In a previous post, we began discussing some basic
information about rock salt, also known as halite, so you can understand more
about the substance that helps you drive safer each winter. We left off talking
about how halite forms during the evaporation of seas, however we didn’t go
into too much detail about it.
Over 200 million years ago, certain continents were
covered in seas that contained high salt contents. The crystal deposits of rock
salt and table salt form in times when these large bodies of water rapidly
evaporate. The salt forms in large, chunky crystals underground that are later
mined. These underground salt beds can be hundreds of meters thick and span
very broad areas. In North America alone, there are massive salt beds that span
from the Appalachian basin in New York to Ontario. Other deposits are located
in Kansas, Ohio, New Mexico, Nova Scotia, and Saskatchewan. One of the largest
salt beds, producing an average of a million tonnes per year, is in the United
Kingdom at Winsford in Cheshire.
Salt domes are another kind of halite formation in which
vertical pipe-like masses of salt form from underlying salt beds. The weight of
overlying rock essentially squeezes these domes from the ground. Salt domes
also commonly contain gypsum, anhydrite, sulfur, and sylvite. These formations
are commonly seen along the Gulf coast of Texas and Louisiana.
No comments:
Post a Comment