In his 2002 bestseller Salt: A World History, Mark Kurlansky discusses how salt has historically been essential and valuable to human food, health, trade, and culture. Many places from Salt Lake City—where I live—to Salzburg, Austria have been centers of salt mining and trade.
A new book in two huge volumes published by the American Geophysical Union (AGU) discusses how salt is a core topic within geoscience. While going through these volumes I remembered the late Martin Jackson, one of the pioneer researchers in salt tectonics, whose course I took and who kindly accepted my visit to his salt tectonics lab at The University of Texas at Austin. Let’s look at salt in Earth Science.
Chemical and physical properties of evaporite rocks
Salt deposition in different sedimentary environments
About the author: Webster Mohriak is a professor at Rio de Janeiro State University and has worked in the oil and gas industry for more than three decades. Mohriak has commented on his new publication in a YouTube video.
Stratigraphic distribution of major salt basins:
Neoproterozoic: Salt basins in Australia, Africa, and the Middle East
Cambrian: Middle East
Silurian: North America
Devonian: Eastern Europe
Carboniferous: North and South America
Permian: Europe, North, and South America
Triassic: Central Atlantic rifts
Jurassic: Gulf of Mexico and Central Europe
Cretaceous: South Atlantic margin
Paleogene: Rhine Graben and Iberia
Neogene: North Africa, Red Sea, Dead Sea, Mediterranean, Anatolia
Quaternary: Eastern and Northern Africa, Central Europe
Global distribution of lakes:
Freshwater lakes (54 percent) such as Lake Baikal, Lake Tanganyika, Laker Superior, and Lake Malawi
Salt lakes (46 percent) the largest being Caspian Sea (41 percent)
Salinity of select salt lakes: The average salinity of the oceans is 35 grams of salt per kilogram of water (or 35 parts per thousand).
Highest saline lakes:
Don Juan Pond in Antarctica (403)
Lake Retba in Senegal (400)
Lake Vanda in Antarctica and Lake Karabogaz in Turkmenistan (350)
Lake Assal in Djibouti (348)
Dead Sea in Isreal and Jordan (337)
Low salinity lakes:
Great Salt Lake in Utah (50–270)
Red Sea (36–41)
Mediterranean (38)
Caspian Sea (12)
Major evaporite minerals:
The major evaporite minerals are: Halite, Sylvite, Anhydrite, Gypsum, Magnesite, Calcite
With chemical formulas: Halite (NaCl), Sylvite (KCl), Anhydrite (CaSO4), Gypsum (CaSO4.2H2O), Magnesite (MgCO3), Calcite (CaCO3)
Magnesite (3.0 gram per cubic centimeter) is the densest, and Sylvite (1.86) is the lightest evaporite mineral.
Sylvite is highly radioactive with 500 gamma ray API units.
Modern evaporite environments:
Coastal marine including tidal and sabkha environments
Example: Persian Gulf
Eolian or arid environments including salt flats, shallow brine lakes, and playa (seasonal) lakes between sand dunes
Example: North African Sahara
Lacustrine
Example: Bristol Dry Lake in California
Major salt producers: In 2022, global production of salt was about 290 million tons. The six top producers are (in tons):
China (64,000)
India (45,000)
The United States (42,000)
Germany (15,000)
Australia (13,000)
Canada (11,000)
Fun fact: Next time you receive your salary, remember that the Latin word salarium means “salt money” because in ancient Rome, wages were sometimes paid in salt.
A message from SNH, Cameroon
Call for expression of interest within the scope of a licensing round of nine free blocks of the Cameroon Oil and Gas Domain.
Deadline for submission is 30 March 2026 at noon (local time).
Bottom line: These two volumes offer the most comprehensive coverage of salt geology to researchers and professional geologists.
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