Bedding
The presence of layers is the universal feature of all sedimentary rock.
Stratification.
no its sedimentary rock feature
Porphyritic
Bedding
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Sedimentary rocks are often deposited in layers as strata. The feature that tells how a sedimentary rock is layered is called the bedding.
Stratification. The existence of layers.
The feature common to nearly every type of sedimentary rock is layering, known as stratification, which is formed by the accumulation and compaction of sediments over time. This layering provides information about the environment in which the rock was formed.
Correct, porphyritic texture is typically associated with igneous rocks and is not a common feature of sedimentary rocks. It is characterized by larger crystals, known as phenocrysts, surrounded by a fine-grained or glassy matrix. Sedimentary rocks are formed through the accumulation and lithification of sediments, which do not typically undergo the same crystallization processes as igneous rocks.
Unconformity