AIncrease in porosity and melting
BReduction in porosity and hardening of material
CWeathering and fragmentation
DExpansion of volume and cooling
Answer:
B. Reduction in porosity and hardening of material
Read Explanation:
Lithification: Transforming Sediment into Rock
Lithification is the geological process by which loose sediment, such as sand, silt, and clay, is transformed into solid sedimentary rock. This complex process primarily involves two key physical changes:
1. Reduction in Porosity
Definition: Porosity refers to the amount of empty space (pores) within a sediment or rock. During lithification, this pore space is significantly reduced.
Mechanisms:
Compaction: The weight of overlying sediments presses the grains closer together, squeezing out water and reducing the volume of pore spaces. This is particularly effective in fine-grained sediments like clay and silt.
Cementation: Dissolved minerals in groundwater precipitate (crystallize) within the pore spaces. Common cements include calcite, silica (quartz), and iron oxides. These minerals act like glue, binding the sediment grains together and filling the remaining voids.
Significance: Reduced porosity leads to a denser material and limits the ability of fluids (like water or hydrocarbons) to move through the rock.
2. Hardening of Material
Definition: This refers to the transformation of a loose, unconsolidated sediment into a firm, coherent rock.
Processes Contributing to Hardening:
Compaction: As mentioned above, the physical squeezing of grains into closer contact contributes to a more solid structure.
Cementation: The precipitation of cementing minerals is crucial for binding the grains. Without cementation, even compacted sediments might remain relatively loose.
Recrystallization: In some cases, mineral grains may undergo slight changes in shape and size due to pressure and temperature, interlocking more effectively.
Result: The material gains strength and rigidity, becoming resistant to erosion and deformation.
