Minerals and Rocks
ЁЯУР Formula & Cheat Sheet (English)
Quick Revision Notes: Class 11 Geography
Chapter: Minerals and Rocks (рдЦрдирд┐рдЬ рдПрд╡рдВ рд╢реИрд▓)
1. Introduction to Minerals (рдЦрдирд┐рдЬ рдкрд░рд┐рдЪрдп)
- Mineral (рдЦрдирд┐рдЬ): A naturally occurring, inorganic, solid substance having a definite chemical composition and atomic structure.
- Key Characteristics:
- Formed by inorganic processes.
- Has a definite chemical composition (
рдирд┐рд╢реНрдЪрд┐рдд рд░рд╛рд╕рд╛рдпрдирд┐рдХ рд╕рдВрдЧрдарди). - Has an internal atomic structure (crystalline form).
2. Physical Characteristics of Minerals (рдЦрдирд┐рдЬ рдХреЗ рднреМрддрд┐рдХ рдЧреБрдг)
Minerals are identified based on their physical properties:
- External Crystal Form (рдмрд╛рд╣реНрдп рдХреНрд░рд┐рд╕реНрдЯрд▓реАрдп рд░реВрдк): Determined by internal arrangement of molecules (cubes, pyramids, hexagonal prisms, etc.).
- Cleavage (рд╡рд┐рджрд▓рди): Tendency to break along planes of weak atomic bonding (results in smooth, flat surfaces).
- Fracture (рднрдВрдЧ): The way a mineral breaks when it does not cleave along flat planes (uneven, conchoidal, hackly).
- Luster (рдЪрдордХ): The appearance of a mineral's surface in reflected light (Metallic, Vitreous/Glassy, Pearly, Silky, Earthy).
- Color (рд░рдВрдЧ): Determined by internal molecular structure (some minerals show color due to impurities like quartz).
- Streak (рдзрд╛рд░рд┐рддрд╛/рдЪреВрд░реНрдг рдХрд╛ рд░рдВрдЧ): The color of a mineral's powder when rubbed on an unglazed porcelain plate.
- Transparency (рдкрд╛рд░рджрд░реНрд╢рд┐рддрд╛): Transparent (рдЖрд░-рдкрд╛рд░), Translucent (рдзреБрдВрдзрд▓рд╛), or Opaque (рдЕрдкрд░рджрд░реНрд╢реА).
- Structure (рд╕рдВрд░рдЪрдирд╛): Particular arrangement of individual grains or crystals (fibrous, bladed, granular, massive).
- Hardness (рдХрдареЛрд░рддрд╛): Resistance to being scratched. Measured on Mohs' Hardness Scale (рдореЛрд╣реНрд╕ рдХрд╛ рдкреИрдорд╛рдирд╛) from 1 to 10.
- Specific Gravity (рд╡рд┐рд╢рд┐рд╖реНрдЯ рдЧреБрд░реБрддреНрд╡): Ratio of the weight of a given volume of the mineral to the weight of an equal volume of water.
3. Mohs' Scale of Hardness (рдореЛрд╣реНрд╕ рдХрд╛ рдХрдареЛрд░рддрд╛ рдкреИрдорд╛рдирд╛)
Standard reference scale to measure mineral hardness (1 = Softest, 10 = Hardest):
- Talc (рдЯреИрд▓реНрдХ) - Softest
- Gypsum (рдЬрд┐рдкреНрд╕рдо)
- Calcite (рдХреИрд▓реНрд╕рд╛рдЗрдЯ)
- Fluorite (рдлреНрд▓реЛрд░рд╛рдЗрдЯ)
- Apatite (рдПрдкреИрдЯрд╛рдЗрдЯ)
- Feldspar (рдлреЗрд▓реНрдбрд╕реНрдкрд╛рд░)
- Quartz (рдХреНрд╡рд╛рд░реНрдЯреНрдЬ)
- Topaz (рдЯреЛрдкрд╛рдЬ)
- Corundum (рдХреЛрд░рдВрдбрдо)
- Diamond (рд╣реАрд░рд╛) - Hardest
4. Major Groups of Minerals (рдЦрдирд┐рдЬ рдХреЗ рдкреНрд░рдореБрдЦ рд╡рд░реНрдЧ)
- Feldspar (рдлреЗрд▓реНрдбрд╕реНрдкрд╛рд░): Half of the earth's crust is composed of feldspar. Color ranges from cream to pink. Used in ceramics and glass making.
- Quartz (рдХреНрд╡рд╛рд░реНрдЯреНрдЬ): Consists of silica. Highly weather-resistant. Used in radio and radar.
- Pyroxene (рдкрд╛рдЗрд░реЛрдХреНрд╕реАрди): Consists of calcium, aluminum, magnesium, iron, and silica. Makes up 10% of the earth's crust. Found in meteorites.
- Amphibole (рдПрдореНрдлреАрдмреЛрд▓): Aluminum, calcium, silica, iron, magnesium. Green or black color. Makes up 7% of earth's crust. Used in asbestos industry.
- Mica (рдЕрднреНрд░рдХ): Contains potassium, aluminum, magnesium, iron, silica. Forms thin sheets. Used in electrical instruments.
- Olivine (рдСрд▓рд┐рд╡рд╛рдЗрди): Magnesium, iron, silica. Used in jewellery; major component of basaltic rocks.
- Other Minerals: Carbonates (Calcite, Dolomite), Sulphides, Oxides, Native Elements (Copper, Gold, Silver).
5. Classification of Rocks (рд╢реИрд▓реЛрдВ рдХрд╛ рд╡рд░реНрдЧреАрдХрд░рдг)
Rocks are aggregates of minerals. Based on their mode of formation, rocks are classified into three major groups:
A. Igneous Rocks (рдЖрдЧреНрдиреЗрдп рд╢реИрд▓ - "Primary Rocks")
- Formed out of magma and lava from the interior of the earth.
- Sub-types based on cooling location:
- Intrusive Igneous Rocks (рдЕрдВрддрд░реНрднреЗрджреА рдЖрдЧреНрдиреЗрдп рд╢реИрд▓): Magma cools slowly deep inside the crust (e.g., Granite, Gabbro, Pegmatite). Forms coarse grains.
- Extrusive Igneous Rocks (рдмрд╣рд┐рд░реНрднреЗрджреА рдЖрдЧреНрдиреЗрдп рд╢реИрд▓): Lava cools rapidly on the earth's surface (e.g., Basalt, Deccan Traps). Forms fine-grained rocks.
B. Sedimentary Rocks (рдЕрд╡рд╕рд╛рджреА рд╢реИрд▓ - "Stratified Rocks")
- Formed through the process of lithification (compaction and cementation of sediments).
- Sub-types based on formation:
- Mechanically Formed (рдпрд╛рдВрддреНрд░рд┐рдХ рд░реВрдк рд╕реЗ рдирд┐рд░реНрдорд┐рдд): Sandstone, Conglomerate, Limestone, Shale, Loess.
- Organically Formed (рдЬреИрд╡рд┐рдХ рд░реВрдк рд╕реЗ рдирд┐рд░реНрдорд┐рдд): Geyserite, Chalk, Limestone, Coal.
- Chemically Formed (рд░рд╛рд╕рд╛рдпрдирд┐рдХ рд░реВрдк рд╕реЗ рдирд┐рд░реНрдорд┐рдд): Chert, Halite, Potash, Gypsum.
C. Metamorphic Rocks (рдХрд╛рдпрд╛рдВрддрд░рд┐рдд рд╢реИрд▓)
- Formed under the influence of heat, pressure, and chemical solutions on pre-existing rocks.
- Types of Metamorphism:
- Dynamic Metamorphism (рдЧрддрд┐рдЯрд┐рдХ рдХрд╛рдпрд╛рдВрддрд░рдг): Caused by mechanical disruption and reorganization due to breaking and crushing without chemical changes.
- Thermal Metamorphism (рддрд╛рдкреАрдп рдХрд╛рдпрд╛рдВрддрд░рдг): Caused by high heat from magma/lava. Divided into Contact Metamorphism and Regional Metamorphism.
- Foliation / Lineation (рдкрд╛рддреАрднрд╡рди / рд░реЗрдЦрди): Arrangement of minerals in parallel lines or layers during metamorphism.
6. The Rock Cycle (рд╢реИрд▓ рдЪрдХреНрд░)
- Definition: The continuous cycle of transformation in which old rocks are converted into new ones.
- Key Steps:
- Magma cools to form Igneous Rocks.
- Igneous rocks weather and erode into sediments, forming Sedimentary Rocks.
- Igneous and Sedimentary rocks undergo extreme heat and pressure to form Metamorphic Rocks.
- Under excessive heat, all rocks melt down into Magma, restarting the cycle.