How Do You Spell THEOPARACELSITE?

Pronunciation: [θiːəpˈaɹe͡ɪslsˌa͡ɪt] (IPA)

"Theoparacelsite" is a mineral discovered in Bologna, Italy in 2003. The word comprises of several phonemes that can be transcribed using IPA phonetic transcription. The first three letters "theo" are pronounced with a voiced dental fricative /ð/ in English. Followed by "para" which has two syllables, each with a short vowel sound: /pærə/. The last part of the word "celsite" has two syllables with the first syllable having the same short vowel sound as the second syllable of "para". The second syllable has a long vowel sound /si:l/. When combined, the word is pronounced as "θiɒpærəselʃaɪt".

THEOPARACELSITE Meaning and Definition

  1. Theoparacelsite is a rare mineral that belongs to the sulfate class of minerals. It is primarily composed of lead, copper, and sulfur, with chemical formula Cu3Pb(AsO4)2(SO4)(OH)2. The mineral derives its name from the combination of the Greek word "theos," meaning god, and the name of the Swiss alchemist and physician Paracelsus.

    Theoparacelsite typically forms in the oxidized zone of lead and copper-rich hydrothermal deposits. It occurs as small, translucent to transparent prismatic crystals or as grainy aggregates. The crystal structure of theoparacelsite is orthorhombic, meaning it possesses three mutually perpendicular axes of different lengths.

    The mineral frequently exhibits a yellow to greenish-yellow coloration, often with a vitreous to pearly luster on crystal surfaces. It has a Mohs hardness of approximately 2.5 to 3, indicating a relatively low scratch resistance. The specific gravity of theoparacelsite ranges around 5.9.

    Due to its scarcity and limited occurrences, theoparacelsite has limited practical uses. However, it is considered a valuable specimen among mineral collectors and enthusiasts. Its intricate crystal formations, vibrant coloration, and association with notable historical figures such as Paracelsus make it desirable for display and study purposes.

    While the mineral itself may not hold significant industrial importance, its unique composition and formation provide valuable insights into the geological processes and conditions that contribute to the formation of hydrothermal mineral deposits.