Category Archives: environmental management

The beach cliffs north of Stansbury

North of Stansbury on Yorke Peninsula (South Australia), towards Port Vincent, there is an interesting hike along the beach at low tide.  Prominent cliffs of yellowish fossiliferous limestone overlain by reddish sand and mottled clay are in places capped by white carbonate-rich silts and hard limestone called ‘calcrete’ (1).  The cliffs are up to 20m high except where broken in a few places by gullies that mark once active, short streams.  At high tide the sea laps at and erodes the base of the cliffs across a shore platform cut into the limestone. Version 2

The limestone beds (Port Vincent Limestone) were deposited in Oligocene to Miocene times, roughly 20-30 million years ago.  The overlying reddish sands and clays (Hindmarsh Clay) are probably around 700,000 years old (Pleistocene age) and the white carbonate (lime) capping is even younger.

At the Stansbury jetty, the cliffs are mostly of Port Vincent Limestone.  The original bedding in the limestone is outlined in places by thin rubbly layers and elsewhere by shell-rich beds.  The limestone was deposited in shallow seas that once occupied the St Vincent Basin. Conspicuous amongst the fossils are whole-shell sea-urchins (echinoderms), bivalves (clams and oysters) and bryozoa in a sandy matrix that is largely made of shell fragments (4).  The cliffs show spectacular evidence of former caves, sinkholes, pipes and other solution features: these are obvious because they are filled with mottled green, yellow and red sandy clays (2, 3).   Undercutting by the sea has progressively collapsed the limestone to expose these structures and in places wash out the clays.  The caves and pipes characteristically have smooth surfaces dating from a time when lime-rich solutions seeping over their walls precipitated calcite on evaporation. Version 2

Version 2

Version 2

In the section from Beach Point (Long Beach) northwards, the Port Vincent Limestone is overlain by Hindmarsh Clay, a thick band of mottled green-yellow clays and deep red sandy clays.  In contrast to the marine origin of the limestones, these were deposited during the Pleistocene in fluvial environments.  The boundary between the two formations is important as it represents a large time break of several million years, during which the seas retreated from St Vincent Gulf to well south of Kangaroo Island.  As this was happening, in the Late Tertiary period, the changing conditions exposed the limestones at the landsurface and subjected them to erosion, weathering and dissolution to generate a significant karst (caves, sinkholes, pipes, and the like) landscape.  Major riverine and lake environments later became established in the former gulf.  The river systems drained highlands to the north and generated widespread alluvial and lacustrine deposits of sand and clays over the karst limestone, filling the caves and sinkholes to produce the remnants we see in the cliffs today.

It’s interesting to speculate as to whether the remains of any fauna (including megafauna) occur within this cave and sinkhole landscape.  It did, after all, form at about the same time as the extensive cave systems in the limestones of the South East and the Nullarbor which contain abundant mammalian and other fossils.

A feature of the Hindmarsh Clay is the occurrence in places of white bands of the mineral alunite (potassium aluminium sulfate).  Towards the northern end of Long Beach it was sufficiently abundant for local entrepreneurs to begin to mine it to produce potassium sulfate fertilizer (according to a report by RL Jack, Assistant Government Geologist, in 1918),  which was in short supply during the First World War, but the venture failed.   Remnants of mining operations can still be seen at the base of the cliffs behind sand dunes (5).  The alunite was formed from a reaction between acid groundwater and potassic clays in the sediments.  The process in detail is unclear, but the occurrence of alunite in superposed near-horizonal seams suggests that appropriate conditions may have related to flow of local acid groundwater.Version 2

Above the Hindmarsh Clay in most of the cliff-line is a ‘blanket’ of younger Pleistocene lime deposits.  These consist of unconsolidated silts with interlayers of hardened calcrete.  The youngest calcrete is exposed as sheets over large areas of the landsurface on this part of Yorke Peninsula, and was exploited in earlier days for the local production of quicklime.  It remains an impediment to cropping but is progressively being crushed and disaggregated by farmers using heavyweight rollers hauled behind large tractors.  The unconsolidated carbonate silts are considered to be a loess-like aeolian deposits whereas the calcrete bands are likely to represent the remnants of ancient soils that formed at successively younger times.

What else can we note about the geology of the Stansbury cliffs?

Projecting the top of the cliffs seawards provides an indication of the former extent of the Pleistocene landscape that has now been disrupted and incised as the St Vincent ‘valley’ was drowned by rising seas.

Fallen blocks accumulated at the base of the cliffs is the result of mass collapse of limestone and calcrete in the cliffs caused by back-wasting under the attack of waves.  Some rock fragments are very large; others are small and part of a lag concentrated by tides at the back of beach.  Many are angular, which indicates that they have relatively recently fallen from the cliff; some are rounded and smoothed which indicates that they have been washed around in the surf zone for a long period of time.   It’s interesting to speculate about the time that it takes the cliff to retreat under the attack of the rising sea.  Only observations over the long-term (mapping of fallen blocks or reference to old photographs to compare with the present) might answer this question.  However, most cliff erosion is likely to take place at comparatively rare times of severe storms and powerful wave and wind attack, whereas little change occurs under usual weather conditions.

The cliffs in some places are coated with a ‘wash’ of sediment from higher in the sequence, and this sometimes obscures the geology and makes it difficult to pinpoint breaks in the rock sequence. This coating varies from a thin surface veneer to substantial talus deposits, and usually occurs in places where the cliff is less exposed to wind and waves.  As well, in places, the red sand and clay fill in the old caves and pipes has spilled out from the cliffs where erosion has exposed them.

Collapsing masses of rock, spilling of sands and clays from less coherent deposits, breaking apart and exposure of karst features, and wash over cliff surfaces, are all components of cliff retreat in this region.

It’s interesting that the cliffline can be traced from actively eroding beach cliffs north of the jetty at Stansbury to a subdued hillslope at the back of the town to beach cliffs again south of the cemetery. The townsite is actually an embayment that was filled by shallow water shelly limestones (deposited around 10,000 years ago in seas that were at a slightly higher level than today) and covered by more recent sand dunes.  It seems to have been a quirk of nature that preserved the embayment, in much the same way that winds, tides and seawater circulation on this eastern side of the gulf produced distinctive, recurved sand and mud spits that protect other bays like Stansbury.

Further reading.

RP Bourman, CV Murray-Wallace, N Harvey (2016)  Coastal Landscapes of South Australia.  (University of Adelaide Press: Adelaide).  423pp.

AR Crawford (1965)  The Geology of Yorke Peninsula.  Bulletin No. 39.  Department of Mines, Geological Survey of South Australia. 139pp.

RL Jack (1918)  Alunite deposits, Section A. Hundred of RamsayInSouth Australia Department of Mines, Mining Review No. 28 for the half-year ended June 30th, 1918.  pp51-53.

AR Milnes, JT Hutton (1983)  Calcretes in Australia – a Review.  In ‘Soils: an Australian Viewpoint’, Chapter 10, 119-162. (CSIRO, Melbourne/Academic Press, London).

WJ Stuart (1970)  The Cainozoic stratigraphy of the eastern coastal area of Yorke Peninsula, South Australia.  Transactions of the Royal Society of South Australia 94, 151-178.

Dr Tony Milnes – Earth Sciences, University of Adelaide

Gulf St Vincent & Adelaide beaches

Over the last million years in southern Australia, sea levels have fluctuated between about 120m below present sea level, during the Ice Ages, to about 2m above during the interglacials.  As humans first arrived in Australia more than 50,000 years ago, the sea level fluctuated between 60 and 40m below present, and vast coastal areas were exposed for settlement.  Gulf St Vincent has a maximum depth of 40m so, during those times, it had the form of a flat landscape of alluvial plains veneered with calcrete and covered by thin sandy soils and sporadic desert dunes gently sloping towards a central oblong saline swamp (Fig. 1).

Around 30,000 years ago the Earth plunged into a severe Ice Age that lasted until about 15,000 years ago, with sea levels dropping to 120m below present.  A warming climate then caused rising sea levels, so that by around 9,700 years ago the sea encroached into the land to form the Gulf (Fig. 2).  Continued climate warming and further sea level rise progressively filled the Gulf.  The warm shallow seas enabled prolific growth of algae and marine grasses that were nurseries to a rich ecology of fish, shellfish, starfish, sponges, calcareous algae and some corals.  Sand-sized foraminifera were abundant, especially in the nearshore and intertidal zones (corresponding to the mangrove-rich areas north of Adelaide).

By around 6,500 years ago the sea had reached its present level and the Gulf achieved its current shape.  Abundant shells and shell grit were deposited to form a meter-thick veneer of calcareous sediment covering the now drowned landscape.  Predominant south-southwesterly winds created waves that eroded these sediments, for example around Port Norlunga and Maslins Beach, and quartz sand winnowed from them mixed together with more recent shell grit to create the modern beaches (Figs 3, 4).  Some quartz sands came from more ancient deposits that are now exposed at Hallett Cove.

Frequent southwesterly storms drove coastal sands northward from Marino Rocks and Glenelg to form a coastal dune series that enclosed the Patawalunga and Westlake depression.  This wave-dominant dune system continued to grow northward creating the present Le Fevre Peninsula where around 10m of sand has accumulated (Fig. 5).

European settlement since 1836 has altered the coastal zone by building on or removing most sand dunes, thus allowing storms to attack roads and residences. Placement of rocky rip-rap with the aim of protecting the shoreline has in fact increased wave turbulence and lowered the beach profile by removing additional sand.  Replenishment of beach sands to maintain amenity is a continuing Government-funded activity.  Tennyson Dunes is one of a few tiny remnants that provide a glimpse of the original Adelaide metropolitan coastline.


Bourman RP, Murray-Wallace CV, Harvey N. 2016. Coastal Landscapes of South Australia.Available as a free ebook from

Fuller MK, Gostin VA. 2008. Recent coarse biogenic sediments of Gulf St Vincent.InSA Shepherd et al. (eds) Natural History of Gulf St Vincent.  Ch.3 , 29-37. (Royal Society of South Australia).

Harvey N, Belperio AP, Bourman RP. 2001.  Late Quaternary sea-levels, climate change and South Australian coastal geology.  InV Gostin (ed.) Gondwana to Greenhouse: Australian Environmental Geoscience. Geol. Soc. Aust. Spec. Publ. 21, 201-213.  (Geological Society of Australia: Sydney).

James NP, Bone Y. 2011. Neritic Carbonate Sediments in a Temperate Realm, (Springer Science+Business Media).

Author: Dr VA Gostin

New report

Professor Bob Bourman and I have just submitted a report to the Inman River Catchment Landcare Group (southern Fleurieu Peninsula, South Australia) entitled ‘The geology and landforms of the Inman River Catchment‘.  Some funds in support of the project came from the Regional Landcare Facilitator Programme, an initiative of the Australian Government’s National Landcare Programme.  Our time in researching the subject and writing the report was a voluntary effort.  front-page

The general aim of the project was to prepare an overview of the geology and geomorphology of the Inman Catchment.  This was to provide a basis for improving local knowledge and awareness of how landscape and landforms have changed (and continue to change) according to landuse and land management practices.  We enlisted the help of landowners and gained new insights via their responses to a wide-ranging questionnaire.

The report can be downloaded via the following link:

Dr Tony Milnes, Earth Sciences, University of Adelaide

A conversation with the community about Mining and environmental management

A context for Yorke Peninsula in South Australia

This article was the basis of a talk to a community group (‘Friends of Gulf St Vincent’) based in Adelaide, South Australia , which is committed to improving the ecology and amenity of the Gulf St Vincent biozone.  It was one of several talks given at a gathering of members of the Group and the local community in the Community Hall at Pine Point, a small village on the eastern coast of Yorke Peninsula.  The focus of the meeting was the possible impacts on Gulf St Vincent of an impending open-cut iron ore-copper-gold-uranium mine nearby (Hillside Mine), but broader issues of environmental impacts and controls were discussed.  Having earlier prepared and submitted a response to the Government regulator on the proposing Company’s submission of a mine and environmental management plan, my presentation at this meeting was broadly to overview mining and mine environmental management on Yorke Peninsula (in 20 minutes or so).

When faced with making a presentation on mining and mine environmental management, which is one of the issues that local communities are finding it increasingly difficult to deal with, I find it interesting and somewhat enlightening to take a step back and look at some history.  Community perspectives on industry, and especially coexisting with large-scale industry, has changed in Australia over the decades.  Perhaps with a historical perspective in mind, it might be possible to map a pathway forward to a productive and acceptable coexistence?

The following notes for my presentation are basically dot-points from a series of ‘slides’ which summarise the approach I’d taken in my presentation.  I’m not sure how it went.

Mining & agriculture started early

  • Both industries significantly changed landscapes.  Mining – local but intensive disturbance.  Agriculture – regionally extensive forest clearing but largely surface disturbance
  • Communities benefited from & adapted to both enterprises – but regulation, attitudes & circumstances changed with time
  • ‘Small’ farmer has gone; properties now amalgamated into large enterprises with fewer workers; rural towns & services have dwindled
  • ‘Mines’ neither larger nor necessarily closer to population centres now than in the past are being viewed as environmentally damaging & socially disruptive

Some history of mining on Yorke Peninsula

  • Copper mined from Wallaroo & Moonta from ~1860. Intermittent mining in 1930s & 1940s. Renewed exploration & from 1989 – 1994
  • Parara Mine (west of Ardrossan) operated for Cu-Au in the 1870s; the Hillside & Harts Mines were opened further south at about the same time in a similar geological setting
  • Salt mined & exported from Yorketown, Port Vincent & Edithburg from ~1874. Later developments at Price & Stenhouse Bay
  • Gypsum mined around Yorketown (1870s), Stenhouse Bay & Marion Bay (1890s) for export for plasterboard production
  • Calcrete mined almost everywhere for local building stone & lime mortar.  Lime kilns were very common & lime was exported to Adelaide.
  • Marine limestones mined for export as flux in Port Pirie Pb-Zn smelters from ~1896, mostly from quarries adjacent to ports
  • Cement produced & exported to Adelaide from Tertiary limestone at Stansbury from ~1913 & quarrying continues to this day at Klein Point
  • Dolomite produced from Cambrian limestone at Curramulka since ~1930s & from Ardrossan since 1948.  Exported as refractory for steel furnaces in Newcastle & Port Kembla
  • Construction sand now mined from a Tertiary paleochannel near Price for Adelaide building industry

Some history of agriculture

  • First agriculture ~1846 at Stansbury on an ‘Occupation license’
  • First pastoral lease in 1851 at Wallaroo
  • Agriculture on Yorke Peninsula as a whole expanded from ~1869 with land clearing & crop production.  Establishment & growth of port towns followed for export of goods; inland settlements & towns were established later
  • Poor yields during early days of agriculture addressed by superphosphate additions to soils starting ~1892. High demand for superphosphate.  Imported phosphate from Nauru (high Cd) & Christmas Island (high U) – widespread additions to South Australian soils
  • New barley crop varieties introduced ~1901
  • Extensive clearing of forest to produce additional agricultural land at ‘bottom end’ of the peninsula from 1950s – significant Cu & Mn deficiencies corrected by additives in superphosphate
  • Widespread modern use of ‘direct-drilling’ in croplands with increases in use of herbicides, pesticides, fertilisers

Getting back to mining – what about minerals exploration?

  • Basically, minerals exploration is controlled by geology. Main search areas are in the ancient basement rock complexes.  Gawler Craton – Olympic Dam orebody in central South Australia, Wallaroo-Moonta mines in northwestern Yorke Peninsula; Curnamona Province in northwestern South Australia – Broken Hill mines.

Old crustal elements form the foundations of South Australia and some of the State’s largest orebodies are found in them.  (Map from Preiss W V et al. 2002 MESA Journal 27, 39-53;  Cratons

  • In Australia all mineral deposits are owned by the Crown & the Government approves applications to explore (& possibly later to mine) – on conditions


  • Much exploration & analysis utilises remote sensing data – well before field work starts
  • Exploration leases are granted on application to Government
  • Drilling of target areas follows much deliberation, assessment, sampling & analysis (high costs)
  • Success in finding an economic orebody is very lowAirborne magnetics give clear indications of the geological makeup and structure (‘bones’) of the land at various depths beneath the surface (red = most magnetic rock; blue = least magnetic rocks). (Map from SARIG)

Airborne magnetics give clear indications of the geological makeup and structure (‘bones’) of the land at various depths beneath the surface (red = most magnetic rock; blue = least magnetic rocks). (Map from SARIG)



Radiometric K

Airborne radiometrics provide unique information about the distribution of radioactive elements (K,Th,U) in surface rocks and soils from gamma ray signals (red = most potassium; blue = least potassium). (Map from SARIG)


  • If, after exploration, an orebody is discovered and assessed to be ‘economic’, Government approves (or not) an application to mine on conditions based on submission of a ‘comprehensive’ formal Proposal or Plan
  • Legislation drives the process & the outcomes: Mineral Resources Division (Department of State Development) in South Australia is the regulator
  • Consultation with landowners & communities (particularly at the exploration stage) can be inadequate.  Community angst leading to ‘outrage’ is a common consequence
  • Environmental management guidelines (& community expectations) can be ‘downplayed’ in favour of ‘public good’
  • Company (& shareholders), Government (through royalties & taxes) & Community (employment, local Company spend, services) can all benefit from a mining operation. What about landowners?  How is best to benefit neighbouring landholders?
  • BUT legislation (& regulation) is generally inadequate in terms of environmental management & rehabilitation (post-mining) – can lead to significant environmental legacy
  • Information about what can & can’t be ‘done’ should be readily available & clearly explained to communities.  How? By whom?
  • Community lobby can change legislation: best practice environmental management ‘guidelines’ should become ‘requirements’?
  • Cost of mining projects must include the full cost of rehabilitation of project areas to something like that existing pre-mining according to best practice guidelines – not currently the case .  Many mining projects would not proceed if this was the case!
  • Mining companies & legislators should include community representatives on site-specific environmental management committees that operate for the term of the project and have ‘teeth’?
  • Community groups must remain active & vigilant?


  • Historically, mining has predated agriculture & other enterprises to ‘kick-start’ local economies, usually in ‘outback’ areas
  • In time, agriculture & pastoral pursuits generally ‘subsume’ land after mining ceases, even though there are on-going environmental legacies
  • Different forms of community development attach to mining & agriculture – community attitudes/perspectives change (and will continue to do so)
  • Legislation drives environmental regulation – community attitudes & perspectives can help to change legislation
  • Knowledge is key – monitoring & acceptance (or not) of impacts of any enterprise on local & regional landscapes ultimately falls to the community
  • Change is inevitable – alertness, communication, regulation, adaptability, science all help

Some mining operations currently on southern Yorke Peninsula

Ardrossan dolomite quarry & port facility  Ardrossan





Klein Point limestone quarry & port operations  Klein Point





Stenhouse Bay gypsum operations  Stenhouse Bay





Price salt pans  Price saltpans





Dr A R Milnes

Rex Minerals’ Hillside Mine – a critique of the proposal

There are components of the Rex Minerals’ Mining Lease Proposal and Management Plan (Hillside Project, east coast of Yorke Peninsula between Ardrossan and Pine Point; dealing with operational environmental management, and closure and rehabilitation of the operation, that are far from ‘best practice’ in the mining industry in this day and age. This is particularly the case with a proposed base metal (including uranium) mining, processing and transport/export operation close to urban infrastructure, existing agricultural landuse and the marine environment.     

Map showing location of proposed Hillside Project in relation to Ardrossan and Pine Point on Yorke Peninsula, South Australia

Map showing location of proposed Hillside Project in relation to Ardrossan and Pine Point on Yorke Peninsula, South Australia

In particular:

1. There is a less than rigorous and transparent approach to describing and managing the uranium content of the targeted ore and its fate in the processing and waste streams. IOCG ores (Olympic Dam, Prominent Hill) always contain uranium. The issue is principally one of radiation protection for the workforce during the operational stage of the operation (especially when mining underground) and the legacy phase following decommissioning and rehabilitation of the contaminated minesite. I’m concerned that there was no mention of mining uranium (even though it is not one of the target metals) in the Referral (EPBC 2012/6434) submitted by Rex in 2012 to the Commonwealth under the Environment Protection and Biodiversity Conservation Act 1999.

2. There is a lack of rigour in the design and management of the TSF, particularly from the viewpoint of adequately engineered and HDPE-lined floor and walls to minimise seepage during operations.

3. The proposal to ‘bury’ the pipelines carrying slurried concentrate and process water between the mine and the port is far from best practice. No experienced mining or energy company will bury pipelines carrying toxic materials because of the inadequacy of leak detection systems (which ideally detect significant leaks) and the inability to make daily inspections along the pipelines to detect small-scale failures and leaks that may be a prelude to significant failure. Examples of companies paying large fines for contaminating the environment as a result of undetected leaks in buried pipelines in Australia (for example, GEMCO’s Groote Eylandt operation – leaking fuel and ERA’s Ranger Mine – leaking tailings pipeline) are well documented.

4. Using the open pit as a final contingency for containing excess leachate from mine landforms and contaminated runoff water and sediment during operations is good practice. However, the lack of a water treatment facility allowing treatment and disposal of pit water may restrict access to the pit (and the underground) following periods when this contingency is required. A water treatment facility would also have considerable value in facilitating mine closure.

5. The proposed rehabilitation strategy is minimal, inadequate in terms of the long-term stability of the post-mining landscape, and espouses the outmoded view that ‘… backfilling the pit and properly rehabilitating the site may sterilise the resource for future operators ….’. To state that the regulator (DMITRE) ‘requires’ this approach is of great concern. It is very unlikely that an operator such as Rex would not fully exploit the existing ore resource and any additional brownfield expansions identified during the mining process. The truth is more likely to be found in the bottom-line economics of the project. By implementing a minimal (and least costly) rehabilitation strategy, the legacy of managing a contaminated base-metal hard-rock minesite such as Hillside, including an open pit part-filled with water of dubious quality, can be passed on to subsequent ‘owners’ and eventually the community and the taxpayer. There are many examples of this dilemma, including former mines at Rum Jungle, Nairne and Mount Todd, where inadequate attention to rehabilitation has left contaminated sites that continue to pollute local and downstream environments.

6. The value of a rehabilitation bond mentioned in the MLP is predicated on approval by the regulator of Rex’s minimal and inadequate rehabilitation strategy. Consequently, in the event that the project becomes uneconomic or for some other reason is curtailed prematurely, there will be significantly less money available than needed to appropriately rehabilitate the mine and port facilities, as well as to manage the post-closure landscape in case there is a legacy of surface erosion, failure of revegetation or contamination of surface and groundwater systems.

7. An appropriate and effective rehabilitation strategy would place all contaminated rock and soil wastes (including tailings and unprocessed ore) back in the pit, which is an effective and stable geological containment structure. The pit would then be backfilled with waste rock and the surface landscape returned, as closely as possible, to the pre-mining condition so that it could be managed in the context of the surrounding landscape and therefore have some value to the local and regional community. There are good examples of this approach (Normandy Woodcutters Ag-Pb-Zn mine near Batchelor and the well-known and widely publicised strategy being implemented by ERA/Rio Tinto at Ranger Mine in the Northern Territory (

8. Pit backfill can be initiated during operations if there is a clear transition from open cut to underground mining. This can be very cost effective in comparison with a post-mining backfill operation, and would minimise costs associated with managing tailings as well as contaminated waste rock and below economic grade ore on the surface. It would require the portal to the proposed underground operation to be located outside the pit or in the highest levels of the pit. This is the approach currently being undertaken at Ranger Mine.

9. The value of the rehabilitation bond should be calculated, based on an independent audit each year, on the full cost of rehabilitating the site (according to a strategy similar to that described above) from the state of the mining, processing and exporting operation each year. This would ensure that the community and the taxpayer are not left with a legacy issue should the operation become uneconomic or for some other reason close prematurely. This circumstance has occurred at many small mines and one current example is the Angus Mine near Strathalbyn, which has been ‘mothballed’ and has an uncertain future.

10. The lack of a water treatment facility and thus a stated reliance on upstream interception, evaporation, and re-injection of ‘surplus’ (waste) water into local groundwater or release into the sea (depending on water quality) is a risky proposition from the perspective of avoidable environmental detriment.

In summary:

Significant effort has gone into the production of the Hillside Mining Lease Proposal and Management Plan as a component of the Pre-Feasibility Study for the Project. The Project is a short-term, large-cost operation and is representative of several new mining proposals in South Australia that are beginning to impinge on modern agricultural (as distinct from outback pastoral) and urban environments. Consequently, local communities and interest groups are rightly demanding a role in the approval process, guarantees that they will benefit from the project, and assurances that the landscape will neither suffer degradation or environmental damage during operations nor be left in a condition after mine closure which has no community value and may require ongoing maintenance.

Unfortunately, much of the plan for the mine described throughout the MLP assumes that there is minimal rehabilitation. That is: (a) the infrastructure will be removed unless there is a downstream benefit to the local community or added value to any subsequent land use by leaving in place storage sheds and associated water and power reticulation. On relinquishment of the site by Rex, the ‘new owner’ will be responsible for any future maintenance and liability; (b) the haul roads will remain in the pit to divert runoff water to the pit lake and these will link to haul roads from the waste rock dumps to form an internal drainage system to divert runoff; (c) the pit and underground will remain as voids filled with water (including contaminated site water), taking more than 500 years to fill to an ‘equilibrium’ level, according to Rex’s modelling, and will be the repository for contaminated sediments and soils as required. Earth bunds will be constructed around the pit to prevent access by light vehicles and will remain ‘in perpetuity’, together with ‘appropriate’ fences and signage, to ‘make it safe’; (d) the waste rock dumps, to be shaped and rehabilitated in-situ, will encapsulate the TSF, any potentially acid-forming waste rock, any ‘uneconomic’ copper ore, and any ‘residual high level radioactive materials’; and (e) the operational water management (drainage) system will be maintained after closure until surface water quality meets the agreed upon water standards for the naturally occurring drainage.

This approach will leave the minesite in a similar condition to many small-scale, short-term, hard-rock base-metal mines throughout the country – that is, areas of major land disturbance and essentially (geomorphically) unstable waste rock landforms that encapsulate environmentally hazardous waste materials from the mining operation, together with pit ‘lakes’ containing contaminated waters. Compared with the pre-mining condition, these areas have no value to the community, but remain places to avoid and, commonly, require major sources of funding from the taxpayer to minimise the ongoing degradation and contain the contamination that can seriously affect downstream environments (note for example, Nairne Pyrite mine, Mount Todd gold mine, Rum Jungle uranium-copper mine). This is unacceptable in this day and age.

Mining companies must take the responsibility to rehabilitate their mining operations in such a way that the post-mining landscape is returned to something approaching the pre-mining condition, which means returning all contaminated wastes to geological encapsulation in the mine pit (or underground), backfilling the pit void to match if possible the former topography, and reconstructing ecosystems (vegetation) that are appropriate and self-sustainable. Under these circumstances, the area should have value to the community (and any future owners) and not represent a shameful and costly environmental legacy.

Dr Tony Milnes (