The mineral cleavage is made up of many other particles to form a rock when the rock cleavage is just a rock.
Density would be the most noticeable difference between the rock and the model.
You can tell if a mineral is a mineral by its characteristics: *color *luster *streak *hardness *cleavage/fracture *crystalline structure
The fracture type of the Pumice rock is either jagged or splintery. The Pumice has both fracture and cleavage type.
No. A rock is an assemblage of at least two different minerals. One mineral can't be two or more minerals.
That means when you break it it will form a smooth flat surface. Slate has near perfect cleavage so it's used to make pool tables and blackboards.
I dont think so because a rock can not have cleavage, but a mineral can
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.
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.
Rock salt.
It is a type of igneous or sedimentary rock.
The term is called CLEAVAGE. It is a special form of Foliation in rock metamorphism.
In lesser terms, oxidation is when a rock or mineral of some sort interacts with oxygen and carbonation is when a rock or mineral interacts with carbon or carbon dioxide.
In lesser terms, oxidation is when a rock or mineral of some sort interacts with oxygen and carbonation is when a rock or mineral interacts with carbon or carbon dioxide.
A mineral's ability to split easily along planes of weakness, producing flat surfaces.
Magma is molten rock, the dissolved mineral remains of solid rock. During cooling and solidification, the magma will crystallize into a mass of crystallized mineral components.
Magma is molten rock. A mineral is a naturally occurring inorganic solid, with a definite chemical formula, and a crystalline structure.
Magma is molten rock. A mineral is a naturally occurring inorganic solid, with a definite chemical formula, and a crystalline structure.