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The mineral cleavage is made up of many other particles to form a rock when the rock cleavage is just a rock.
Serpentine is a general name for 5 different minerals. These are antigorite, clinochrysotile, lizardite, orthochrysotile, and parachrysotile. Antigorite and lizardite have cleavage in one direction. The others have fracture.
The parent rock of serpentine is called peridotite which is an ultramafic rock
Cobalt has perfect cleavage in all directions.
Serpentine is a type of metamorphosed sedimentary rock.
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The parent rock for Serpentine is ultramafic rock, such as peridotite or dunite. Serpentine forms through the metamorphism of these ultramafic rocks under high pressure and temperature conditions.
Serpentine Rock
Cleavage is a property of minerals. Sandstone is a rock type. As such it doesn't have the property of cleavage.Cleavage is a metamorphic fabric. Sandstone is not a metamorphic rock and thus can not display a cleavage.
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Cleavage is when you can break the rock into square like pieces and Fracture is when you break a rock into uneven different shaped pieces.
Hematite has a characteristic fracture, meaning it breaks irregularly with rough or jagged edges and no smooth cleavage planes.