Answer :
Non-fossiliferous limestones, mudstone, and fine sandstone are all sedimentary rocks, meaning they have been formed by the deposition and compaction of tiny mineral or organic particles.
All three are composed primarily of calcium carbonate (CaCO3). While they may vary in terms of color, texture, and structure, they all have a similar chemical composition and are typically soft and easy to break.
Limestones and mudstones are similar in that they both often contain organic material that is mixed with inorganic material from sources such as calcareous skeletal remains and detrital fragments. While fine sandstone often has small amounts of organic material, it primarily consists of quartz and other siliceous grains.
All three of these sedimentary rocks are often used for decoration or landscaping purposes due to their appearance. Mudstone and fine sandstone have a more unified, grainy texture, whereas limestone typically contains visible shells and fragmented debris making it more visually attractive.
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