Linked from

The 18 pages that link to Compaction, each with the reason it gives.

• PorosityRelated: Burial compaction commonly collapses pore spaces and lowers porosity.

• Sedimentary rockRelated: Burial compresses sediment layers and expels some of their water.

• DiagenesisRelated: Burial pressure squeezes sediment, reducing porosity and expelling pore water.

• SandstoneRelated: Compaction reduces pore space and brings sandstone grains into contact.

• Sedimentary basinRelated: Burial compacts basin fill and changes its thickness and pore space.

• LithificationRelated: Burial pressure packs grains and expels pore water, reducing sediment volume during lithification.

• Bulk densityRelated: Compaction reduces void space and usually raises bulk density without changing particle mass.

• Soil liquefactionCompared with: Post-shaking settlement often results from reconsolidation and compaction, not ongoing liquefaction.

• ShaleRelated: Burial pressure compresses muddy sediment during shale formation.

• Niobrara FormationRelated: Burial transformed loose marine deposits into the formation’s solid sedimentary rocks.

• SiltstoneRelated: Burial pressure packs silt grains together during siltstone formation.

• CementationCompared with: Unlike cementation, compaction binds sediment chiefly through pressure-driven grain rearrangement.

• Dirt roadRelated: Compaction helps soil particles resist displacement under vehicle loads.

• MudrockRelated: Compaction reduces pore space as buried mud becomes mudrock.

• Road rollerNarrower topic: A road roller achieves compaction by repeatedly loading the road surface.

• Clastic rockRelated: Burial compacts clastic sediment and brings grains into closer contact.

• Construction aggregateRelated: Compaction brings aggregate particles into closer contact and increases layer stability.

• Isostatic depressionCompared with: Compaction can cause subsidence within sedimentary layers, unlike mantle-displacement-driven depression.