Construct · 3 fields · 3 citations
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In geology, gradualism is the doctrine that the Earth's features are produced by the same slow, ordinary processes seen acting today (erosion, deposition, uplift) accumulated over immense stretches of time, rather than by sudden catastrophes. Lyell's Principles of geology (1830–1833) made this the working assumption of the science and supplied the deep-time framework it needs. The construct is big change as the sum of many small, steady increments; it is the same tempo that reappears in how species and how societies are held to change.[1]
In political theory, gradualism is the position that lasting social change is best reached by incremental, lawful reform rather than by abrupt revolution, each step consolidating before the next. Bernstein's The preconditions of socialism (1899) argued the reformist, evolutionary road against revolutionary rupture, borrowing the language of evolution itself. It is the same construct (large change built from accumulated small steps over time) realised in institutions and policy rather than rock strata or lineages.[2]
In evolutionary biology, phyletic gradualism is the view that new forms arise by slow, steady, gradual transformation spread across whole lineages, so that the fossil record should show smooth intermediate series. Eldredge and Gould's 1972 Punctuated equilibria: An alternative to phyletic gradualism named this orthodox position precisely in order to contrast it with long stasis broken by rapid change. It is the same slow-accumulation tempo found in Lyell's Earth and in reformist politics, here applied to morphological change through time.[3]
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