A sphere is a three-dimensional geometric shape that does not have sides in the traditional sense. A sphere is defined by its curved surface, which is continuous and without any edges or corners. Therefore, a sphere does not have sides, as it is a smooth, continuous surface with no flat faces.
Smooth
3 faces: two plane and one curved,2 edgesno vertices.3 faces: two plane and one curved,2 edgesno vertices.3 faces: two plane and one curved,2 edgesno vertices.3 faces: two plane and one curved,2 edgesno vertices.
Reflections occur when light bounces of a smooth and shiny surface. Glass mirrors have a thin layer of silver on the back so that light is reflected.
Raw diamonds are not naturally smooth, but may have smooth faces: a polished diamond gemstone is smooth.
Diamond
a conchoidial fracture is a "shell-like" fracture with a smooth curved surface
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.
Conchoidal refers to the smooth, shell-like fracture pattern seen in certain minerals and glasses, such as obsidian. It is a type of fracture that produces smooth, curved surfaces resembling the shape of a shell.
In minerals, fracture refers to the way a mineral breaks when subjected to stress. Fracture can be either conchoidal (smooth and curved) or uneven (rough and irregular). It is a useful property for distinguishing between minerals.
Calcite and quartz have a conchoidal fracture, which results in smooth, curved-shaped fractures with characteristic concentric ripples.
Conchoidal describes the smooth, curved, shell-like fracture surface characteristic of some minerals and glasses, such as obsidian. It is a type of fracture pattern that results in smooth, curved surfaces with concentric ridges.
Halite fractures conchoidally, meaning it breaks into smooth, curved surfaces similar to a clamshell. This type of fracture is characteristic of brittle minerals with no preferred cleavage direction.
Fracture in minerals refers to the way a mineral breaks when it is not subjected to cleavage. It can result in irregular, jagged surfaces or smooth, curved surfaces. This property helps in identifying minerals based on how they break.
Conchoidal describes a type of fracture in minerals and rocks, characterized by smooth, curved surfaces resembling the interior of a seashell. It is commonly seen in minerals with strong atomic bonds, such as quartz, obsidian, and flint.
a property called conchoidal fracture, which is characterized by smooth, curved breakage surfaces similar to those seen on broken glass. This type of fracture is common in minerals like quartz, obsidian, and flint.
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.