Origins and deposits

Rock salt, Zechstein salt, salt from the Röt Formation or from the Muschelkalk (shell-bearing limestone), and Jurassic salt: there is a vast range of salt deposits that differ distinctly from one another as regards their age and geology. Sodium chloride – the chemical name for salt – consists of the metallic element sodium and the gaseous element chlorine.

Bex Toursime

Halite/rock salt

The phrase “salt of the earth” is used with symbolic meaning in the bible, but it also reminds us that salt is closely linked to the earth and its history. Halite (as rock salt is known) is derived from the Greek words “hals” for salt and “lithos” for stone.

Rock salt is one of the softest minerals, with a hardness value of 2 (the value for diamonds is 10). The basic form of salt is a perfect cube (a hexahedron or a body with six surfaces). A crystal of common salt consists of a “cubic face-centered” crystal lattice of sodium and chlorine ions. In this configuration, one sodium (Na) ion is symmetrically surrounded by six chlorine (Cl) ions, and each Cl ion is surrounded by six Na ions.

Halite crystallizes strictly in accordance with the rules of the cubic crystal system. This has been proven by laboratory experiments under a variety of different solution conditions. There are no exceptions to the rule for any of the crystallized forms – octahedron (with eight surfaces), rhombic dodecahedron (with twelve surfaces), whisker (needle-shaped) or dendrite (scale).

Halite or rock salt is classified as one of the evaporite rocks (minerals formed through evaporation), created by precipitation when the water in a salt lake or lagoon dries up. As well as salt, other minerals are left behind, such as sylvite (potassium chloride, KCl), gypsum (calcium sulphate, CaSO4, 2H2O), lime (calcium carbonate, CaCO3), dolomite (calcium/magnesium carbonate, CaMg(CO3)2) and anhydrite (gypsum with no water content). The precipitation process always follows the same rules. The influx of new water disrupts the process and the minerals can either dissolve again or be covered by new layers (cf. the bar theory).

Zechstein salt

The most substantial and widespread rock salt deposit in Central Europe originates from the Zechstein era, with numerous salt cycles that were created as the sea advanced and retreated. The thickness of the cycle layers varies from 100 to 600 metres. Four to six cycles of Zechstein salt contain potassium (potash) salts. Zechstein salt was partially covered over by younger rock layers that are over 2,000 metres thick. The pressure exerted by these layers caused the salt to flow and rise upwards towards the earth’s surface. Huge salt domes (diapirs) were formed. These diapirs are used to extract rock salt and potassium salt, to collect oil and natural gas, and for the final storage of waste.

Upper Permian/Werfenian salt

Includes the salt deposits in the Eastern Alps, especially in the region of Hall im Tirol, Berchtesgaden, Bad Ischel, Hallstatt and Altaussee. They were only shifted from the south, away from the area where they were deposited in the Tethys, during the formation of the Alpine mountain range. These salt deposits are not layered, but are folded and accreted with other rocks (as denoted by the term “Haselgebirge Formation”); they are therefore heavily interspersed with clay, anhydrite and dolomite (low salt content).

Geologische Bezeichnung: Oberes Perm
Vor ca. Mio. Jahren: 245
Verbreitung: Österreich und Bayern (Hallein bis Altausee)

Röt salt

This salt, in layers of between 60 and 80 metres, is mainly known from oil drilling operations. It is extracted by leaching at a location in Hengelo (Netherlands), from a depth of 300 to 400 metres.

Muschelkalk (shell-bearing limestone) salt

This salt was created 235 million years ago as the sea advanced from what is now the area of the North Sea, and it extends into Switzerland and Eastern France. The layers attain a maximum thickness of 100 metres. This salt aroused interest at an early stage because it feeds numerous inland salt springs, making it possible to extract salt. More modern extraction methods have added to the importance of Muschelkalk salt. It does not contain any potassium salts and is frequently interspersed with anhydrite, clay and dolomite.

The Swiss Saltworks at Schweizerhalle and Riburg obtain their salt by leaching from this Muschelkalk rock salt. Other important extraction locations include Heilbronn and Stetten in Germany, and Varangeville, Tavaux and Dombasle in Lorraine. The salt is extracted as rock salt with the help of mining techniques, but is then stored as evaporated salt. See the illustration: «Salt in Switzerland».

Keuper salt

In the Keuper (Upper Triassic), evaporite rock (mainly gypsum and anhydrite) was again precipitated in Central Europe 225 million years ago. Regional saliniferous basins are located in this rock, for example in Cheshire (UK), Nancy (France) and in Lons-le-Saunier (Jura). They are less than 100 metres thick and their quality is modest.

The isolated salt deposit at Bex (in the canton of Vaud) in the Rhone valley is also Keuper salt, but it originates from the southern section of today’s Alps. Like Haselgebirge, this is a breccia (or mix of rocks) which is interspersed with salt. The salt content is low.

Jura (Jurassic) salts

Precipitations of salt also occurred in Central Europe during the Jurassic era, about 150 million years ago. No use of these salt deposits is known.

Tertiary salts

In the Cretaceous period (145 to 65 million years ago), saliniferous formations remained limited to the Mediterranean region. It was only in the Lower Tertiary that salt deposits were formed north of the Alps again, 40 million years ago. These include the deposits of rock salt and potash salt in the Rhine Rift Valley between the Black Forest and the Vosges (Eocene/Oligocene), the substantial Bresse salt deposit (gas storage) and the deposits that have been exploited since the Middle Ages along the Carpathian Foredeep Basin in Wieliczka and Bochnia (both in Poland).