Long-term Cyclic Drift
Cyclic drift is the mechanism of long-term evolution that changes the functional characteristics of a language over time, such as the reversible drifts from SOV word order to SVO and from synthetic inflection to analytic observable as typological parameters in the syntax of language families and of areal groupings of languages open to investigation over long periods of time. Drift in this sense is not language-specific but universal, a consensus achieved over two decades by universalists of the typological school as well as the generativist, notably by Greenberg (1960, 1963), Cowgill (1963), Wittmann (1969), Hodge (1970), Givón (1971), Lakoff (1972), Vennemann (1975) and Reighard (1978).
To the extent that a language is vocabulary cast into the mould of a particular syntax and that the basic structure of the sentence is held together by functional items, with the lexical items filling in the blanks, syntactic change is no doubt what modifies most deeply the physiognomy of a particular language. Syntactic change affects grammar in its morphological and syntactic aspects and is seen as gradual, the product of chain reactions and subject to cyclic drift
The view that the genesis of creole languages or other natural languages may be the product of catastrophism is heavily disputed.
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