Consolidation in geology refers to the processes by which loose, soft sediments are compacted and hardened into solid rock. This typically involves:
- Compaction: As sediments accumulate, the weight of overlying material compresses the lower layers. This pressure reduces the pore spaces between grains by packing them more tightly and expelling water.
- Cementation: Minerals dissolved in groundwater precipitate in the pore spaces, binding the sediment grains together.
Porosity is the measure of the void or pore space within a rock or sediment, expressed as a percentage or fraction of the total volume. The effect of consolidation on porosity:
- As sediments undergo compaction, the grains are pushed closer together, reducing the volume of the pore spaces.
- As cementation occurs, the precipitated minerals fill up some of the remaining pore spaces.
Both compaction and cementation, which are key aspects of consolidation, lead to a
reduction in porosity. Therefore, a
higher degree of consolidation generally leads to lower porosity. Freshly deposited, unconsolidated sediments (e.g., loose sand or mud) typically have higher porosity than their consolidated rock equivalents (e.g., sandstone or shale). Option (a) is incorrect. Option (b) is incorrect. Option (c) is incorrect; there is a clear relationship. Option (d) is correct. \[ \boxed{\text{Higher degree of consolidation leads to lower porosity}} \]