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11.3: Soil Classification

  • Page ID
    63425
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    Some of the compliance methods permitted under the Excavation standards require a competent person to classify soil and rock deposits as: (1) Stable rock; (2) Type A soil; (3) Type B soil; and (4) Type C soil.

    Stable Rock – Natural solid mineral matter that can be excavated with vertical sides and remain intact while exposed. Type A – Cohesive soils with an unconfined compressive strength of 1.5 tons per square foot (tsf) (144 kPa) or greater. Examples include clay, silty clay, sandy clay, and clay loam. Certain conditions preclude soil from being classified as Type A. For example, no soil is Type A if it is fissured or has been previously disturbed. Type B – Includes cohesive soil with an unconfined compressive strength greater than 0.5 tsf (48 kPa) but less than 1.5 tsf (144 kPa) and granular cohesionless soils (such as angular gravel, similar to crushed rock, silt, silt loam, sandy loam, and, in some cases, silty clay loam and sandy clay loam). Type C – Cohesive soil with an unconfined compressive strength of 0.5 tsf (48 kPa) or less, granular soils (including gravel, sand, and loamy sand), submerged soil or soil from which water is freely seeping, submerged rock that is not stable, or material in a sloped, layered system where the layers dip into the excavation or with a slope of four horizontal to one vertical (4H:1V) or steeper.


    This page titled 11.3: Soil Classification was last modified on Fri, 14 Aug 2026 17:00:21 GMT and is shared under a CC BY 4.0 license and was authored, remixed, and/or curated by Jenny Huang.