West Coast Marine and Coastal Localities:
a Detailed Description of 14 Segments

5.14 Cascade
(Jackson Head – Cascade Point, 22 km)

5.13.1 Summary
The Cascade segment comprises a mostly steep and forested coastline, backed by hilly catchments in the north and the Cascade Plateau in the south, with several small streams flowing out to sea and no coastal wetlands present. The shoreline is dominated by rocky reefs that also extend offshore and the few beaches are mostly of coarse sand and fine gravel. The continental shelf lies wholly within the territorial limits, with the steeper continental slope and several canyons dropping off from depths of about 200 metres. The area supports marine life that is important to the southern West Coast, representing a transition between the northern parts of the West Coast and the outer Fiordland coast. Coastal access to this area is for fishing and recreational activities, mostly by boat from Jackson Bay or by several walking routes to the coast. The landscape and habitats in this segment are unmodified.

Notable features of this segment include accessibility by boat from Jackson Bay in the north, limited access by land, unmodified catchments and coastline, the visually-impressive coastal landscape of the Cascade Bluffs, rocky reefs, canyons and other seabed formations, and recreational uses. Fishing is the main commercial use of the coastal marine area.

Existing protection includes conservation lands that cover almost all of the land in this segment and several specified areas under the Regional Coastal Plan.

Cascade Bluffs waterfall
Photo: N. Shears, Auckland University


5.13.2 Natural Features

Coastal Land and Islands
The coast from Jackson Head to near Teer Creek comprises a series of rocky headlands and small embayments, backed by generally steep hillslopes and catchments covered in indigenous forest.

The Cascade Bluffs are an imposing landscape feature, extending from about Teer Creek to Cascade Point. The bluffs are the eroded end of a large lateral moraine from glaciers that once flowed down from the Olivine Range and the Red Hills, and are composed mostly of compacted ultramafic boulder deposits. A ramp of large boulders forms the shoreline at the base of the bluffs in most parts, but in places (especially in the vicinity of Cascade Point) the bluffs drop vertically down to well below sea level. Cascade Point is a fossil site of geological interest309.
About ten vegetated rock stacks of less than 0.1ha each are scattered throughout this segment, including ‘Cascade Island’, which has a dominant cover of the threatened seal cress310.

Coastal Wetlands and Waterways
Several small rivers and streams enter the coast in this segment, including the Smoothwater and Stafford Rivers and Teer Creek. The Duncan, Donald and Dougal Creeks terminate in waterfalls over the edge of the bluffs, inspiring the name ‘Cascade’ for several features in this area. There are no coastal wetlands of note in this segment due to the general absence of lowland flats.

Seashore and Marine Areas
Coastal rocky reefs occur along the whole segment, and these support a diversity of habitats that are generally typical of such habitats in the southern West Coast, representing a transition between the northern parts of the West Coast and the outer Fiordland coast.

Small beaches occur only at Ocean Beach, Smoothwater Bay, Homminy Cove and Stafford Bay. Nephrite and semi-nephrite cobbles can be recovered from some of the beaches in this segment311.

A complex formation of submarine canyons extends to within about two kilometres of the coastline in this Cascade segment. The accurate detail of these formations is uncertain, as charts portray different topographies312. NZ Oceanographic charts label three main canyons in this area (the Arawhata, the Jackson and part of the Cascade), and show small extensions of continental shelf extending out no more than about 10 kilometres in the vicinity of Smoothwater Bay and Cascade Point. The seafloor reaches depths of about 2000 metres within the territorial limits, while locally rising to about 1000 metres in some outer parts of the territorial waters. The continental slope and canyons are very steep-sided formations with slopes of up to about 30 degrees in some places.

Important anchorages for commercial fishing vessels are located inside Cascade Island, around a headland just north of there and in Smoothwater Bay.

Cascade Point reefs
Photo: N. Shears, Auckland University
Jackson Head boulder shore
Photo: D Neale, DOC.

Coastal and Marine Wildlife
The Jackson Head – Cascade Point coast has been rated as a habitat of outstanding wildlife value313.

About 300 tawaki (Fiordland crested penguin) nests are dispersed from Stafford Bay to Cascade Point, while others occur at the large Jackson Head colony (see Segment 12).314

When surveyed in 1990, the rocky coast north from Cascade Point had one of the largest New Zealand fur seal breeding colonies on the West Coast, with an estimated 3000 seals (including at least 500 pups)315.

Petrels and possibly prions were reported in 1980 to be breeding at Jackson Head316 but there are no more recent published reports.

Marine Fish and Other Species
This coastal region, like the whole west coast of the South Island, supports a rich diversity of fish and invertebrate species that are fished both commercially and recreationally by a number of fishing methods including trawl, longlining, trolling, potting and set netting.

Inshore trawl fisheries are multi-species and are primarily based on flatfish (several species), red gurnard, red cod, giant stargazer, tarakihi and blue warehou. Other species taken as bycatch include arrow squid, dark ghost shark, ling, barracouta, jack mackerel, spiny dogfish, rig, school shark, sea perch, rough skate and smooth skate317.

Commercial fishing using other methods such as longline, potting, set net, and trolling for a number of species such as bluenose, ling, stargazer, warehou, lemon sole, hapuka, school shark, tuna and crayfish (to mention a few) is extensive.

Surveys in this area of shallow reef communities318 and coastal reef fish319 indicate that the reefs in this segment are generally typical of the South Westland coast, representing a transition between the northern parts of the West Coast and the outer Fiordland coast. A high diversity of 60 coastal reef fish species have been recorded in this segment. Paua in this area have been found to be relatively scarce and small320.

There is little published information on the fish communities of the continental shelf and canyons in this area, in part because the NIWA West Coast trawl surveys do not extend this far south.

Jackson Head bedrock shore
Photo: D Neale, DOC.
Ocean Beach, Jackson Head
Photo: D Neale, DOC.

5.13.3 Historical and Archaeological Heritage
The Cascade coastal segment was an important nephrite collecting and working area. Post European sites are generally associated with shipwrecks321, including the Pacific in 1857322. Cascade Point was named by Captain Cook in 1776, after the several waterfalls on the nearby bluffs.

5.13.4 Recreation and Tourism
Walking tracks lead through coastal forest from Jackson Bay to Ocean Beach (the Wharekai Te Kou track), and to Smoothwater and Stafford Bays, providing access to natural coastal landscapes and rocky coasts that are used for exploring, fishing and other activities.

Recreational boats access this area from nearby Jackson Bay for such purposes as fishing and sightseeing, and these activities appear to have increased significantly here in recent years323. Rod fishing is the main type of fishing, but scuba diving, snorkelling and recreational set netting appear to be popular in this region as well.

Bluffs of Cascade Point, looking south to mouth of Cascade River and Barn Bay
Photo: D.L. Homer, GNS

5.13.5 Commercial Use
The Cascade area, as for most of the inshore West Coast, is fished by commercial fishers using a variety of methods including bottom trawl, trolling, potting, set netting and longlining. Vessels in this area mostly operate out of Jackson Bay and Greymouth, but also Milford, Westport and Nelson. Reefs in this area are also fished for rock lobster using craypots by vessels out of Jackson Bay and Milford.
Abundance surveys have indicated that there are poor prospects for a paua fishery in this area324 but there is still potential for development of a fishery.

5.13.6 Other Public Uses and Facilities
Access to the area is mainly by boat from Jackson Bay, and also from the airstrip at the mouth of the Cascade River, or the track down the Cascade River from the roadend at Martyr Homestead. Walking routes exist on the Wharekai Te Kou, Smoothwater Bay and Stafford Bay tracks. There is a Department of Conservation hut at Stafford Bay.

There is one Resource Management Act coastal permit issued in this segment325, for stone extraction in Homminy Cove.

5.13.7 Existing Protection and Management Areas

Most of the coastal land and catchments in this segment are within conservation lands, except for small areas of legal road along the Smoothwater River.
Whitebaiting is not permitted in non-tidal areas, nor upstream of ‘back pegs’ on the Smoothwater River326.
The area lies within Fisheries Statistical Area FSA 33, which is part of the Challenger Fishery Management Area (FMA 7). The adjoining land area is within the Westland District.
The operative West Coast Regional Coastal Plan recognises:

309 Hayward & Kenny 1999
310 Neale 2006e
311 Hooker 1986
312 Carter 1981, RNZN 1985
313 Coker & Imboden 1980
314 McLean et al 1997
315 Anderson 1990
316 Coker & Imboden 1980
317 Stevenson and Hanchet 2000
318 Shears in prep
319 Roberts et al 2005
320 McShane et al 1993
321 Hooker 1990
322 Ingram 1990
323 G. Newton pers comm 2005
324 McShane et al 1993
325 West Coast Regional Council, www.wcrc.govt.nz “Maps on the Web”, June 2006
326 Whitebait Fishing (West Coast) Regulations 1994

Cascade MapHabitats & Ecosystems People & UseAnimals & Plants Existing Protection & Management Plans Submission Form