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Rock salt

General information and occurrence

Polish rock salt deposits are related to two main halite formations: of the Miocene and Zechstein age.

The earliest explored and developed in Poland were deposits of the Miocene formation which are situated in a belt extending from the Silesian region to Wieliczka and Bochnia towns and further eastwards up to the Poland-Ukraine border and running along and close to the present-day frontal overthrust of the Carpathian Mts. on their Foredeep. The exploitation of these deposits ended in 1996 when the salt mining was phased out in the Wieliczka mine. The documented anticipated economic resources of the Miocene rock salt deposits are estimated to be over 4.36 billion tonnes, accounting currently for about 4.8% of the domestic resources. However, a geological structure of these deposits is very complex due to an intense folding (the majority are folded and folded-bedded deposits, except for Rybnik-Żary-Orzesze deposit which is a bedded deposit in a tectonic trough). That complexity of the geological structure along with a markedly varying salt quality and high risks of water flooding and methane inflow to mining works were the reasons why further mining of these deposits became practically uneconomic. The Wieliczka mine was included on the UNESCO World Heritage list in 1978. Nowadays the Wieliczka and Bochnia mines are great tourist attractions and recreation centers.

The Zechstein halite formation is at present the major source of mined salt in Poland. The salt-bearing series are distributed throughout two-thirds of the country area, mainly in the Polish Lowlands. In the Late Permian these areas were occupied by the evaporitic epicontinental basin which was the place of a salt sediments accumulation with the total thickness of over 1,000 m. Bedded rock salt accumulations were documented down to 1,000 m depth in the marginal parts of the basin and in the Łeba Elevation and the Fore-Sudetic Monocline. The anticipated economic resources of these deposits (beyond the protective pillars) are estimated at about 26.15 billion tonnes, which accounts for above 28.9% of domestic salt resources. In turn, in an axial part of the basin (Central Poland) the salt-bearing series are buried at depths up to 7 km, locally rising almost to the surface in salt dome- and pillow-like structures. The salt structures occur in a belt stretching from Wolin in the northwest to the vicinities of Bełchatów town in the south-east. Deposits of the rock salt and potassium-magnesium salt were explored and documented in a number of the shallowest of these structures. The documented anticipated economic resources (beyond protective pillars) of deposits related to the salt structures are estimated at almost 59.81 billion tonnes, which accounts for 66.2% of the domestic salt resources. The exploitation of the latter deposits gives 100% of the current domestic salt production (table 2). The bedded rock-salt deposits have been also documented in the bed of the oldest rock salt – in the overburden of the copper ore deposits in the Fore-Sudetic Monocline (e.g. the rock salt deposit within the copper ore deposit Sieroszowice and forming its part – documented in 2013 – rock salt Bądzów deposit).

The bedded rock-salt deposits are being documented down to the depth of 1,200 m, providing that the deposit series (including partings) is at least 30 m thick and the minimum weighted mean of NaCl in the deposit series and partings equals at least 80%. In accordance with the Polish regulations, salt deposits related to the dome and pillow salt structures are explored down to 1,400 m, providing that the distance between top surface of salt deposits and salt mirror (a protective shelf) is not smaller than 150 m. The remaining requirements are the same as in the case of the bedded deposits. At present, the salt deposits increasingly begin to be treated as the geological objects, especially advantageous for the construction of underground facilities for a storage of crude oil, natural gas and fuels - such as already operating Mogilno II (gas), Góra (fuels) and put into operation in 2014 Kosakowo storage with the active capacity of 4 storage caverns being equal 119 million m3 (within Mechelinki deposit).

In the world, the salt domes are also being used as the safe disposal underground sites for wastes – e.g. Asse and Morsleben domes and Herfa-Neurode and Heilbronn mines in the bedded rock-salt deposits in Germany, or mines located in the bedded potassium and rock salt deposits in the area of Regina (southern Saskatchewan) in Canada. In recent years, in Alberta Province (Canada) the crude oil recovered from so-called bituminous sand is stored, whereas the exploitation wastes are being disposed in caverns within Devonian salt formations: Lotsberg and Prairie.

Resources and output

The anticipated economic resources of rock salt (beyond protective pillars) in 2019 amounted to over 90.32 billion tonnes, decreasing by almost 28.5 million tonnes in the relation to the previous year, whereas the anticipated sub-economic resources remained unchanged. The economic resources dropped by 126.79 million tonnes (almost 6.7% of the domestic resources) due to the ongoing exploitation.

Rock salt deposits in Poland are presented on the map.

Table 1 shows resources and the current state of exploration and development of domestic rock salt deposits. Data refer to resources excluding those within protective pillars.

In 2019, the total domestic output of rock salt amounted to 4,063 thousand tonnes (decreasing by 1.5% in comparison with the previous year), including 2,819 thousand tonnes coming from a solution mining method (Góra and Mogilno I mines – accounting for almost 69.4% of the domestic production, increasing by almost 1.1% year to year, despite the lack of exploitation from Mogilno II deposit). Moreover, 578 thousand tonnes of crushed salt were obtained from Kłodawa 1 deposit (about 14.2% of the domestic production, 4.7% more than in 2018) and from Bądzów deposit – 295 thousand tonnes (almost 7.3% of the domestic production, decreasing by 9.2% in comparison with 2018).

There was also the production coming from the copper ores Sieroszowice mine where 68.28 thousand tonnes of rock salt as the accompanying raw material above cooper ores deposit Sieroszowice were exploited (the more than twofold growth in comparison with 2018).

The production (in the form of brine) from Mechelinki deposit amounted to 370 thousand tonnes (about 9.1% of the domestic production, decreased by almost 14.41% in comparison with 2018) – the brine was dumped to the Bay of Puck.

In 2019 Przedsiębiorstwo Gospodarki Wodnej i Rekultywacji Spółka Akcyjna (in Polish) – the former name: Dębieńsko Desalination Plant Ltd., recovered 68,906 tonnes of evaporated salt from the treatment of brines and salty water from Upper Silesian coal mines. The production increased by 2.8% in comparison with the previous year when.

The figure given below shows changes in resources and production of rock salt in Poland in the years 1989-2019.

The foreseen (prospective and prognostic) resources of rock salt in Poland, assessed to the depth of 2 km, amount to almost 4,060 billion tonnes, including over 4,050 billion tonnes of the Permian salts and 6.9 billion tonnes of the Miocene salts*.


Prepared by: Grzegorz Czapowski

* Czapowski G., Bukowski K., Mazurek S., 2020 - Sól kamienna (rock salt, salt, halites), sole potasowo-magnezowe (potash salts, potassium salts, potassium-magnessium salts). In: Bilans perspektywicznych zasobów kopalin Polski wg stanu na 31.12.2018 r. (eds. Szamałek K., Szuflicki M., Mizerski W.): 218-232. PIG-PIB, Warszawa.