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Serpentine minerals are made of tiny sheets of silica tetrahedrons that are loosely held together.

Sedimentary rock is the type of rock that is loosely held together. They are

usually formed from the deposition of particles at a particular place.

Sedimentary rock formation mostly occur through the accumulation of these

particles which is then followed by cementation to aid the particles to be

held together resulting in the formation of the rock.

Sedimentary rocks are always loosely held together unlike the igneous and

metamorphic which are formed through higher pressure deep in the earth

strata. This makes them to be tightly held together.

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