Consolidation (geology)
In geology, consolidation is used in several senses:
- Lithification, the overall process of conversion of loose sediments to solid rock.[1][2]
- Any other process in which loose or fluid material becomes solid rock, such as solidification of magma.[1]
- Compaction (geology), the decrease in volume and increase in density of sediments as the weight of overlying sediments increases, mineral grains move to more compact arrangements, and pore water is expelled.[1] The term is particularly used for soil consolidation.[2]
- Rarely, as a term for the conversion of a mobile belt to a rigid part of a continental platform; an orogeny.[1]
References
[edit]- ^ a b c d Jackson, Julia A., ed. (1997). "consolidation". Glossary of geology (Fourth ed.). Alexandria, Virginia: American Geological Institute. ISBN 0922152349.
- ^ a b Allaby, Michael (2013). A dictionary of geology and earth sciences (Fourth ed.). Oxford: Oxford University Press. ISBN 9780199653065.
Geologic principles and processes | ||
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| Stratigraphic principles |  | |
| Petrologic principles | ||
| Geomorphologic processes | ||
| Sediment transport | ||
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