vitreous
Garnets are commonly found as single, well-formed crystals, so they typically exhibit a conchoidal fracture, which is a smoothly curving, shell-like break. This fracture pattern can be observed when garnets are broken or fractured.
Yes, glass does exhibit conchoidal fracture, which is characterized by smooth, curved surfaces resembling the shape of a shell. This type of fracture occurs because glass is an amorphous solid, lacking a crystalline structure, which allows it to break in a way that produces these distinctive curves. The conchoidal fracture is often seen in broken glass edges, making them sharp and jagged.
The rock you are describing is likely a type of peridotite, specifically composed of olivine crystals. Olivine is commonly green, has a hardness of around 6.5 on the Mohs scale, and can exhibit a conchoidal fracture. This non-vesicular rock typically forms in ultramafic igneous environments, such as the Earth's mantle.
The crystals may display a "Crescumulate texture".
Solid crystals have a fixed, ordered arrangement of molecules or atoms, while liquid crystals have a partially ordered structure that can flow like a liquid but still exhibit some properties of a solid. Solid crystals have a defined melting point where they transition to a liquid state, while liquid crystals have a range of temperatures over which they exhibit liquid-like and solid-like properties.
Garnets are commonly found as single, well-formed crystals, so they typically exhibit a conchoidal fracture, which is a smoothly curving, shell-like break. This fracture pattern can be observed when garnets are broken or fractured.
Conchoidal fractures are commonly associated with rocks such as flint, obsidian, and chert. These rocks exhibit a smooth, curved fracture surface similar to the inside of a seashell, which is where the term "conchoidal" originates from.
Yes, glass does exhibit conchoidal fracture, which is characterized by smooth, curved surfaces resembling the shape of a shell. This type of fracture occurs because glass is an amorphous solid, lacking a crystalline structure, which allows it to break in a way that produces these distinctive curves. The conchoidal fracture is often seen in broken glass edges, making them sharp and jagged.
Rocks that contain crystals exhibit a coarse texture. The crystals within the rock are generally large enough to be seen with the naked eye, giving the rock a grainy appearance.
The term you are looking for is "conchoidal fracture," which is common in glasses and some minerals like quartz. This type of fracture produces curved and nested crack surfaces resembling the shape of a seashell, hence the term "conchoidal."
The rock you are describing is likely a type of peridotite, specifically composed of olivine crystals. Olivine is commonly green, has a hardness of around 6.5 on the Mohs scale, and can exhibit a conchoidal fracture. This non-vesicular rock typically forms in ultramafic igneous environments, such as the Earth's mantle.
The fracture of magnetite is typically subconchoidal to uneven, with irregular or jagged edges. It can also exhibit a brittle fracture pattern.
Liquid crystals are unusual because they exhibit properties of both liquids and crystals. They have a distinct molecular ordering like crystals, but are able to flow and change orientation like liquids. This enables them to switch between different phases and exhibit unique optical properties.
yes, they do.
whoever knows please answer below :P
You can find natural crystals most anywhere in the world, depending on what kinds of crystals you want to see. Or your can visit a local natural history museum, a local meteorological exhibit.
The crystals may display a "Crescumulate texture".