Definitions
- Describing a crystal structure with one principal axis of symmetry. - Referring to a joint or articulation that moves in one plane or direction. - Talking about an optical device or instrument that has a single axis of rotation.
- Describing a crystal structure with three unequal axes of symmetry, two of which intersect at an oblique angle. - Referring to a geological formation or rock that has a specific type of crystalline structure. - Talking about a type of microscope or polarizing filter that uses light refraction to produce images.
List of Similarities
- 1Both words are used to describe the structure of crystals.
- 2Both words have scientific and technical applications.
- 3Both words are adjectives that modify nouns.
- 4Both words have Greek roots in their etymology.
What is the difference?
- 1Axes: Monaxial refers to one principal axis of symmetry, while monoclinic refers to three unequal axes of symmetry, two of which intersect at an oblique angle.
- 2Geometry: Monaxial describes a crystal structure with a single axis of symmetry, while monoclinic describes a crystal structure with three unequal axes of symmetry.
- 3Usage: Monaxial is more commonly used in the context of joints and optics, while monoclinic is more commonly used in the context of geology and mineralogy.
- 4Symmetry: Monaxial implies a higher degree of symmetry than monoclinic, which has oblique angles and unequal axes.
- 5Complexity: Monoclinic is a more complex and specific term than monaxial, which has a broader range of applications.
Remember this!
Monaxial and monoclinic are both adjectives used to describe the structure of crystals, but they differ in their axes of symmetry, geometry, usage, symmetry, and complexity. Monaxial refers to a crystal structure with one principal axis of symmetry, while monoclinic refers to a crystal structure with three unequal axes of symmetry, two of which intersect at an oblique angle. Monaxial is more commonly used in the context of joints and optics, while monoclinic is more commonly used in the context of geology and mineralogy.
