Hornblende: meaning, definitions and examples
๐
hornblende
[ หhษrnหblษnd ]
mineral composition
Hornblende is a common and important mineral of the amphibole group and is characterized by its complex silicate structure. It typically occurs in igneous and metamorphic rocks and is recognized for its dark green to black color. The mineral often appears in granite and diorite, contributing to the overall composition and texture of these rocks. Hornblende is significant not only for its geological applications but also for understanding the conditions of rock formation.
Synonyms
amphibole, hornblende rock
Examples of usage
- The granite contained a significant amount of hornblende.
- Geologists often study hornblende to reveal the history of rock formation.
- Hornblende crystal structures can indicate the temperature and pressure conditions during metamorphism.
Translations
Translations of the word "hornblende" in other languages:
๐ต๐น hornblende
๐ฎ๐ณ เคนเฅเคฐเฅเคจเคฌเฅเคฒเฅเคเคก
๐ฉ๐ช Hornblende
๐ฎ๐ฉ hornblende
๐บ๐ฆ ะณะพัะฝะฑะปะตะฝะด
๐ต๐ฑ hornblende
๐ฏ๐ต ใใซใณใใฌใณใ
๐ซ๐ท hornblende
๐ช๐ธ hornblende
๐น๐ท hornblende
๐ฐ๐ท ํผ๋ธ๋ ๋
๐ธ๐ฆ ููุฑูุจูููุฏ
๐จ๐ฟ hornblende
๐ธ๐ฐ hornblende
๐จ๐ณ ่ง้ช็ณ
๐ธ๐ฎ hornblende
๐ฎ๐ธ hornblende
๐ฐ๐ฟ ะณะพัะฝะฑะปะตะฝะด
๐ฌ๐ช แฐแแ แแแแแแแ
๐ฆ๐ฟ hornblende
๐ฒ๐ฝ hornblende
Etymology
The term 'hornblende' originates from the German word 'Hornblende', which means 'horn' (from 'Horn') and 'blende' (which refers to a variety of minerals that are commonly shiny or lustrous). The name reflects the mineral's horn-like appearance and its association with other blende minerals. It was first identified in the late 18th century by miners and geologists in Europe, as they examined the diverse mineral compositions of the region's geological formations. Over time, the study of hornblende has expanded, leading to a greater understanding of its role in various rock types and geological processes. The systematic study of hornblende also contributed to the broader field of mineralogy, helping to classify other amphiboles and establishing connections between mineral features and environmental conditions during rock formation. As a result, hornblende remains a subject of interest in both academic research and practical geology.