Minerals & Earth's Crust
Minerals vs Elements · 8 Major Crustal Elements · Mineral Composition (28 Micro-Realms)
The Geochemical Building Blocks
About 98% of the total crust of the Earth is composed of just eight major elements—led by Oxygen (46.6%) and Silicon (27.7%). Rather than existing alone, these elements bond inside cooling magma into ordered crystalline Minerals, which in turn aggregate to build the rocks of the lithosphere.
I. Minerals vs. Elements & Fundamental Criteria
Elements vs Minerals
- Element: Pure single atom
- Mineral: Ordered compound
- Elements combine into minerals
5 Criteria of a Mineral
- Naturally occurring & inorganic
- Definite chemical formula
- Ordered atomic structure
Single-Element Minerals
- Gold, Silver & Copper
- Sulphur, Graphite, Diamond
- Uncombined native state
Compound Minerals
- 2 or more elements
- Quartz ($\text{SiO}_2$) & Calcite
- Over 4,000 known species
Mineraloids (Amorphous)
- Lack crystalline lattice
- Opal & Volcanic glass
- Amber & Pearl (organic)
Hot Magma Origin
- Basic source of all minerals
- Crystallizes as magma cools
- Coal & petroleum excepted
Minerals vs Rocks
- Rock: Aggregate of minerals
- No fixed rock formula
- Granite = Quartz + Feldspar
II. The Eight Major Elements of Earth's Crust (NCERT Table 5.1)
The Crustal Eight (98.6%)
- 8 elements = 98.59% weight
- O, Si, Al, Fe, Ca, Na, K, Mg
- Rest 90+ elements = 1.41%
1. Oxygen (46.60%)
- #1 crustal element by weight
- 93.8% of crustal volume
- Bonds into oxides/silicates
2. Silicon (27.72%)
- #2 element in crust
- Tetravalent metalloid
- O + Si = 74.3% of crust
3. Aluminium (8.13%)
- #1 most abundant METAL
- #3 element overall
- Forms SIAL & Feldspars
4. Iron (5.00%)
- #4 in Crust (5.00%)
- #1 in WHOLE Earth (32.1%)
- Sank to core early
5. Calcium & 6. Sodium
- #5 Calcium: 3.63% (Calcite)
- #6 Sodium: 2.83% (Plagioclase)
- Key alkali/alkaline cations
7. Potassium & 8. Magnesium
- #7 Potassium: 2.59% (Orthoclase)
- #8 Magnesium: 2.09% (SIMA)
- Completes top 8 list
Minor & Trace (1.41%)
S · C · Ni (1.41%)
- Titanium (#9 · 0.44%)
- Hydrogen, Phosphorus, Sulphur
- Concentrated in ore veins
III. Crystal Lattices, Bonding & Silica Tetrahedra
Silica Tetrahedron ($\text{SiO}_4^{4-}$)
- 1 central $\text{Si}^{4+}$ ion
- 4 corner $\text{O}^{2-}$ ions
- Fundamental silicate brick
Silicate Polymerization
- Isolated (Olivine) to Chains
- Sheets (Mica) to 3D (Quartz)
- Shared oxygen corners
Mineral Chemical Bonds
- Covalent: Strongest (Diamond)
- Ionic: Soluble (Halite)
- Van der Waals: Weak (Talc)
Polymorphism
- Same formula, different lattice
- Diamond vs Graphite (C)
- Calcite vs Aragonite ($\text{CaCO}_3$)
Isomorphism (Solid Solution)
- Similar-sized ions swap
- $\text{Mg}^{2+} \leftrightarrow \text{Fe}^{2+}$ in Olivine
- Same crystal geometry
Six Crystal Systems
- Cubic, Tetragonal, Hexagonal
- Orthorhombic, Monoclinic, Triclinic
- Internal symmetry axes
IV. Mineral Composition Groups & Bowen's Series
Silicate Dominance (92%)
- 92% of Earth's crust
- Feldspar (50%) + Quartz (12%)
- Primary rock-forming group
Felsic vs Mafic Silicates
- Felsic: Light, K/Na/Al, SIAL
- Mafic: Dark, Mg/Fe, SIMA
- Low vs High specific gravity
Oxide Minerals
- Metal bonded with Oxygen
- Hematite & Magnetite (Fe)
- Bauxite & Corundum (Al)
Carbonate Minerals
- Built on $\text{CO}_3^{2-}$ ion
- Calcite & Dolomite
- Forms Limestone & Marble
Sulphides & Sulphates
- Sulphides: Pyrite, Galena (Pb)
- Chalcopyrite (Cu), Sphalerite
- Sulphates: Gypsum & Barite
Halides & Phosphates
- Halides: Halite ($\text{NaCl}$), Fluorite
- Evaporite salt basins
- Phosphates: Apatite (teeth/bones)
Bowen's Reaction Series
- Magma crystallization order
- First (Hot): Olivine, Ca-Plag
- Last (Cool): Quartz, Muscovite
Core Distinctions
Earth's Crust ("OSiAlFeCaNaKMg"): 1. Oxygen (46.6%), 2. Silicon (27.7%), 3. Aluminium (8.1%), 4. Iron (5.0%). Whole Earth (including Core): 1. Iron (32.1%), 2. Oxygen (30.1%), 3. Silicon (15.1%), 4. Magnesium (13.9%).
2. Element vs. Mineral vs. RockElements (O, Si, Fe) are pure atoms. They combine to form Minerals (Quartz, Feldspar)—naturally occurring inorganic solids with a definite chemical formula. Rocks (Granite, Basalt) are aggregates of one or more minerals with no fixed chemical formula.
3. Most Abundant Mineral in Crust vs. Whole EarthFeldspar is the most abundant mineral group in the Earth's Crust (~50%), followed by Quartz (~12%). Bridgmanite (silicate perovskite in the lower mantle) is the most abundant mineral in the Whole Earth (~38%).
The Crustal Eight (NCERT Table 5.1)
Percentage by Weight in Earth's Crust (98.59% Total)