Molybdenum

Definition and stakes

1911 Encyclopædia Britannica (1911)

“ Molybdenum disulphide, MoS2, is found as the mineral molybdenite, and may be prepared by heating the trioxide with sulphur or sulphuretted hydrogen. It is a black crystalline powder, resembling graphite in appearance. It is readily oxidized by nitric acid, and when strongly heated in a current of hydrogen is reduced to the metallic condition. Molybdenum trisulphide, MoS3, is obtained by saturating a solution of an alkaline molybdate with sulphuretted hydrogen and adding a mineral acid. It is a brown powder which on heating in air loses sulphur and leaves a residue of the disulphide. ”
Source: Wikisource

Political and commercial geology and the world's mineral resources (1920)

“ It is valuable in electric work.
Up to about 1916 practically all the molybdenum ore (molybdenite, a sulphide of molybdenum) came from Australia and Norway. Shortly after the opening of the war, the molybdenite in Canada became prominent; and later the United States came to the fore as a producer. At present the United States can probably produce as much if not more molybdenum than all the rest of the world put together, principally from the great newly discovered deposits at Climax, Colorado. Before this development, Great Britain was the largest producer, in Australia and Canada.
”
Source: Gutenberg

C. K. Leith,  The Economic Aspect of Geology

“ The world's principal sources of molybdenum ores in approximate order of importance are the United States, Canada, Norway, Australia, Korea, Austria, Peru, and Mexico.
About half of the world's supply is produced in the United States. Production of molybdenum in this country practically began in 1914. Most of the production has come from Colorado and Arizona. It is believed that the United States contains reserves more than sufficient to meet any possible future demand. Thus far the demand has not kept up with capacity for production.
”
Source: Gutenberg

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