Answer:
Step-by-step explanation:
Bedding. Bedding is often the most obvious feature of a sedimentary rock and consists of lines called bedding planes, which mark the boundaries of different layers of sediment. .
Graded beds are common when a sediment is being deposited by a slow‐moving current.
Fossils.
Desiccation cracks and ripple marks.
Sedimentary rocks contain rounded grains in layers. The oldest layers are at the bottom and the youngest layers are at the top. Sedimentary rocks may contain fossils of animals and plants trapped in the sediments as the rock was formed.