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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. ... Desiccation cracks and ripple marks.
H⃣ o⃣ p⃣ e⃣ t⃣ h⃣ i⃣ s⃣ h⃣ e⃣ l⃣ p⃣ s⃣ y⃣ o⃣ u⃣
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