Definition
Granular material such as sand, gravel, or crushed stone used for a variety of purposes, but most commonly in relation to construction activities (Bobrowsky 1998).
Context
Natural aggregates (sand and gravel) occur in various deposits, reflecting different processes of erosion, transportation, abrasion, and deposition often representative of local/regional lithologies and all textural classes. The most common aggregate rich environments are fluvial and glacial deposits, but coastal, marine, desert, and other environments can also be exploited. In a fluvial environment, fine-grained aggregates are more common in meandering river and distal high energy streams conditions, whereas coarser aggregates occur in proximal high energy or braided stream conditions. Glacial environments are by nature more variable in sand and gravel composition but somewhat more predictable when relying on facies analysis and sequence stratigraphy (e.g., glaciofluvial deposits).
Crushed stone aggregate...
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References
Bobrowsky PT (ed) (1998) Aggregate resources: a global perspective. Balkema, Rotterdam
Langer WH (1993) Natural aggregates of the conterminous United States. USGS Bulletin, vol 1594. United States Government, Washington, DC
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Bobrowsky, P.T. (2018). Aggregate. In: Bobrowsky, P.T., Marker, B. (eds) Encyclopedia of Engineering Geology. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-73568-9_9
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DOI: https://doi.org/10.1007/978-3-319-73568-9_9
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