Whare Flat – Information and Trips Library
Leaders:
10/10/2001 Chalkies, Hamilton (Invermay). Round trip. Medium. Elaine D, Barbara McC
Taieri Recreational Tramping Club
Mid-week recreational and social walking group based in Mosgiel NZ
Post linked to Info Post
Whare Flat – Information and Trips Library
Leaders:
10/10/2001 Chalkies, Hamilton (Invermay). Round trip. Medium. Elaine D, Barbara McC
3. 6/6/2001. Port Chalmers, Deborah Bay. Easy+. Leaders: Bill H, Lesley S, Winnifred
Contacts:
DCC Forestry, 300 King Edward St, 455 5512
Scouts Assn 17 Moray Place 477 6644
M.A.E. Invermay waiora Farm, Silverstream Valley Road 489 5401
por Invermay Research Centre 489 3809
Mr & Mrs Fraser, Three Mile Hill, 489 3767.
1/4/2001 Three Mile Hill walking track. Leaders: Daphne, Jean M
1. 22-23/9/1989. Moeraki Motor Camp. Leaders: Bob & Audrey. 24 attended this weekend camp. Everyone had a great time and Audrey and Bob were thanked for a job well done.
28/2/1996. Bus Trip – Post Office Creek – Government Track. Downhill all the way. Leaders: Jack R, Barbara McC, Joyce, Mary Y.
2. Friday 22/9/1992 – Sunday 23/9/1992. Moeraki Motor Camp. 23 attended. Leaders: Bob & Audrey
1. 22-23/9/1989. Moeraki Motor Camp. Leaders: Bob & Audrey. 24 attended this weekend camp. Everyone had a great time and Audrey and Bob were thanked for a job well done.
In 1876 a report was written for the Dunedin City Council outlining the various options available for the supply of water to the low-lying areas in the city. The two options available were the Leith Valley supply which was to be very expensive, or the Silverstream supply which would be cheap and effective but would supply water to only the low levels.
In December 1877, during the on-going debate over the two systems there came a dry spell and Ross Creek Reservoir was so low that a fire in the city drained the reservoir. This incident served to motivate a decision and in December 1877 the Silverstream project was decided on.
By 1880 13 miles of water race was constructed out of a total of 18 miles and in 1881 it consisted of 29 km of winding open earth ditch 3 to 4 feet across, timber sluices, tunnels, weirs and steel pipes. It began at the top weir on Silver Stream and wound around the western slopes of Swampy Summit, Flagstaff and Three Mile Hill to the Southern Reservoir in Kaikorai Valley. It was opened on 15th December, 1881. All eastern tributaries of Silver Stream from the top weir to the Three Mile Hill Road were diverted into the open race by small masonry inlets.
Water shortages still recurred from time to time and it was soon found that the Silverstream scheme was not as wonderful as previously thought. In times of heavy rain the open water-race could not cope with the volume of water while there was not enough storage at the Southern Reservoir for a long period of heavy draw-off.
In 1895 it was decided that additional pumping and storage was required. The final location for a pumping station was at Powder Creek. In 1920 an electric pump was installed at the bottom weir, pumping water up a pipeline and into the water-race when needed. Apart from in 1890, it was not used again until 1928. By 1933 the population growth and the increase in water use made it practical to appoint a full-time attendant at the pumping station.
Since the early 1940s, land subsidence and the need for constant maintenance resulted in much of the open water-race being replaced with pipeline. The water-race in this area of tracks was the only major part that was not piped. Following a severe flood in 1957, the water-race above the pumping station was closed. After this, water for the race was pumped from the pumping station directly up the hill into the open water race.
The Silver Stream Water-Race was abandoned in the late 1960s. The current pumping station moves water along a buried pipeline following a new route to the Southern Reservoir.
In the late 1980s the Track Clearing Group began to re-open and develop the Silver Stream Water-Race Tracks. This group, with the assistance from the WEA over 50s Tramping Club continues to do great work in maintaining these tracks. The late Steve Amies was the founder of both groups and instrumental in re-opening the tracks.
Other matters receiving attention during this time were the afforestation of the water reserves and the detection and prevention of pollution. Considerable planting was done around the Leith and Silverstream catchments. The aim of this policy was commercial as well as functional. It was claimed that afforestation kept down noxious weeds, kept the area free from stock and rabbits, and increased the efficiency of the area as a water catchment as well as increasing the beauty of the country.
Since 1948 the open water race has been progressively replaced with a pipeline. The catchment lies to the West of the Flagstaff-Silverpeak divide, and comprises 4275 hectares which is largely council owned with much of it in native bush, some in tussock and some in exotic plantation.
– Adapted From City Forests Ltd hard copy information sheet and DoC Silver Stream Water-Race Tracks.
It is also interesting to note how dry this slope is. This stands in sharp contrast to the cooler gully at the bottom of the hill. A bridge spans the creek here, about 20-30 minutes from the carpark. Beyond this are more mature patches of forest.
Fuchsia (with orange bark) predominates in this valley, while little kanuka can been seen. A good variety of ferns thrive here in the moist conditions, the most distinctive of which are the tall tree ferns. The one with milky-coloured frond stalks is the silver tree fern.
Just 2-3 minutes beyond the bridge is a clearing. From it the hill just descended is apparent. More of the story becomes obvious. The whole hillside is of an even aged kanuka. Above nearer the road one sees old macrocarpas.
Kanuka and manuka often thrive after fire or in areas cleared either by humans or nature. Could it be that this hillside was once cleared, and that maybe the macrocarpas indicate an old homestead site – a base for a farm now abandoned and reverting to native forest?
In such a role kanuka is a successional species; i.e. it thrives after disturbance allows light into the forest floor. In time it gets over-topped by other forest species and becomes replaced with more mature forest.
An example of this mature forest that once covered this hill and what will once again be seen is 10 minutes further down the track.
One cannot fail to be impressed by the huge boles in the rimus (with hammer bark) and miros (with soft green leaves and dark mossy trunks). These giants are survivors of a once extensive podocarp forest that covered most of the Dunedin district. Fortunately their poor shape precluded their being logged for timber and consequently they now serve as a seed source to re-vegetate the reserve in podocarps. The dominant trees forming the forest canopy in this area are kanuka.
A second small patch of these trees occurs a little below the second bridge. Beyond them further evidence of the impact of humans on the area is seen – hawthorns growing in the forest! These exotic trees from Europe add a new shade of green to the forest each spring. Being deciduous, like so many continental trees, they lose their leaves in summer and grow a new set in spring. In New Zealand the only common tree with this habit is the fuchsia – the orange shaggy-bark trees. Like kanuka, fuchsia is one of those successional species. Their roles are very similar but they fill them in different locations – fuchsia preferring damper cooler sites.
– Adapted from DoC hard-copy information sheet
P N Johnson, Botany Division, DSIR, Dunedin March 1987
Quarantine Island has a fenced 1.4 ha of low Halls totara – broadleaved forest in excellent condition, plus other native scrub and coastal communities. …
Quarantine and Goat Islands owe their origin to former spurs drowned with the sinking of valleys now occupied by Otago Harbour. Both were used for quarantine purposes in early days of European settlement, and are Crown Land, formerly managed by Health Department. Goat Island has now largely reverted to native low forest and scrub. … Quarantine Island is leased to the St Martins Island community, who maintain a house and other buildings on the eastern headland, and graze sheep over most of the island, except in a fenced-off portion of bush, facing south at the western end. Historical remnants persist in the form of one of the old quarantine buildings, a small graveyard, chimney and flagpole remnants and old wrecks at the boat landing. The island is c. 17 ha in area, and reaches 58 m at its summit. There are two pylons on the crest, carrying electricity from Port Chalmers to Portobello.
Broadleaved – totara forest. This comprises most of the c. 1.4 ha fenced-off area to which sheep do not have access. The canopy, mostly about 4m tall, comprises Halls totara, broadleaf, ngaio, kohuhu, lancewood, peppertree and divaricating shrubs. These last two become more common in the understorey, especially Melicope simplex and Coprosma areolata. Traces remain of shrubs which would previously have been more common: Corokia cotoneaster and Helichrysum aggregatum, while the abundance of mahoe saplings 1m tall indicates that this species will become more common in future. Ground cover is dense, despite the dry stony soil, with Asplenium lyallii, shield fern, Carex forsteri and Libertia ixioides. Creepers are also abundant below and upon the shrubs, especially Scandia, Calystegia, climbing rata, Parsonsia and Clematis paniculata. Condition of this forest is very much better than adjacent grazed forest, or any similar forest remnants on mainland sites on Otago Peninsula.
Cabbage tree – coprosma – totara forest. An eastern portion of the fenced-off bush, probably more open at the time stock were excluded, has cabbage trees above a mixture of windswept totara and Coprosma propinqua scrub. Former grassy openings illustrate the process of regrowth of scrub and forest. The grasses browntop and cocksfoot of the former pasture are being invaded by bidibid, Coprosma propinqua shrubs, and the tall palatable grass Hierochloe redolens.
Flax, some of it possibly planted, is establishing vigorously from seedlings, even among long rank grass, and there are healthy saplings 1m tall of Olearia avicenniaefolia, lancewood, kohuhu and Hebe elliptica.
Coprosma – mixed scrub. Shady faces of the southernmost headland have dense 2-3m scrub of Coprosma propinqua, Halls totara, Melicope, kowhai, ngaio and creepers (mostly Muehlenbeckia australis).
Flax – Hebe scrub. Above the sea shore, in a zone below forest or in patches below pasture, flax grows densely with Hebe elliptica shrubs, and scattered ngaio trees. Patches of bracken are present on some small spurs.
Pasture. On the island crest the main components are browntop, crested dogstail and white clover. Patches of rushes (Juncus gregiflorus, J distegus) occur on moist gentle slopes. Dry crests encourage infestations of barley grass and Scotch thistle (especially common at the south-east end). On sunny faces, Rytidosperma unarede and sweet vernal are common grasses and there are a few patches of silver tussock on upper parts of northern faces. Western faces hold thin, dry, erodible soils between rock outcrops and ledges. Grazing here is heavy, so that the native coastal tussock Poa astonii is reduced to a stubble.
Carex sedgeland. A few small seeps have tussocks of Carex appressa and in one place the tall blue coastal sedge Carex trifida which is of very local occurrence on Otago coasts.
Coastal rocky banks. Some of these are draped with native ice plant, though trampling and grazing prevent this moving up-slope onto ground accessible to sheep. Poa astonii tussock and Linum monogynum are characteristic of rocky outcrops, with other native herbs such as Wahlenbergia gracilis. Easter orchid (Earina autumnalis) surives as a clump atop one northern coastal detached boulder. Crumbling loess banks near the houses have become covered with garde escapes – wallflower, shrubby stonecrop, marguerite daisies and periwinkle.
Coastal herb field in wave-splashed zones. There are small areas of turfy coastal herbs such as Toula dioica, Puccinellia stricta, Crassula moschata, native celery and glsswort. Beach heads become colonised by Atriplex hastata growing among drift and flotsam.
Island at NW corner. Being inaccessible to sheep, this little island illustrates the density and diversity of native plants which would otherwise occupy all opens sites close to the coast. Above a fringe of coastal herb-field is a terrace sward of knobby club-rush, holy-grass, Elymus, Dichelachne and Linum. The rocky sides have dense low Hebe elliptica, tussocks of Poa astonii, mats of native ice plant and the coastal fern Asplenium obtusatum. On the crest, compact shrubs of Coprosma propinqua shelter an infestation of ivy and periwinkle.
Planted trees. As well as the usual macrocarpas typically planted for shelter, there are groups of pines (Scots pine round the graveyard, bishop pine and radiata on the SW grassy promontory). There is a line of Arizona cypress here too. Along the north side are a few trees of Lawsons Cupress, at least two trees of brush wattle on one spur, and a few kowhais which have survived despite the crude netting fences which one protected them. One red beech has been planted near the summit. None of these tree species appear to be spreading naturally.
The Tunnel Beach Walkway, one of the most popular scenic walks around Dunedin will be officially opened by the Minister of Lands, Mr Elworthy, on March 16. (1983).
Access to Tunnel Beach has been negotiated by the Lands and Survey Department with the farmer who owns the land the walkway crosses.
The advantage to the farmer of the walkway is that under the Walkways Act he can be compensated if there is damage done and the access can be controlled. For example, the Tunnel Beach Walkway will be closed during lambing.
…
The steps down the tunnel are worn and water seeps through it so concrete steps will be poured before the official opening.
The Tunnel Beach Walkway is a coastal walk, descending a line of seacliffs south of St Clair where the wild Pacific breakers have carved sheer headlands, sea stacks and arches, and the wind has sculptured extraordinary shapes.
From the road end the track descends across green pasture and within a few minutes reaches the clifftops above Tunnel Beach.
The rock underfoot is the soft Caversham sandstone, an extensive thick sediment laid down during the sea’s encroachment of the Dunedin area 20 million years ago. The sandstone was generally overlain by other sediments, but near here lava from the Dunedin volcano flowed over the sandstone itself. This occurred about a dozen million years ago. The soft nature of the almost uniform sandstone makes walking too close to the cliff-edge a dangerous practice, but has also allowed the magnificent carving both by humans and by nature that is in evidence here.
At Tunnel Beach the rock is seen in detail. Careful examination will reveal shell fragments and with luck a fossil such as a brachiopod shell or echinoderm (sea urchin) or even bones of an extinct whale could be found.
At the top of the tunnel and on the promontories, the rock supports a community of salt-resistant species including Austral spleenwort, Selliera sp and Samolus sp. Species that occur further up the slope do not grow here as they cannot cope with the sea water that splashes up during the high seas that can batter this stretch of coastline.
The tunnel was dug in the 1870s by workmen employed by John Cargill, a son of Captain William Cargill, and who farmed the area. It’s reputed to have been a birthday present to his daughter.
The Cargill families found seclusion and shelter on the beach at the foot of the tunnel steps.
The swift flowing current, with is load of sand and erosive potential, heads up the coast just beyond the extremities of this little bay. It must have deterred all but the strongest swimmer from entering the water. At low tide the sandy beach makes an attractive setting for picnics, with the deeply cleft sandstone buttresses towering above. Some are intricately carved, some lie scattered as blocks already tumbled to the beach. Needless to say, common sense dictates where to sit in safety.
Some of the smaller boulders beneath the cliff are derived from the lava floors above, or from Blackhead, a headland of down-thrown volcanic rock being quarried to the south-east.
Vertical rusty streaks of iron-staining make a cross-cross pattern with the near horizontal traces of each successively deposited layer, called “bedding planes”, visible on the cliff faces.
Caves and sea-arches are eroded into the cliffs and an arch at the southern edge of Tunnel Beach, when seen from the walkway above is an excellent example showing the formation of a “stack”.
When the arch has finally eroded and collapsed, the leg on the right will stand free of the mainland just as the stacks off the northern edge of the beach do. Horizontal bedding visible on these stacks suggests that these are still in situ and are not blocks that have fallen from elsewhere.
Amongst a group of trees atop the cliffs, Cargills Castle awaits further depredation by time, vandalism and weather. It was built in 1876 for Edward Cargill, another son of the founder of the Province, Captain William Cargill; and a Mayor of Dunedin 1879-98. Originally called “The Cliffs” it was not long before the Italian-designed building was given its present name by locals. It was one of the first concrete buildings in Otago.
The “castle” was of 21 rooms and cost £14,000 to erect. It was nearly completely destroyed by fire in 1892 and although rebuilt by 1923 – “the biggest white elephant in Dunedin” according to one building contractor – was unfit for habitation.
In more recent years there have been several attempts to instill new life into the building, including an opera venture and plans for a tavern, but all to no avail.
– Dunedin Midweek, Wednesday, Feb 23, 1983.
Point of access; Double Hill Road – 500m on right beyond gate below Forest HQ. 45 minutes return. Moderate.
The Seacliff Mental Hospital was competed in 1884 and at the time was the largest public building in New Zealand. Water for the complex was originally supplied from a spring behind Warrington. However, as the hospital developed, this supply became inadequate. An alternative supply was sought and it was decided that a dam and pipeline at Double Hill would be suitable.
As a consequence, this dam and an associated pipeline were built around 1912 for the purposes of supplying water to the Seacliff Hospital. The dam is some 6m high and approximately 1.5m thick at the base. It is estimated that 80 cu m of concrete were necessary to build the structure. In addition, the construction required 17,000m of 150mm pipe to link the dam with the storage tanks at Seacliff. The flow was gravity fed, the dam being at a greater elevation than the hospital.
All equipment to build the dam and pipeline was packed into the upper reaches of the Whaitiripaka Stream on horseback or horse-drawn sled. The pipeline was laid along the stream-bed to Evansdale Glen and thence over Porteous Hill to Omimi and Seacliff.
Problems were associated with the scheme however, primarily due to silting up of the dam and a subsequent loss of capacity. The tragic fire at the Seacliff Hospital in 1942, which resulted in the loss of 37 lives prompted greater concern over the reliability of the Double Hill water supply. Corrosion of the pipeline and unstable ground over Porteous Hill compounded the problems.
An auxiliary water supply was installed at Evansdale in 1944 to augment the supply during the summer period. However the condition of the pipeline continued to deteriorate. Major repairs to the pipeline were considered too expensive and in 1952 it was replaced by a new line from Cherry Farm. Thus ended the useful life of the Double Hill dam and water supply.
Since 1981 the N.Z. Forest Service staff have improved access to the damaged sections of Whaitiripaka Stream where remnants of the water supply scheme remain. The walk to the dam is quite short and well worth a visit in light of its historical background.