In geology, sedimentary rocks are typically divided into distinct layers known as "beds" or "strata." These layers are formed as sediment accumulates and is deposited over time. Each layer represents a distinct period of deposition and can vary in thickness, composition, color, and texture.
The process of layering in sedimentary rocks is often referred to as "stratification." Stratification occurs as sediments settle and form horizontal layers or beds. These layers can range in scale from millimeters to meters thick, depending on the depositional environment and the sedimentary process involved.
The study of these sedimentary layers and their characteristics can provide valuable information about past environments, geological history, and the processes that formed the rock. It allows geologists to interpret the conditions under which the sediment was deposited and provides insights into Earth's history.
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