ANORTHIC Meaning and
Definition
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Anorthic is an adjective that pertains to the field of mineralogy, referring to a specific crystalline structure commonly found in certain minerals. This term describes a crystal system known as the orthorhombic system, characterized by three crystallographic axes (a, b, and c) that are mutually perpendicular to each other but none of them are of equal length. In this system, the crystal symmetry exhibits three-fold rotational symmetry around the axes, and each axis possesses a two-fold rotational axis perpendicular to it.
The term anorthic is derived from the Greek word "an" which means "without" and "orthos" which means "straight" or "right." The prefix "an-" indicates a lack or absence of something, in this context, referring to the absence of right angles in the crystal axes of minerals in the orthorhombic system.
Minerals displaying an anorthic crystal structure typically have elongated or prismatic shapes due to the unequal lengths of the crystallographic axes. Notable examples of minerals with an anorthic structure include topaz, augite, olivine, and orthoclase. The anorthic crystal system is quite common in various types of rocks and plays a crucial role in understanding their formation and subsequent geological processes.
Overall, anorthic denotes the specific crystallographic structure of minerals in the orthorhombic system, characterized by three unequal axes and the absence of right angles between them.
Common Misspellings for ANORTHIC
- znorthic
- snorthic
- wnorthic
- qnorthic
- aborthic
- amorthic
- ajorthic
- ahorthic
- anirthic
- ankrthic
- anlrthic
- anprthic
- an0rthic
- an9rthic
- anoethic
- anodthic
- anofthic
- anotthic
- ano5thic
Etymology of ANORTHIC
The word "anorthic" has its roots in the field of mineralogy. It is derived from the Greek word "anorthos", which means "oblique" or "not straight". It refers to a specific type of crystal structure found in certain minerals where the crystal axes are not at right angles to each other. The term was first introduced and defined by the German mineralogist Johann Friedrich Christian Hessel in the late 18th century. Over time, it became commonly used within the scientific community to describe minerals and rocks with this particular crystal structure.
Similar spelling words for ANORTHIC
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