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    Match List - I with List – II Choose the correct answer from the options given below:
    Question



    Match List - I with List – II

    Choose the correct answer from the options given below:

    A.

    (A) – (IV), (B) – (III), (C) – (II), (D) – (I)

    B.

    (A) – (III), (B) – (II), (C) – (I), (D) – (IV)

    C.

    (A) – (II), (B) – (I), (C) – (IV), (D) – (III)

    D.

    (A) – (IV), (B) – (I), (C) – (II), (D) – (III)

    Correct option is A

    Explanation:
    · (A) Dissolution of calcite → (IV) Travertine Calcite dissolves in carbonic acid and reprecipitates as travertine in hot springs and caves.
    · (B) Oxidation of olivine → (III) Hematite Olivine contains iron which, when oxidized, forms iron oxides like hematite (Fe₂O₃).
    · (C) Hydrolysis of orthoclase → (II) Kaolinite Orthoclase (a feldspar) undergoes chemical weathering, resulting in the formation of kaolinite, a clay mineral.
    · (D) Hydrolysis of quartz → (I) Chert Although quartz is resistant, prolonged weathering can dissolve silica which reprecipitates as microcrystalline quartz (chert).
    Information Booster:
    · Travertine is a form of limestone resulting from the precipitation of calcium carbonate, often from dissolved calcite. Hematite forms through oxidation of ferromagnesian minerals like olivine. Kaolinite is a clay mineral formed from feldspar hydrolysis. Chert, composed of microcrystalline silica, originates from quartz dissolution and reprecipitation, often in marine environments.
    Additional Knowledge:
    · Option (2): Incorrect – Dissolution of calcite forms travertine, not hematite.
    · Option (3): Incorrect – Olivine forms hematite, not chert.
    · Option (4): Incorrect – Olivine and chert are mismatched; orthoclase does not form chert.

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