It has both cleavage and fracture.
Plagioclase feldspar is a non-metallic mineral. It has 2 cleavages at nearly right angles. It is also differentiated from potassium feldspar because it contains striations. Potassium feldspar has 2 cleavages at nearly right angles.
Feldspar's fracture is brittle
The term used to describe the shape of a mineral that has three directions of cleavage intersecting at 90-degree angles is "cubic" or "isometric." Minerals that exhibit this type of cleavage typically form cubic crystal systems, such as halite or pyrite. This characteristic cleavage results in the mineral breaking along smooth, flat surfaces that create cube-shaped fragments.
cleavage lines
Feldspar is commonly used in the production of ceramics and glass, contributing to their strength and durability. It's also utilized as a filler in paints, plastics, and rubber to improve texture and enhance properties. Additionally, feldspar plays a role in the manufacturing of tiles and sanitary ware, making it an essential material in construction and home decor.
feldspar
Feldspar.
Orthoclase Feldspar.
Feldspar exhibits two directions of perfect cleavage that intersect at approximately 90 degrees. This characteristic allows feldspar crystals to break along these planes, resulting in smooth surfaces. The cleavages are typically observed in two forms: one that is more prominent and can be seen in plagioclase feldspar, and another that is more subtle in potassium feldspar. This cleavage is a key diagnostic feature in identifying feldspar minerals.
2 at 90 degreesHere is a discussion on feldspar.It says it has uneven fracture and cleavage in 2 directions.http://www.theimage.com/mineral/feldspar/index.htm
Plagioclase feldspar is a non-metallic mineral. It has 2 cleavages at nearly right angles. It is also differentiated from potassium feldspar because it contains striations. Potassium feldspar has 2 cleavages at nearly right angles.
Cleavage and Fracture
Calcite can be identified by its rhombohedral cleavage and effervescence in acid. Feldspar can be identified by its two cleavage planes at nearly 90 degrees, and it often has a white to pink color. Both minerals can also be identified by their hardness using the Mohs scale.
Cleavage is a minerals ability to break into even pieces useful for identification. Cleavage in two directions equals Feldspar for example.
Two directions of cleavage, at 90 degrees to each other.
Step-like cleavage is a property of the mineral mica. Mica minerals exhibit a planar arrangement of atoms that allow them to easily separate along flat surfaces, giving them a distinctive step-like appearance when broken or cleaved.
Orthoclase feldspar typically exhibits two cleavage planes at right angles to each other, forming blocky or prismatic shapes. Plagioclase feldspar, on the other hand, shows two cleavages at nearly 90 degrees but often also has a third cleavage at a slightly different angle, resulting in more varied forms.