This description highlights the differences in permeability between shale and sandstone and how groundwater is stored in geological formations.
In this scenario, sandstone acts as an aquifer, allowing water to permeate through its porous structure. The overlying layer of shale, being relatively impermeable, creates a confining layer that traps water within the sandstone. As groundwater seeps into the sandstone, it can accumulate in the spaces between the grains, providing a valuable water source for aquifers.
When there is a fault line, the movement of tectonic plates can cause displacement of rock layers. In some cases, this movement can bring the impermeable shale layer up to the surface, disrupting the natural flow and storage of groundwater. This can lead to changes in local hydrology, affecting the availability of groundwater resources and potentially influencing surface water bodies.
Understanding these geological formations is essential for water management and environmental studies, as they play a significant role in the hydrology of an area. Proper assessment of aquifers and confining layers is crucial for sustainability, water supply planning, and preventing contamination of groundwater resources.