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Waikakaho/Cullen Creek Walkway Mt Richmond Forest Park

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Waikakaho/Cullen Creek Walkway Mt Richmond Forest Park Waikakaho/Cullen Creek Walkway Mt Richmond Forest Park Introduction The Waikakaho/Cullen Creek Walkway follows an old was found shortly after in the Waikakaho and in most goldminers’ trail across the range between the Wairau of the streams draining the schist highlands east of the Valley and Linkwater. It can be walked or ridden in one Kaituna Valley. day but you will need to arrange transport between the After quickly exhausting the easily-won surface gold road ends. It is best to begin at the Waikakaho end to the miners turned to the more difficult deep gold of avoid the steep climb on the Cullen Creek side. Both the flood plains and terraces. These had to be worked the Waikakaho and Cullen Valleys provide historically like underground solid rock mines, with deep shafts interesting half-day return trips. and tunnels. Often the mines had to be drained with The walkway is classified as a tramping track; a waterwheel-driven pumps. reasonable level of fitness and strong footwear is Also in 1888, gold-bearing quartz reefs were discovered recommended. The streams at both road ends and in the ranges above. Within a short time over 40 claims those flowing into Cullen Creek are unbridged and were licensed — on both sides of the range — and become impassable after heavy rain. numerous shafts, tunnels, and trenches were dug. Most proved unsuccessful, but by the end of 1890 about Access and how to get there 1000 tons of gold bearing quartz was waiting to be processed. Access to the start of the track at the northern end is at the end In 1891 the Ravenscliffe Gold Mining Company of Havelock London took over these claims and began processing of Cullensville Road, Linkwater. Picton The track entrance is through the quartz. The company installed a five kilometre-long aerial tramway to take the quartz from the mine high in private land. Please keep to the Blenheim marked track and respect farm the hills, 600 metres down to the floor of the Waikakaho stock and the private property Valley. The cable way was reputed to be the longest in leaving all gates as you found them. the country; the steel cable weighed 10 tons and carried 150 buckets, each with a 75 kilogram capacity. In the south the track begins at the end of Waikakaho Road. This road leaves the Kaituna–Tuamarina Road On arrival at the battery, the rock was initially broken along the northern side of the lower Wairau River, up by a 20-stamper battery of heavy hammers that midway between State Highway 1 at Tuamarina plunged up and down, crushing the gold-bearing and State Highway 6 at Kaituna. Please keep to the rock to powder. The power to operate the battery was road and the track which provide legal access to the provided by Pelton Wheels driven by a jet of water Mt Richmond Forest Park boundary. from the Waikakaho River. The water fell 78 metres over two kilometres and was run into progressively smaller pipes to increase the pressure of the final jet driving the History Pelton Wheels. Payable gold was discovered in Cullen Creek in The crushed rock was treated with ‘quicksilver’ 1888 and within two weeks over 200 diggers were (mercury) which instantly spreads over the grains of working there. At the height of the rush there were gold forming an amalgam. The amalgam was heated nearly 1000 men on the diggings. A township called to drive off the mercury, leaving the gold behind. The Cullensville was established, with three hotels, two poisonous mercury vapour was then condensed back to billiard saloons, a bank, courthouse, and five bakeries. a liquid to use again. No visible evidence of the town now remains although The Ravenscliffe Battery began operation in 1892 but, signs mark the sites of many of the old buildings. Gold despite good returns from samples tested overseas, Published by: Department of Conservation, Nelson/Marlborough Conservancy, Private Bag 5, Nelson 7042 | November 2011 only 112 oz of gold was extracted. It was thought that Although it looks relatively undisturbed, there are the mercury-amalgam extraction system was being many sawn off stumps, especially below the track where incorrectly used. Despite trying other extraction the forest was once logged by the miners. The timber methods the company went into liquidation in 1899. produced was used to build the huge wooden pylons of Following the failure of this venture, there were the cable way which took the quartz ore from the mine sporadic efforts to work the deep leads in the early to the battery. 1900s. Then, in a pattern repeated all over New Zealand, On the Cullen Creek side too, the vegetation is mostly the miners returned during the 1930s depression but regenerating. Bracken fern and shrubs are the main were once again unsuccessful. cover of the lower valley. Above the private hut is a pine plantation and above that the beech forest of the forest Vegetation park. At the southern end the track initially passes through regenerating forest with the toothed leaves of kāmahi Walking the track and needle-like foliage of turpentine bush dominant. Higher up the forest becomes taller with large red and Waikakaho Valley to ‘Village Clearing’, 2 h silver beech forming the canopy. From the farm house, the road continues between other farm buildings and yards, and through several gates for two kilometres to a parking area beside the Linkwater Waikakaho River. Sealed road QUEEN CHARLOTTE DRIVE Just before this crossing you will see, on Unsealed road D A To Picton each side of the stream, sheds surrounded O To Havelock R 20 km E by buckets and machinery. Each shed Tramping track W L L h I it V e covers the entrance to a deep (20 m) shaft. S P i N n e Locked gate E The shafts were dug during the 1930s. A L C L re U e k Car park C tunnel links them deep under the river, with a number of short exploratory drives Historic site Cullensville extending back up into the bedrock base of Cullensville interpretation the river. These sheds are on private land and access to them is not available without k ee C Mt Duncan the owners’ permission. r u • C l l s e 892 m ll a n F k The Ravenscliffe Battery was sited against e 0 1 e C r re C e the base of the hill across the river from the rs k le kilometres ha farmhouse. However, apart from a series of W r to c e terraces cut into the hillside, little evidence Mt Cullen p k s e • o e r r of it remains. This map is a guide only. 1055m P C For more information consult Parkmap Mt Richmond Cross Golden Belt Stream and climb edition 2 2009 or Topo50 gradually on the eastern face of this spur map BQ28 Havelock. through scrub and pasture before crossing Waikakaho am re Saddle to the western face and climbing all the way St Dukeshead ) ( s • uir to village clearing, zigzagging occasionally. M 948 m Disused mine (see inset) The Village Clearing am Stre k To saddle Dukeshead e e r This terraced clearing was the centre of C e m l a M o e activity during the quartz extracting period. p r t a - S i p n t o l e In its heyday there were about 200 men Drive t H r B a entrances n c e employed in the mining or processing of k ld o Village Disused G quartz. Now, only the remains of stone Clearing mine B ull dog P Cr chimneys, foundations and rock-lined pools Storage bin ig eek r O remains e AH C v AK r are left. i IK D e R A A e W O R k o h About five minutes above the clearing, a a Farm house k a k i side track leads to the entrance of a drive a Base data supplied by Geographx Ltd W To Waikakaho River copyright reserved which extends over 100 metres into the To Tuamarina rock. It is not maintained and should not be 15 km entered. Waikakaho/Cullen Creek Walkway, Mt Richmond Forest Park | 2 www.doc.govt.nz Village Clearing to Waikakaho Saddle, 30 min Tramping track The main track leaves the village and zigzags before • Challenging day or multi-day tramping/hiking. climbing steadily to the saddle. Sections of rock • Track is mostly unformed with steep, rough or muddy sections. benching, cuttings through rocky spurs, and stone • Suitable for people with good fitness. Moderate to high-level culverts remain from the mining era. backcountry skills and experience (including navigation and survival skills) required. Waikakaho Saddle to Cullensville, 2 h 30 min • Track has markers, poles or rock cairns. Expect unbridged stream and river crossings. Beyond the saddle the track is a little rougher. It sidles • Tramping/hiking boots required. to the left and descends gradually for about 30 minutes to a small grassy clearing. Throughout this stretch, Mountain biking grade 4 (advanced) mountain cabbage trees, capped with tufts of broad, A mixture of long, steep climbs, narrow track, poor traction strap-like leaves, are common. At the clearing is a stone and obstacles that are difficult to avoid or jump over. Generally chimney and the collapsed remains of a hut left over exposed at the track’s outside edge. Most riders will find some from the 1890 quartz era, and the depression of the sections easier to walk. 1930s.
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