Pyrite can form in a myriad of different crystal habits. Primary pyrite habits such as framboid, colloform and spheroidal textures are those most often associated with growth in soft sediments. Cubes and the more characteristic forms are associated with increased P-T conditions and recrystallisation. So, the reason pyrite has many shapes is because it can be found in virtually every rock type, it is generally rigid and stable at temperatures up to ~743 degrees and so throughout its history it will be affected by a number of different factors which may alter crystal forms. Why and how certain textures grow is still contentious
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Pyrite can have various shapes due to its crystal structure, which allows it to form different geometric patterns. Additionally, environmental factors during its formation, such as pressure and temperature changes, can influence the growth of pyrite crystals, resulting in a variety of shapes.
Sulfides
Pyrite belongs to the sulfide mineral group. It is composed of iron and sulfur, with a chemical formula FeS2.
Pyrite is sometimes called fool's gold because of its metallic luster and pale brass-yellow hue, which can resemble real gold to the untrained eye. However, pyrite is a different mineral with a lower value and hardness compared to gold.
Pyrite is a mineral that has a streak that is greenish black, even though its external color is brassy yellow. This difference in color is due to the oxidation of iron in pyrite.
No, pyrite is not radioactive. Pyrite is a naturally occurring mineral that is composed of iron and sulfur, and its chemical composition does not include radioactive elements.