Clinopyroxene definitions
| Word backwards | enexoryponilc |
|---|---|
| Part of speech | Noun |
| Syllabic division | cli-no-py-ro-xene |
| Plural | The plural of clinopyroxene is clinopyroxenes. |
| Total letters | 13 |
| Vogais (3) | i,o,e |
| Consonants (7) | c,l,n,p,y,r,x |
Clinopyroxene is a group of inosilicate minerals found in many types of igneous and metamorphic rocks. It is characterized by its monoclinic crystal system and a chemical formula that typically includes calcium, sodium, magnesium, iron, and aluminum.
Formation and Occurrence
Clinopyroxene forms as a result of the crystallization of magma deep within the Earth's crust. It is commonly found in basaltic rocks, such as gabbros and basalts, as well as in some metamorphic rocks. The mineral can also be found in some meteorites and lunar samples.
Physical and Optical Properties
Clinopyroxene typically appears as dark green, brown, or black crystals with a vitreous to dull luster. It has a Mohs hardness of around 5 to 7, making it relatively hard compared to other minerals. The mineral has two distinct cleavage directions, making it easy to cleave into prismatic or tabular fragments.
Uses and Significance
Clinopyroxene is an essential mineral for petrologists and geologists as it provides valuable information about the formation and evolution of rocks. Its presence in certain rock types can indicate specific tectonic environments or magma compositions. Additionally, studying clinopyroxene can help geoscientists understand the thermal and chemical history of a particular region.
In conclusion, clinopyroxene is a significant mineral in the field of geology, providing insights into the Earth's processes and history through its unique properties and occurrences. Its presence in various rock types contributes to our understanding of the planet's geological evolution.
Clinopyroxene Examples
- The mineral composition of the rock sample indicated the presence of clinopyroxene.
- Researchers studied the arrangement of clinopyroxene crystals under a microscope.
- The geologist identified the clinopyroxene mineral based on its distinct cleavage.
- The chemical composition of clinopyroxene is commonly found in mafic rocks.
- Thin sections of the rock were analyzed to determine the abundance of clinopyroxene.
- The clinopyroxene mineral group includes diopside, augite, and jadeite.
- The presence of clinopyroxene in the sample suggested high pressure and temperature conditions during formation.
- Petrologists use clinopyroxene as an indicator mineral for the classification of igneous rocks.
- The color and texture of clinopyroxene crystals can vary depending on the chemical composition.
- Scientists use X-ray diffraction to analyze the crystal structure of clinopyroxene minerals.