community, in a report of October 2018. The TRC, in collaboration with
NPDC has now requested BERL to complete comparisons of the potential future values of the 8
Options proposed. These have been studied and planned by architects and engineers locally: by
Elliott Architects, TSE Taranaki, Calibre Consulting and BCD Group. BERL assessed the options using
the same approach as used in the 2018 retrospective study of the previous shape of Yarrow Stadium.
Our approach here is to
Greenwaste Composting & Vermiculture
Water may need to be added at this stage. The completed windrow is then
numbered and is entered onto a chart for monitoring purposes (refer example
windrow monitoring sheet & plan Appendix 1).
1.2.4. Windrow monitoring and operational procedure
Temperature testing of the windrows begins four to nine days after they have been
formed. When the temperature reaches between 60-70 degrees Celsius the windrow
is turned from the outside to the middle
vouchers before you travel to a region where an
electronic card is not available.
› Contact the regional council at least 10 days before a planned trip, which will allow time for
vouchers to be posted if required.
› When travelling in another region please advise the driver you are from out of town and are
using a card and/or vouchers from your home town.
› You must present your total mobility card and/or vouchers to the driver at the start of the
trip.
Restrictions to the Total
redevelopment work planned in
that area is completed. Solid lines indicate line lengths currently able to be monitored. Dashed lines
can be monitored when instruments are installed at Dawson Falls. The base map is from Google
Earth.
page
Confidential 2017
GNS Science Consultancy Report 2017/142 14
Figure 7.2A The displacement of the GNSS site PGKH at Kahui Hut on Mt Taranaki for 2014 to 2017.
Displacements in the north-south (dn), east-west (de), and up-down (du)
intention is to also install a site at Dawson Falls once redevelopment work
planned in that area is completed. Solid lines indicate line lengths currently able to be monitored.
Dashed lines can be monitored when instruments are installed at Dawson Falls. The base map is
from Google Earth.
page
Confidential 2016
GNS Science Consultancy Report 2016/139 13
Figure 7.2 The displacement of the GNSS site PGKH at Kahui Hut on Mt Taranaki. Displacements in the
north-south
Umbrella: regional sustainability – requires information sharing
6
Coordination is critical through regional plan that structures the efforts of stakeholders – everyone knows
what the collective goals and priorities are
6 Person to collate information in a centralised database
6 Annual biodiversity forum
6 Advocate for increased central government support
6 Policy
7 Support admin for smaller groups
7 Support smaller projects that are successful and grow them
7 We don’t
of the western portion of the North Island of
New Zealand. No deformation of the volcano is apparent in the data collected so far.
page
Confidential 2015
GNS Science Consultancy Report 2015/132 13
Figure 6.5 Locations of GNSS sites on or near Mt Taranaki. Sites are labelled by their 4-letter site codes.
NPLY is New Plymouth, PGKH is Kahui Hut and PGNE is North Egmont. The intention is to also
install a site at Dawson Falls once redevelopment work planned in
responsible for processing data
recorded by the network from January 1994 until June 1997. These data were regularly
reported to Taranaki Regional Council (TRC), and data from the period January 1994 to
March 1995 were summarised in Cavill et al. (1997). In July 1997, GNS Science took over
responsibility for data analysis and annual reporting under contract to TRC.
In 2001, the GeoNet project started to improve the existing network for monitoring
earthquakes in New Zealand. In 2005, planning
performance of resource users against regional plans and consents. Compliance
monitoring, including impact monitoring, also enables the Council to continuously
assess its own performance in resource management as well as that of resource users
particularly consent holders. It further enables the Council to continually re-evaluate
its approach and that of consent holders to resource management, and, ultimately,
through the refinement of methods, to move closer to achieving sustainable
development of
1995 were summarised in Cavill et al. (1997). In July 1997, GNS Science took over
responsibility for data analysis and annual reporting under contract to TRC.
In 2001, the GeoNet project started to improve the existing network for monitoring
earthquakes in New Zealand. In 2005, planning began for upgrading seismographs in
Taranaki to an equivalent standard to that in other parts of New Zealand. With this upgrade
came two important changes. Firstly, the role of the network expanded from