aflejringsmønstrene
Aflejringsmønstrene, often translated as depositional patterns, refer to the observable arrangements and structures within sedimentary rocks that record the processes and environments under which sediments were deposited. These patterns are crucial for geologists in reconstructing past environments, understanding sediment transport mechanisms, and dating geological formations.
Key aflejringsmønstre include stratification, which is the layering of sediments. Different types of stratification exist, such
Other significant aflejringsmønstre include ripple marks, formed by the action of wind or water on sand, and