If water is observed freely seeping from the exposed sides of a cut, what is the most likely soil type?

Water seeping from the exposed sides of a cut is indicative of the presence of granular or coarse-textured soils, which are more permeable. Soil types are categorized based on their properties, including cohesion and grain size. Type C soils, classified as coarse-grained soils with little or no cohesion, include sands and gravels. These soils often allow for easy movement of water through their structure, leading to observable seepage.

In contrast, Type A soils are cohesive, clayey soils that generally hold water and do not allow for free draining or seepage. Type B soils have a mix of cohesive and granular properties, which can have moderate permeability but are not as prone to free seepage as Type C soils. Type D soils consist mainly of organic material or silty soils, which typically retain moisture and may also inhibit free drainage.

Considering these classifications, the observed behavior of water freely seeping suggests the characteristics aligned with Type C soils, making it the most appropriate choice.