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Wentworth Grade Scale

sedimentology

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In sedimentology, a grain size scale divides a continuous range of particle sizes into discrete groups for standardization and statistical analysis. The Udden-Wentworth scale, adapted from J.A. Udden's work, is widely adopted. This scale categorizes particles from finest to coarsest as clay, silt, sand, granules, gravel, pebbles, cobbles, and boulders. The specific size limits for each category can vary between different scales. Grain size is a crucial textural parameter in clastic sedimentary rocks, offering insights into the conditions of sediment transportation, sorting, and deposition, as well as events at the depositional site before lithification.12

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