Communities
The proposal would
have a significant long-term detrimental impact on the amenity of people
living nearby and is therefore contrary to the provisions of NPPG6 and
SPP6 in this respect.
Dr Stuart Black
wrote in a letter to Stop Highland Windfarms Campaign: "I agree with
you that development that is judged to have significant long-term detrimental
impacts on communities or individual householders for that matter should
not be granted. Indeed, this is a fundamental aspect of the Council's
current planning policy."
Cumulative
Impact
Let us not repeat
the same mistake as the Causeymire windfarm where 4 turbines are too
close to the A9, causing disorientation, especially approaching them
round the bend travelling north. Turbines 8, 12, 15 and 16 of Halsary
windfarm would also be too close to the A9 but on the opposite side
of the road from the Causeymire windfarm and would distract whether
travelling north or south round the same bend. The experience of approaching
and driving through the combined developments would be one of oppression.
Figure
2.1 'Local Cumulative Developments' shows only too clearly the devastating
effect should Spittal and Halsary be added to the existing wind farm at
Causeymire. This is over provision on a massive scale and would be an
intolerable situation for the residents of Spittal.
From
the A99 North of Wick along the stretch from the Staxigoe Junction and
out past Tesco, the windfarms at Achairn and Bilbster are prominent with
the Causeymire Windfarm frequently clearly visible in the distance beyond
Bilbster. When Camster Windfarm is constructed it, seen along with Achairn,
will become the dominant feature in the landscape but there will be a
separation between that grouping and the Bilbster/Causeymire grouping.
If Halsary were to be constructed, there would be an unbroken array of
turbines on the horizon from Camster to Bilbster, occupying 30 degrees
of the view.
From the A9 Southwards
entering Spittal, there would be an unbroken array of turbines from
Camster to Causeymire with Buolfruich visible over the Causeymire turbines,
occupying 80 degrees of the view forward. Bilbster is visible to the
left of this grouping.
From the A9 travelling
northwards Buolfruich Windfarm is visible at Dunbeath and again shortly
after leaving Latheron Wheel. It remains prominent until it is passed,
before which Causeymire turbines come into view and remain in view until
leaving Spittal. North of Rangag, the Halsary turbines will appear as
a huge extension to Causeymire, further extending the windfarm experience
on the journey North.
From the East and
north east, the experience of the Causeymire Windfarm would be extended
and its density intensified by seeing Halsary turbines through and beyond
the Causeymire Windfarm.
Approaching Mybster
on the minor Road from Watten, Causeymire is already an industrial intrusion
on the views to Morven with turbines and pylons mingling on the skyline.
Halsary would
complete the industrialisation of the landscape seen from this direction.
The current level
of windfarms constructed in central Caithness is tolerable. Camster
will add considerably to the windfarm experience and it could be argued
that its construction will verge on the creation of a landscape dominated
by windfarms. Halsary would close over open views seen between existing
and consented developments and the creation of a truly windfarm-dominated
landscape would be completed.
Halsary Windfarm
should be rejected on grounds of unacceptable Cumulative Visual Impact.
Geology
and Hydrology
Areas immediately
adjacent to Causeymire wind farm and to the proposed Halsary wind farms
include the following conservation designations: Caithness and Sutherland
Peatlands Special Area of Conservation (SAC), Shielton Peatlands Site
of Special Scientific Interest (SSSI), Caithness and Sutherland Peatlands
Special Protection Area (SPA) and RAMSAR site.
A Special wet moorland
site is overplanted with forestry and major changes occur to the upper
layers of peat and by increasingly deep cracking in the lower layers.
This leads to more drying out which de-stabilises the peat beds.
This is exacerbated
by the felling of trees, the construction of access tracks, cable tracks,
increased ditching, huge turbine bases and the infrastructure which
is all part of wind farms.
Our peatlands are
the best eco-system in the world and we destroy them at our peril. They
are the best source of natural carbon sink so it is ironic to be destroying
them with wind farms. They represent a massive area of peat destruction
with the resulting loss of CO2 from the atmosphere.
The Environmental
Statement (ES) states "Depth probing indicates that approximately 95%
of the land surface within the development site comprises peat."
The deeper the peat
the greater the carbon storage capacity. The peat on this site varies
between .01m to over 7.7m in depth. The ES states that the maximum length
of probe was 7.9m, so the total depth of peat is unknown in much of
the development site and it is further stated that those marked as 6m
depth of peat are actually of unknown depth. In other words the peat
is enormously deep and so it is impossible to calculate how much CO2
storage will be destroyed. It could be that this will negate building
the wind farm in the first place.
Peatlands absorb
water and release it slowly which helps to prevent flooding at lower
levels and is more than ever necessary with our climate becoming increasingly
wet.
It is stated that
the in situ peat will be a major issue to overcome. There is no doubt
that any construction, especially heavy turbine bases, will be enormously
difficult and this in an area where tree roots will have damaged the
surface structure of the peat.
The hydrology of
the area is already upset by the ditching for the plantation and will
be further adversely affected by the construction of a wind farm which
may put the whole structure of the peat at risk. Runoff must be carefully
controlled. Pollution of watercourses must be prevented with adequate
pollution measures.
Tourism
The combination
of Halsary, Spittal and Causeymire windfarms on one of the main tourist
routes in Caithness would give a very unfavourable impression. Visitors
will not return if they see a formerly open and unspoilt landscape turned
into a massive industrial site.
The unacceptable
cumulative visual impact of Halsary Windfarm in combination with existing
and consented developments would have a significantly negative influence
on tourists resulting in fewer return visits and the lowering of Caithness'
attractiveness to future visitors.
Ornithology
The wind farm site
will be adjacent to the Caithness and Sutherlands Peatlands SPA and
Ramsar site and the Shielton Peatlands SSSI. The qualifying species
of birds for the SPA are Red-throated diver, Black-throated diver, Wigeon,
Common scoter, Hen harrier, Golden eagle, Merlin, Golden plover, Dunlin,
Wood sandpiper, Greenshank and Short-eared owl. Non-qualifying interests
are North Scottish Greylag goose, Teal, Curlew and Arctic skua. The
Shielton Peatlands SSSI citation lists breeding waders and wildfowl.
Raptors recorded
during surveys were Hen harrier, Merlin, Peregrine, Goshawk, Rough legged
buzzard and Barn owl. During the breeding season Barn owl and Red-throated
divers were recorded breeding within 1km of the development and Merlin
were presumed to have bred within 700m of the development in both 2008
and 2009. Other birds recorded during the breeding season were Arctic
skua, Great skua, Greylag geese, Greenshank, Golden plover, Curlew,
Lapwing, Skylark and Twite. Lesser redpoll, Song thrush and Skylark
were recorded during the non-breeding season. At least 10 Red grouse
territories were recorded during 2008.
The surveys showed
regular use of the Loch of Toftingall for foraging Osprey during the
breeding season. The bird would often fly over the site to perch on
a fence post where it would consume its catch. Collision modeling shows
a potential loss of 1 bird every 5.3 years. This is totally unacceptable.
Caithness only supports one pair of breeding Osprey, the most northerly
breeding pair in Great Britain. Should the lost bird be the foraging
male partner this would likely result in the loss of the offspring that
year and present the possibility of there being no breeding pair thereafter.
Therefore, the conclusions of the Environmental Statement seriously
underestimate the effect on the Osprey population and distribution.
Black throated and Red throated divers were also recorded using the
Loch of Toftingall for loafing. This shows that the Loch of Toftingall
is particularly important to all of these Annex 1 protected birds and
the development would pose an unacceptable risk.
Ecology
There are populations
of Water Vole, a UK Biodiversity Action Plan (BAP) priority species
in severe decline, on the Halsary Burn and its tributary Hector's Burn.
Under the Wildlife and Countryside Act it is an offence to intentionally
or recklessly damage, destroy or obstruct access to any structure or
place which water voles use for shelter or protection, or to disturb
water voles while they are using such a place.
Otter, which is
protected by the EC Habitats Directive and a Priority species in the
UK BAP, is recorded as regularly occurring and a viable population uses
the Development site.
Wildcat is protected
by the EC Habitats Directive and is likely to occur within the forest
area which will be felled if this proposal is approved. The removable
of this potential habitat will impose yet another restriction on an
already rare and vulnerable species.
The following are
covered by the UK BAP and described in the ES as important at Halsary
for their fragility, typicalness, position in the ecological mosaic
and potential ecological value: modified bog, dry dwarf shrub heath,
upland flush. In addition Valley mires, a type of active blanket bog,
is present and is a Priority Habitat under Annex 1 of the EC Directive
92/43/EEC on the Conservation of Natural Habitats and Wildlife Fauna
(The Habitats Directive). It is also a Priority Habitat on the UK BAP.
It is important at Halsary for its fragility, typicalness and position
in the ecological mosaic
Small cranberry
Vaccinium microcarpum and Sphagnum austinii are Nationally
scarce species and confirmed as being present in the site.
The examples of
blanket bog within the Development site are relatively small but are
important on account of their diversity, rarity, fragility, typicalness
and position in the ecological mosaic. In addition, the 'quality' of
the more intact blanket bog within the Development site is similar to
the surrounding SAC designated blanket bog.