Leopold Kober (21 September 1883 – 6 September 1970), an influential Austrian geologist, proposed a number of (subsequently largely discredited) theories of orogeny and coined the term kraton to describe stable continental platforms. Kober, developing geosyncline theory, posited that stable blocks known as forelands move toward each other, forcing the sediments of the intervening geosynclinal region to move over the forelands, forming marginal mountain ranges known as Randketten, while leaving an intervening median mass known as the Zwischengebirge.
- "All this made a mockery of the then prevalent Kober-Stillean model of symmetric orogens and vast, rigid Zwischengebirge in between..." Briegel, U. & Xiao, W. (2001), Paradoxes in Geology, p. 187. Elsevier.
- Linton, D. L. & Mosely, F. (1970), 'The Geological Ages', in the Cambridge Ancient History, vol. 1A., pp. 17–18. Cambridge: Cambridge University Press.
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