipulates that no person may take, use,
dam or divert any water, unless the activity is expressly allowed for by a resource
consent or a rule in a regional plan, or it falls within some particular categories set
out in
Pest Pathways into Taranaki - June 2020
Freshwater ecological monitoring state of the environment report - Taranaki Regional Council.
Freshwater ecological monitoring state of the environment report - Taranaki Regional Council.
Policy and Planning Agenda March 2023 Web
the way of intertidal 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
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 low-lying
coast from Pātea Beach to the southern extent of the region. Cliff-top