This has been answered before but there was no explanation given for the curve. Materials that do not have fracture planes such as glass and obsidian (a natural glass-like mineral) do not follow any particular structural arrangement when fracturing. The curve results from the distribution of stresses radiating from the fracture start point. The fracture pattern is called conchoidal.
The fracture can be described (depending on the mineral) as:-Conchoidal fractureSubconchoidal fractureEarthy fractureHackly fractureJagged fractureSplintery fractureUneven fracture
The type of rock formed from a pyrite crystal breaking into pieces with smoothly curved edges is conchoidal fracture, which is a type of fracture commonly seen in minerals like quartz and obsidian. This fracture pattern results in smooth, curved surfaces resembling the shape of a clamshell.
The mineral quartz show the property of fracture. it breaks along a curved surface. this kind of fracture is called conchoidal fracture. In math the quartz is x3.
Peridot typically exhibits a conchoidal fracture, meaning it breaks in a smooth, curved manner like glass. It does not have a distinctive cleavage pattern due to its crystalline structure.
Conchoidal is a type of fracture that occurs in minerals or stones, characterized by smooth, curved surfaces that resemble the shape of a clamshell. This fracture pattern is commonly seen in materials like obsidian and quartz.
A fracture that breaks along smooth, curved surfaces is called a conchoidal fracture. This type of fracture is commonly observed in materials like glass and minerals with a crystalline structure.
The fracture can be described (depending on the mineral) as:-Conchoidal fractureSubconchoidal fractureEarthy fractureHackly fractureJagged fractureSplintery fractureUneven fracture
Yes, obsidian exhibits conchoidal fracture, which is a smooth, curved breakage pattern characterized by concentric ridges. This is due to its lack of internal crystal structure, which causes it to break in a unique, curved manner.
This is known as conchoidal fracture.
The type of rock formed from a pyrite crystal breaking into pieces with smoothly curved edges is conchoidal fracture, which is a type of fracture commonly seen in minerals like quartz and obsidian. This fracture pattern results in smooth, curved surfaces resembling the shape of a clamshell.
This unique arclike pattern that forms when flint and opals break is called a concoidal fracture. It is characterized by smooth, curved surfaces with concentric ridges radiating from the point of impact, resembling the shape of an arc or horseshoe. This fracture pattern is distinct and useful in identifying these minerals.
The mineral quartz show the property of fracture. it breaks along a curved surface. this kind of fracture is called conchoidal fracture. In math the quartz is x3.
a conchoidial fracture is a "shell-like" fracture with a smooth curved surface
This is known as conchoidal fracture.
the manner in which a mineral breaks along either curved or irregular surfaces is called a FRACTURE.
the manner in which a mineral breaks along either curved or irregular surfaces is called a FRACTURE.
Yes, amethyst minerals can exhibit a conchoidal fracture, which is characterized by smoothly curved breakage surfaces similar to glass. This fracture pattern is a common trait in amethyst, especially when it is subjected to stress or impact.