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Torbern Olof Bergman
(20 Mar 1735 - 8 Jul 1784)

Swedish mineralogist, chemist and naturalist.


Science Quotes by Torbern Olof Bergman (4)

A scientist strives to understand the work of Nature. But with our insufficient talents as scientists, we do not hit upon the truth all at once. We must content ourselves with tracking it down, enveloped in considerable darkness, which leads us to make new mistakes and errors. By diligent examination, we may at length little by little peel off the thickest layers, but we seldom get the core quite free, so that finally we have to be satisfied with a little incomplete knowledge.
— Torbern Olof Bergman
Lecture to the Royal Swedish Academy of Science, 23 May 1764. Quoted in J. A. Schufle 'Torbern Bergman, Earth Scientist', Chymia, 1967, 12, 78.
See also:  |  Enquiry (58)  |  Error (100)  |  Knowledge (341)  |  Scientist (78)  |  Truth (247)

Finally, I aim at giving denominations to things, as agreeable to truth as possible. I am not ignorant that words, like money, possess an ideal value, and that great danger of confusion may be apprehended from a change of names; in the mean time it cannot be denied that chemistry, like the other sciences, was formerly filled with improper names. In different branches of knowledge, we see those matters long since reformed: why then should chemistry, which examines the real nature of things, still adopt vague names, which suggest false ideas, and favour strongly of ignorance and imposition? Besides, there is little doubt but that many corrections may be made without any inconvenience.
— Torbern Olof Bergman
Physical and Chemical Essays (1784), Vol. I, xxxvii.
See also:  |  Chemistry (91)  |  Error (100)  |  Knowledge (341)  |  Name (19)  |  Truth (247)  |  Word (31)

Fossils are of four kinds, viz. saline, earthy, inflammable and metallic; hence arise four classes.
— Torbern Olof Bergman
Outlines of Mineralogy (1783), trans. W. Withering, 12.
See also:  |  Fossil (55)  |  Mineral (14)

The mineral kingdom consists of the fossil substances found in the earth. These are either entirely destitute of organic structure, or, having once possessed it, possess it no longer: such are the petrefactions.
— Torbern Olof Bergman
Outlines of Mineralogy (1783), trans. W. Withering, 5.
See also:  |  Fossil (55)  |  Mineral (14)


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