The word "olivinoid" is spelled with the combination of letters "oi" followed by the letter "v" and ending with the suffix "-oid". The IPA phonetic transcription for this word is /ˌɑlɪˈvɪnɔɪd/. The first syllable begins with the "ah" sound, followed by the "li" sound, then "vin" and "oi" with a slight dip in pitch, and ending with the "d" sound. This word describes minerals that resemble olivine, a common mineral found in volcanic rocks.
Olivinoid is a term that refers to a rock or mineral displaying properties and characteristics similar to olivine, a common silicate mineral found in igneous rocks. Olivine is composed of magnesium, iron, and silicate, and is typically green in color.
In geological terms, olivinoid refers to any rock or mineral that possesses a similar composition, structure, or physical appearance to olivine. This means that an olivinoid substance may contain a high concentration of magnesium, iron, and silicate, and may have a distinct green color or show a characteristic crystal structure resembling olivine.
The term olivinoid can apply to various rock formations or minerals, such as certain igneous rocks like basalt or peridotite, which are known for their high olivine content. It can also encompass metamorphic or sedimentary rocks that have undergone chemical or physical changes over time due to heat, pressure, or weathering.
Olivinoid minerals are of interest to scientists and geologists because they can provide important clues about the geological history and processes that occurred within a particular region. Additionally, they have various applications in industries like construction, as olivinoid rocks are often used as building materials or as abrasives due to their hardness.
A substance occurring in meteorites resembling olivine.
Etymological and pronouncing dictionary of the English language. By Stormonth, James, Phelp, P. H. Published 1874.
The term olivinoid is derived from the mineral olivine. Olivine is a common silicate mineral that is composed of magnesium, iron, and other elements. It has a characteristic green color and is commonly found in igneous rocks such as basalt and peridotite. The word olivinoid is used to describe substances or materials that have similarities to olivine in terms of color, composition, or other physical properties. The suffix -oid is used in English to indicate resemblance or similarity to something. Hence, olivinoid essentially means resembling or similar to olivine.