Slabgrowth

Slabgrowth is a term used in geology and materials science to describe the phenomenon of a solid material increasing in thickness over time due to the accumulation of new layers on its surface. This process is most commonly observed in sedimentary rocks, where layers of sediment are deposited and compacted over geological timescales. Over millions of years, these accumulated layers can form thick strata that constitute large geological formations. The rate of slabgrowth in sedimentary rocks is influenced by factors such as sediment supply, depositional environment, and tectonic activity.

In other contexts, slabgrowth can refer to the intentional or unintentional thickening of artificial slabs, such as concrete slabs used in construction. This can occur due to the addition of new material, such as concrete overlays or screeds, to an existing slab. Environmental factors like freeze-thaw cycles can also contribute to the apparent thickening of concrete slabs through the formation of surface layers or the accumulation of debris. Understanding slabgrowth is crucial for geological analysis, resource exploration, and the long-term durability assessment of engineered structures.