ASKiIMAN™ ARCHIVE / PHYSICAL GEOGRAPHY
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WORLD C · MINERALS & ROCKS · NODE 15 OF 106

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.

CHEMICAL ELEMENTS → BIG 8 (O 46.6% · Si 27.7% · Al 8.1%) → PARENT MAGMA COOLING → SiO₄ TETRAHEDRA → SILICATE & NON-SILICATE MINERALS → CRUSTAL ROCKS

I. Minerals vs. Elements & Fundamental Criteria

MICRO-REALM 01

Elements vs Minerals

→
  • Element: Pure single atom
  • Mineral: Ordered compound
  • Elements combine into minerals
MICRO-REALM 02

5 Criteria of a Mineral

  • Naturally occurring & inorganic
  • Definite chemical formula
  • Ordered atomic structure
MICRO-REALM 03

Single-Element Minerals

AuCuC
  • Gold, Silver & Copper
  • Sulphur, Graphite, Diamond
  • Uncombined native state
MICRO-REALM 04

Compound Minerals

O
Si
O
  • 2 or more elements
  • Quartz ($\text{SiO}_2$) & Calcite
  • Over 4,000 known species
MICRO-REALM 05

Mineraloids (Amorphous)

  • Lack crystalline lattice
  • Opal & Volcanic glass
  • Amber & Pearl (organic)
MICRO-REALM 06

Hot Magma Origin

  • Basic source of all minerals
  • Crystallizes as magma cools
  • Coal & petroleum excepted
MICRO-REALM 07

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)

MICRO-REALM 08

The Crustal Eight (98.6%)

  • 8 elements = 98.59% weight
  • O, Si, Al, Fe, Ca, Na, K, Mg
  • Rest 90+ elements = 1.41%
MICRO-REALM 09

1. Oxygen (46.60%)

O · #146.60%
  • #1 crustal element by weight
  • 93.8% of crustal volume
  • Bonds into oxides/silicates
MICRO-REALM 10

2. Silicon (27.72%)

Si 27.7%
  • #2 element in crust
  • Tetravalent metalloid
  • O + Si = 74.3% of crust
MICRO-REALM 11

3. Aluminium (8.13%)

Al · #38.13%
  • #1 most abundant METAL
  • #3 element overall
  • Forms SIAL & Feldspars
MICRO-REALM 12

4. Iron (5.00%)

5%
32%
  • #4 in Crust (5.00%)
  • #1 in WHOLE Earth (32.1%)
  • Sank to core early
MICRO-REALM 13

5. Calcium & 6. Sodium

Ca 3.63%Na 2.83%
  • #5 Calcium: 3.63% (Calcite)
  • #6 Sodium: 2.83% (Plagioclase)
  • Key alkali/alkaline cations
MICRO-REALM 14

7. Potassium & 8. Magnesium

K 2.59%Mg 2.09%
  • #7 Potassium: 2.59% (Orthoclase)
  • #8 Magnesium: 2.09% (SIMA)
  • Completes top 8 list
MICRO-REALM 15

Minor & Trace (1.41%)

Ti · H · P · Mn
S · C · Ni (1.41%)
  • Titanium (#9 · 0.44%)
  • Hydrogen, Phosphorus, Sulphur
  • Concentrated in ore veins

III. Crystal Lattices, Bonding & Silica Tetrahedra

MICRO-REALM 16

Silica Tetrahedron ($\text{SiO}_4^{4-}$)

  • 1 central $\text{Si}^{4+}$ ion
  • 4 corner $\text{O}^{2-}$ ions
  • Fundamental silicate brick
MICRO-REALM 17

Silicate Polymerization

  • Isolated (Olivine) to Chains
  • Sheets (Mica) to 3D (Quartz)
  • Shared oxygen corners
MICRO-REALM 18

Mineral Chemical Bonds

COVIONMET
  • Covalent: Strongest (Diamond)
  • Ionic: Soluble (Halite)
  • Van der Waals: Weak (Talc)
MICRO-REALM 19

Polymorphism

= C =
  • Same formula, different lattice
  • Diamond vs Graphite (C)
  • Calcite vs Aragonite ($\text{CaCO}_3$)
MICRO-REALM 20

Isomorphism (Solid Solution)

Mg
↔
Fe
  • Similar-sized ions swap
  • $\text{Mg}^{2+} \leftrightarrow \text{Fe}^{2+}$ in Olivine
  • Same crystal geometry
MICRO-REALM 21

Six Crystal Systems

  • Cubic, Tetragonal, Hexagonal
  • Orthorhombic, Monoclinic, Triclinic
  • Internal symmetry axes

IV. Mineral Composition Groups & Bowen's Series

MICRO-REALM 22

Silicate Dominance (92%)

92%
  • 92% of Earth's crust
  • Feldspar (50%) + Quartz (12%)
  • Primary rock-forming group
MICRO-REALM 23

Felsic vs Mafic Silicates

FELSIC
MAFIC
  • Felsic: Light, K/Na/Al, SIAL
  • Mafic: Dark, Mg/Fe, SIMA
  • Low vs High specific gravity
MICRO-REALM 24

Oxide Minerals

Fe₂O₃
  • Metal bonded with Oxygen
  • Hematite & Magnetite (Fe)
  • Bauxite & Corundum (Al)
MICRO-REALM 25

Carbonate Minerals

CaCO₃
  • Built on $\text{CO}_3^{2-}$ ion
  • Calcite & Dolomite
  • Forms Limestone & Marble
MICRO-REALM 26

Sulphides & Sulphates

FeS₂
  • Sulphides: Pyrite, Galena (Pb)
  • Chalcopyrite (Cu), Sphalerite
  • Sulphates: Gypsum & Barite
MICRO-REALM 27

Halides & Phosphates

  • Halides: Halite ($\text{NaCl}$), Fluorite
  • Evaporite salt basins
  • Phosphates: Apatite (teeth/bones)
MICRO-REALM 28

Bowen's Reaction Series

  • Magma crystallization order
  • First (Hot): Olivine, Ca-Plag
  • Last (Cool): Quartz, Muscovite

Core Distinctions

1. Crustal Abundance vs. Whole-Earth Abundance

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. Rock

Elements (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 Earth

Feldspar 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)

1. OXYGEN (O)46.60%
2. SILICON (Si)27.72%
3. ALUMINIUM (Al · #1 Metal)8.13%
4. IRON (Fe)5.00%
5. CALCIUM (3.63%) · 6. SODIUM (2.83%)6.46%
7. POTASSIUM (2.59%) · 8. MAGNESIUM (2.09%)4.68%