Which of the following is the correct ascending order of the given minerals in terms of their presence in the Earth’s crust?
1.Amphibolite
2.Mica
3.Pyroxene
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NDA-I (GAT) Official Paper (Held On: 13 Apr, 2025)
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  1. 2, 3, 1
  2. 1, 2, 3
  3.  2, 1, 3
  4. 1, 3, 2

Answer (Detailed Solution Below)

Option 3 :  2, 1, 3
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Detailed Solution

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The correct answer is 2, 1, 3.

Key Points

  • Amphibolite is a metamorphic rock that primarily consists of amphibole minerals (e.g., hornblende) and plagioclase feldspar. It is less abundant in the Earth's crust compared to silicate minerals.
  • Mica is a group of silicate minerals known for their sheet-like structure. Mica, particularly biotite and muscovite, is more commonly found than amphibole-based rocks in the Earth's crust.
  • Pyroxene is a group of silicate minerals that are more prevalent in the Earth's crust compared to both amphibolite and mica. It is an essential mineral in mafic and ultramafic igneous rocks.
  • The correct ascending order based on their abundance in the Earth's crust is Amphibolite (least abundant), Mica, and Pyroxene (most abundant).
  • This order is consistent with the general distribution of minerals in the Earth's crust, where silicate minerals dominate.

Additional Information

  • Earth's Crust Composition: The Earth's crust is composed primarily of oxygen, silicon, aluminum, iron, calcium, sodium, potassium, and magnesium, with silicate minerals being the most dominant.
  • Silicate Minerals: These minerals form over 90% of the Earth's crust and include groups such as feldspar, quartz, pyroxenes, amphiboles, and micas.
  • Pyroxene Group: Pyroxenes are single-chain inosilicates, commonly found in igneous and metamorphic rocks. They are more abundant than amphiboles.
  • Mica Group: Micas are phyllosilicates and include muscovite (light-colored) and biotite (dark-colored). They are widely distributed but less abundant than pyroxenes.
  • Amphiboles: Amphiboles are double-chain inosilicates and are typically found in metamorphic rocks like amphibolite, which are less common than mica and pyroxene in the crust.
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