Continental drift evidence is a match across a split: rocks, minerals, fossils and sediment systems that line up on facing coasts all count.
(c) I, II and III
All three statements are correct and serve as evidences of continental drift theory, originally proposed by Alfred Wegener in 1912.
| Type of Evidence | Description | Examples |
|---|---|---|
| Geological | Similar rocks and mountain belts on separated continents | Brazil–West Africa, Appalachians–Caledonides |
| Fossil | Identical fossils of extinct species on widely separated continents | Glossopteris (fern), Mesosaurus (reptile) |
| Paleoclimatic | Glacial deposits and coal beds indicating different climatic conditions in now-distant regions | Gondwana glaciation marks in India, Africa |
| Mineralogical | Similar mineral deposits found across continents that are now far apart | Gold in Ghana and Brazil |
| Type of Evidence | Description | Example |
|---|---|---|
| Geological | Similar rock formations and mountain ranges found on separate continents | Precambrian rocks on Brazilian and West African coasts |
| Fossil | Same extinct plant and animal fossils found across now-distant continents | Glossopteris (plant) in India, Africa, and South America |
| Mineralogical | Similar mineral deposits shared between continents | Gold in Ghana and Brazil |
| Paleoclimatic | Glacial striations and coal deposits suggesting different climates in ancient past | Glacial deposits in India, coal in Antarctica |
| Sedimentary | Gondwana rock system found in multiple continents of the Southern Hemisphere | Gondwana rocks in India, Australia, Africa, South America, Antarctica |
| Modern Region | Presence of Gondwana System | Notable Fossils/Rocks |
|---|---|---|
| India | Yes | Talchir Boulder Beds, Glossopteris |
| Africa (South) | Yes | Coal deposits, glacial marks |
| South America | Yes | Similar flora, fossil species |
| Antarctica | Yes | Fossils of flora indicating warm past |
| Australia | Yes | Similar sedimentary structures |
| Madagascar | Yes | Continuity of Gondwanan strata |
| Fossil | Type | Found in | Significance |
|---|---|---|---|
| Glossopteris | Fern-like plant | India, Africa, South America, Australia, Antarctica | Shows land continuity across southern continents |
| Mesosaurus | Freshwater reptile | South America and Africa | Couldn’t swim across oceans; continents must’ve been joined |
| Lystrosaurus | Reptile | India, Antarctica, South Africa | Confirms common landmass before continental drift |
| Aspect | Continental Drift | Plate Tectonics |
|---|---|---|
| Proposed By | Alfred Wegener (1912) | Developed in 1960s based on oceanic studies |
| Mechanism Explained? | No (did not explain how drift happened) | Yes (explains movement via lithospheric plates) |
| Key Idea | Continents were once joined and drifted apart | Earth’s crust is made of plates that move over mantle |