Britain's heritage of science

Научное наследие Британии
Arthur Schuster, A. E. Shipley
1917-01-01

Aymestry limestoneCambrian rocksDelabecheHuttonian theoryOld Red SandstoneSedgwickSilurian systemSt. David's districtWilliam Smithchronological sequencecrystal structurefossilsgeological mappingrock stratauniformitarianism
Great Britain, a geological microcosm-wWilliam Smith, rock strata-Beds of rocks characterized by fossils-Chronological sequence-Hutton and the Huttonian theory-Lyell and Uniformitarianism-Allport, D. Forbes-Sorby, crystal structure-Influence of local surroundings-tThe district of St. David's, oldest rocks in Great Britain-Aymestry limestone-The Silurian system-Sedgwick, Cambrian rocks-Miller, old red sandstone-Delabeche, importance of mapping-The
1
Adam Sedgwick worked on Cambrian rocks, and Miller studied the Old Red Sandstone as significant British formations.
2
Charles Lyell promoted Uniformitarianism, influencing geological interpretation of Britain's formations.
3
Henry De la Beche highlighted the importance of geological mapping for understanding Britain's geology.
4
James Hutton developed the Huttonian theory emphasizing deep time and geological processes shaping Britain’s rocks.
5
Studies by Allport, D. Forbes, and Sorby advanced understanding of crystal structure and the influence of local surroundings on minerals.
6
The Aymestry limestone and the Silurian system were important units in British geological classification.
7
The district of St. David's contains some of the oldest rocks in Great Britain.
8
William Smith identified rock strata in Great Britain using fossil content to establish a chronological sequence of beds.

Great Britain geological record (rock strata and fossil-bearing beds)

Historical development and characterization of Britain's stratigraphy including fossil succession, major rock systems (Silurian, Cambrian, Old Red Sandstone), mapping practices, and influencing theories (Huttonian theory, uniformitarianism)

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1917-01-01
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Arthur Schuster
A. E. Shipley
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