How Do You Classify Sedimentary Rocks?

Sedimentary rock is classified into two main categories: clastic and chemical. Clastic or detrital sedimentary rocks are made from pieces of bedrock, sediment, derived primarily by mechanical weathering. Clastic rocks may also include chemically weathered sediment.

How Do You Classify Sedimentary Rocks?

Sedimentary rocks are a type of rock formation created by the accumulation of sediment over time. These rocks are classified based on their composition, texture, and structure. Sedimentary rocks are the most common type of rock found on the Earth’s surface, and they often form the basis of our understanding of Earth’s history.

The most common way of classifying sedimentary rocks is based on the composition of the particles that make up the rock. This is known as the chemical classification of sedimentary rocks. This classification is based on the minerals that make up the rock, including quartz, feldspar, and mica.

The second way of classifying sedimentary rocks is based on the texture and structure of the rock. This is known as the textural classification of sedimentary rocks. This classification is based on the size and shape of the sediment particles as well as the way in which they are arranged. Common texture types include clastic, chemical, and organic.

Clastic sedimentary rocks are formed from the accumulation of particles from the erosion of other rocks. These particles can range in size from clay to boulders. Clastic sedimentary rocks are further classified based on the size of the particles that make up the rock.

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