Georges Cuvier and Uniformitarianism

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Difference between Georges Cuvier and Uniformitarianism

Georges Cuvier vs. Uniformitarianism

Jean Léopold Nicolas Frédéric, Baron Cuvier (23 August 1769 – 13 May 1832), known as Georges Cuvier, was a French naturalist and zoologist, sometimes referred to as the "founding father of paleontology". Uniformitarianism, also known as the Doctrine of Uniformity,, "The assumption of spatial and temporal invariance of natural laws is by no means unique to geology since it amounts to a warrant for inductive inference which, as Bacon showed nearly four hundred years ago, is the basic mode of reasoning in empirical science.

Abraham Gottlob Werner

Abraham Gottlob Werner (25 September 174930 June 1817) was a German geologist who set out an early theory about the stratification of the Earth's crust and propounded a history of the Earth that came to be known as Neptunism.

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Catastrophism

Catastrophism was the theory that the Earth had largely been shaped by sudden, short-lived, violent events, possibly worldwide in scope.

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Charles Lyell

Sir Charles Lyell, 1st Baronet, (14 November 1797 – 22 February 1875) was a Scottish geologist who popularised the revolutionary work of James Hutton.

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Extinction

In biology, extinction is the termination of an organism or of a group of organisms (taxon), normally a species.

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Geology

Geology (from the Ancient Greek γῆ, gē, i.e. "earth" and -λoγία, -logia, i.e. "study of, discourse") is an earth science concerned with the solid Earth, the rocks of which it is composed, and the processes by which they change over time.

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History of geology

The history of geology is concerned with the development of the natural science of geology.

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History of paleontology

The history of paleontology traces the history of the effort to understand the history of life on Earth by studying the fossil record left behind by living organisms.

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Natural history

Natural history is a domain of inquiry involving organisms including animals, fungi and plants in their environment; leaning more towards observational than experimental methods of study.

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Neptunism

Neptunism, a superseded scientific theory of geology proposed by Abraham Gottlob Werner (1749-1817) in the late 18th century, proposed rocks formed from the crystallisation of minerals in the early Earth's oceans.

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Stratum

In geology and related fields, a stratum (plural: strata) is a layer of sedimentary rock or soil, or igneous rock that were formed at the Earth's surface, with internally consistent characteristics that distinguish it from other layers.

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