low $0.15/kg-DM, average
$0.20/kg-DM and high $0.30/kg-DM. For mapping purposes the marginal benefits of
irrigation were categorised into four levels; low <$150/ha, medium $151-300/ha, high
$301-500/ha and very high >$500/ha.
The results of these assessments are shown in the following three figures:
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Taranaki Irrigation Study – Final Report 4
Figure 1: Irrigation development potential for low pasture price of $0.15/kg-DM
Figure 2:
settlements in the
rohe, such as Ngā Motu and the Waitara River, were on the coast. The papakainga was
the centre of social, cultural, economic and spiritual well-being. Papapakainga such as
Puke Ariki, Purakau, Rewa Rewa and Mangatī were located on the coast close to the
valued resources of water, mahinga kai and kaimoana. The resources sustained and
nourished the iwi and were important to ensure survival and to maintain the spiritual,
cultural and economic prosperity of Te
adopted by this Council under various legislative frameworks
including, but not restricted to, the Local Government Act 2002 and the Land Transport
Management Act 2003.
Iwi considerations
25. This memorandum and the associated recommendations are consistent with the
Council’s policy for the development of Māori capacity to contribute to decision-making
Regional Transport Committee - Key Functions and Terms of Reference for RTC and RTAG
13
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processes (schedule 10 of the
rainfall maps What you should know: The site maps show data from a selection of the sites we monitor, but not all of them. The distribution maps are based on mathematical modelling and may not accurately represent actual rainfall in some unmonitored areas. Click on each map for larger version. MONITORED SITES RAINFALL DISTRIBUTION Related links Monthly rainfall norms Current monitoring data
Plain FMU (green) sitting within the broader Taranaki region. 1
Figure 2 Indicative land use map for the Volcanic Ring Plain FMU. 3
Figure 3 Draft Freshwater Management Unit designations for Taranaki. 5
Figure 4 Ammonia modelling. 11
Figure 5 Nitrate modelling 11
Figure 6 Dissolved reactive phosphorus modelling. 11
Figure 7 Suspended fine sediment modelling 11
Figure 8 Consented surface water abstraction 12
Figure 9 Deposited fine sediment modelling. 13
Figure 10