π Origin β Pangaea Theory
- Pangaea β divided into Angaraland (North) and Gondwanaland (South)
- Indian subcontinent was part of Gondwanaland
π 4 Groups of Indian Rocks
β³ Geological Timeline
Oldest
Archaean / Pre-Cambrian Era
Gneiss & Schist β No fossils β 86.7% of Earth formation
Purana Group
Cuddapah + Vindhyan Systems
Layered sedimentary rocks β Origin of life β Eastern Ghats, Vindhya Plateau
Paleozoic Era
Dravidian Group
First evidence of life β Rich fossils β Absent almost everywhere except Rewa (MP)
Mesozoic β Recent
Aryan Group
Gondwana (coal), Deccan Trap (basalt/black soil), Tertiary (Himalayas), Quaternary
(alluvial)
β‘ QUICK RECALL β Fossil Memory
- Archaean β No fossils (Earth cooling)
- Dharwar β No fossils
- Cuddapah β No fossils (origin of life only)
- Vindhyan β General absence of fossils
- Dravidian β RICH fossils (first life evidence) β
- Gondwana β Fossils present β
βοΈ Group 1 β Archaean
- Contribute ~86.7% in formation of the Earth
- Formed during cooling of the Earth
-
No Fossils β Pre-biological era
- Rock types: Gneiss and Schist
Bundelkhand Gneiss (most ancient)
Bengal Gneiss
Found In:
Karnataka
Tamil Nadu
Andhra Pradesh
Madhya Pradesh
Odisha
Chotanagpur Plateau (Jharkhand)
- Formed by erosion & deposition of Archaean rocks
- Most developed in Dharwar region, Karnataka
- No Fossils
-
Aravalli mountain range β formed from these rocks
β‘ QUICK RECALL
Dharwar rocks β
Aravalli mountainsformed | Most developed in
Karnataka (Dharwar district)
π¨ EXAM TRAP
- Bundelkhand Gneiss = most ancient rocks of India
- Archaean rocks represent the earliest and most extensive phase of Earth's crustal formation described here, accounting for 86.7%.
- The Aravalli system is associated with Dharwar rocks rather than the older Archaean system in this classification.
π¦ Group 3 β Dravidian
- Rocks of Paleozoic Era
- First evidence of life on Earth
- This rock system is especially rich in fossils.
- Absent from almost whole India
- Found only in: Rewa district, Madhya Pradesh
π¨ EXAM TRAP β Most Asked!
Dravidian Group =
almost absent from Indiaβ only
Rewa (MP)are found in. but most important =
First/Rich Fossils. this contradiction remember!
β‘ QUICK RECALL
Dravidian =
Paleozoic Era | Rich Fossils =
First life evidence | Location =
Only Rewa,
MP
π₯ Group 4 β Aryan (4 Sub-Systems)
- Construction of basin landforms
- Fossils present
-
~98% of India's coal reserves found here!
Spread In:
Damodar Valley
Mahanadi Valley
Rajmahal
Satpura
98%
India's Coal Reserves in Gondwana Rocks
- End of Cretaceous Era β Volcanic activity in western Peninsular India
-
Basalt lava flow β step-like landform (trap = step)
- Mainly in Maharashtra and Malwa region
- Also formed: Rajmahal Trap
- Basalt erosion β Fertile Black Soil (Regur)
Deccan Trap States:
Maharashtra
MP
Gujarat
Karnataka
Andhra Pradesh
β‘ QUICK RECALL
Deccan Trap β Basalt Lava β
Black Soil (Regur/Cotton Soil) β Best for cotton cultivation
- Formed: Eocene to Pliocene epoch
- Formation of Peninsular Plateau
- Formation of Himalayan mountains
- Rocks of Pleistocene + Holocene epoch
- Deposits at mouths of Indo-Gangetic Plains
- Also in Deltaic regions
- Most recent rocks
π¨ EXAM TRAP
- About 98% of India's coal resources occur in Gondwana rock formations.
- Black soil developed from Deccan Trap basalt, not from Gondwana rocks.
- "Trap" word comes from Swedish "trappa" = stairs/steps β step-like lava landform
- The Damodar Valley is a major Gondwana coal belt extending through the JharkhandβWest Bengal region and is important for eastern India studies.
π Complete Master Summary Table
| Group |
System |
Era |
Fossils |
Key Feature |
Location/Landform |
| 1. Archaean |
Archaean System |
Pre-Cambrian |
Absent |
86.7% Earth formation, Gneiss & Schist |
Karnataka, TN, AP, MP, Odisha, Jharkhand |
| Dharwar System |
Pre-Cambrian |
Absent |
Formed from Archaean erosion |
Aravalli mountains, Dharwar (Karnataka) |
| 2. Purana |
Cuddapah System |
Pre-Cambrian |
Absent |
Origin of life, layered rocks |
Eastern Ghats, Cuddapah (AP) |
| Vindhyan System |
Pre-Cambrian |
Gen. Absent |
Limestone, Sandstone, Clays |
Vindhya Plateau (GangaβDeccan divide) |
| 3. Dravidian |
Paleozoic Rocks |
Paleozoic |
Rich Fossils |
First life evidence, Absent almost everywhere |
Only Rewa district (MP) |
| 4. Aryan |
Gondwana System |
Mesozoic |
Present |
98% India's coal reserves |
Damodar Valley, Mahanadi, Rajmahal, Satpura |
| Deccan Trap |
Cretaceous end |
β |
Basalt lava β Black Soil (Regur) |
Maharashtra, MP, Gujarat, Karnataka, AP |
| Tertiary System |
EoceneβPliocene |
β |
Himalayas + Peninsular Plateau formed |
Himalayan region |
| Quaternary System |
PleistoceneβHolocene |
β |
Most recent rocks |
Indo-Gangetic Plains, Delta regions |
π― Most Important Points for BPSC/BSSC
- Coal (98%) β Gondwana rocks
- Black Soil β Deccan Trap (Basalt)
- Richest fossils β Dravidian Group
- Dravidian rocks in India β only Rewa (MP)
- Aravalli β Dharwar rocks
- Eastern Ghats β Cuddapah rocks
- Most ancient β Bundelkhand Gneiss
- IST + Tropic of Cancer meet β Chhattisgarh
-
A P D A = Archaean, Purana, Dravidian, Aryan (4 groups order)
- No fossils β Arch, Dhar, Cudd, Vindh (4 oldest)
- Gondwana = Coal = Damodar Valley (JH/Bihar)
- In Deccan Trap, the term trap refers to the step-like landform produced by successive basaltic lava flows.
- Quaternary = most RECENT β alluvial soil of Ganga
β‘ BIHAR SPECIAL RECALL
- The Gondwana coalfields of the Damodar Valley lie along the JharkhandβWest Bengal belt, close to Bihar.
- Chotanagpur Plateau (Jharkhand) = Archaean rocks β mineral rich area
- The Indo-Gangetic Plain, including the Bihar Plain, consists largely of fertile Quaternary alluvial deposits.