2 syllables: chlo, rite. Stress on chlo.
KLAW-reyet
/ˈklɔɹaɪt/
chlorite is pronounced KLAW-reyet (/ˈklɔɹaɪt/). It has two syllables (chlo-rite), with the stress on "chlo". Chlorite is a mineral or chemical compound in which a chlorine-oxygen group is linked with metals or silicates; in minerals it is a member of the chlorite group, typically forming dark green, sheet-like crystals. In chemistry, chlorite refers to the ClO2− anion or related salts. The term is used in geology and inorganic chemistry, often in discussions of mineralogy, petrology, and environmental chemistry.
Chlorite is a mineral or chemical compound in which a chlorine-oxygen group is linked with metals or silicates; in minerals it is a member of the chlorite group, typically forming dark green, sheet-like crystals. In chemistry, chlorite refers to the ClO2− anion or related salts. The term is used in geology and inorganic chemistry, often in discussions of mineralogy, petrology, and environmental chemistry.
"- The chlorite mineral occurs in metamorphic rocks alongside muscovite and biotite."
"- Researchers analyzed chlorite samples to understand fluid composition during metamorphism."
"- Chlorite salts are sometimes used in oxidation-reduction experiments in the lab."
Chlorite is pronounced /ˈklɔːraɪt/ in US and UK usage, with the primary stress on the first syllable: CHLO-rite. The second syllable contains a long “i” sound as in ‘ride’ and ends with a soft 't'. In careful, scientific speech you may hear a brief vowel lengthening on the first syllable: /ˈklɔːr.aɪt/. Note the initial consonant cluster climate—start with a clear 'kl' then 'or' as in 'call', followed by a light 'ite'.
Common errors include misplacing the stress (saying chi-LOR-ite), mispronouncing the ‘chlor’ part as ‘chol’ or ‘chlor’ with a short o, and adding an extra syllable or fading the final -ite. Correct by stressing the first syllable CHLOR- and producing the long vowels: /ˈklɔː.raɪt/. Practice by isolating the two parts: /ˈklɔːr/ then /aɪt/ and connect smoothly.
In US, UK, and AU, chlorite keeps the same two-syllable pattern with primary stress on the first syllable. The main differences lie in the vowel quality: US often uses /ɔː/ as in 'law' plus /raɪt/; UK tends toward a broader /ɔː/ as well; AU is similar but may be slightly broader or flatter in polite or field-specific speech. The final t is released in all; no rhoticity change affects chlorite since the r is part of the first syllable.
The challenge lies in the diphthong /ɔː/ followed by /raɪ/ in a rapid sequence, which can blur into /ɒraɪ/ for non-native speakers. The sequence CHLOR- + -ITE requires precise tongue retraction for /klɔːr/ and a clean, tense /aɪ/ before the final /t/. Additionally, the cluster /kl/ at start and the alveolar /t/ can prompt gendered or regional softening. Focus on the two-part structure and keep the glide distinct.
The critical feature is the strong /klɔː/ onset followed by a clear /raɪt/; there is no silent letter, and the r influences preceding vowel quality in rhotic accents. Some speakers may lengthen the first syllable in formal science talk; maintain a crisp /kl/ onset and a distinct /aɪ/ nucleus. Emphasize not devoicing the final /t/ in careful diction; many speakers stop short in casual speech.
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Chlorite derives from the Greek chloros meaning yellow-green or greenish-yellow, reflecting the mineral’s color. The root chlor- is shared with many chlorine-containing compounds, but in chlorite, the color cue is historical rather than strictly chemical. The suffix -ite is common in mineralogy and chemistry to indicate a mineral, a salt, or a chemical salt form; in minerals, -ite denotes a specific natural solid with a defined composition. The term entered English through 19th-century mineralogical literature as chemists and geologists categorized sheet-silicate minerals with a green appearance. Early descriptions linked chlorite to soapstone or serpentine group rocks, then refined to its distinctive trio of Mg, Fe, or Al-rich sheet minerals. In inorganic chemistry, chlorite can also denote the chlorite ion (ClO2−) in oxo-chemistry discussions, but the mineral name retained its historic usage. First known uses document in mineral catalogs of the early 1800s, with continued refinement as X-ray crystallography and petrography clarified its layered structure. Over time, “chlorite” has carried both geological and chemical senses, particularly in metamorphic petrology, where chlorite’s stability fields inform pressure-temperature histories. Today, the word principally signals Mg-Fe-Al chlorites in rocks and the broader ClO2− chemistry label in labs, with etymology anchored in color observation and mineral taxonomy.
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Words that rhyme with "chlorite"
-ite sounds
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