A break or chip, caused by stress, that is in any direction other than parallel to the planes of atoms in a crystalline mineral. The most common type of fracture appears shell like and is called conchoidal.
Example of a Conchoidal (Shell-Like) Fracture in a Piece of Obsidian.
- Conchoidal Fracture
- Has a curved shell-like appearance. This is the most commonly occurring type of fracture.
- Even Fracture
- These are smooth in appearance but without the single plane regularity of cleavage. This can be seen in some types of quartz.
- Uneven Fracture
- Similar to the edge of broken pottery. This can be found in most all minerals and rocks.
- Splintery Fracture
- This is usually observed in nephrite and hematite. Sometimes this is referred to as fibrous.