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	<title><![CDATA[Mandakini Study Institute - Patna: Concept of Continental Drift, Sea-floor Spreading and Theory of Plate Tectonics]]></title>
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	<pubDate>Tue, 23 Sep 2025 03:09:46 +0000</pubDate>
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	<title><![CDATA[Concept of Continental Drift, Sea-floor Spreading and Theory of Plate Tectonics]]></title>
	<description><![CDATA[<p>Concept of Continental Drift, Sea-floor Spreading and Theory of Plate Tectonics</p><p>1. Continental Drift (Proposed by Alfred Wegener, 1912)</p><p>* The **Continental Drift Hypothesis** states that continents were once joined together in a single supercontinent called **Pangaea** (\~300 million years ago), surrounded by a vast ocean called **Panthalassa**.<br />
* Pangaea later broke into two landmasses &ndash; **Laurasia (north)** and **Gondwana (south)** &ndash; which further drifted to form the present continents.<br />
* **Evidence supporting Continental Drift:**</p><p>&nbsp; * **Fossil evidence** (e.g., Mesosaurus in Africa and South America).<br />
&nbsp; * **Geological similarities** (rock formations across continents match).<br />
&nbsp; * **Paleoclimatic evidence** (glacial deposits in present-day tropical regions).<br />
&nbsp; * **Fit of the continents** (South America fits into Africa like a puzzle).<br />
* **Limitation:** Wegener could not explain the driving mechanism of movement.</p><p>---</p><p>### **2. Sea-floor Spreading (Proposed by Harry H. Hess, 1960s)**</p><p>* Suggests that new oceanic crust is continuously formed at **mid-oceanic ridges** due to upwelling of magma from the mantle.<br />
* The new crust spreads outward, pushing older crust away, and is eventually destroyed at **subduction zones (trenches)**.<br />
* **Key Evidence:**</p><p>&nbsp; * Symmetrical pattern of **magnetic stripes** (paleomagnetism) on either side of mid-ocean ridges.<br />
&nbsp; * **Age of ocean floor** increases away from ridges.<br />
&nbsp; * Distribution of earthquakes and volcanic activity along ridges and trenches.</p><p>---</p><p>### **3. Theory of Plate Tectonics (Unified theory, 1968)**</p><p>* Combines **Continental Drift** and **Sea-floor Spreading** into a comprehensive model.<br />
* States that the Earth&rsquo;s lithosphere is divided into **rigid plates** (7 major + several minor) that float over the **asthenosphere**.<br />
* Plate boundaries are sites of most tectonic activity:</p><p>&nbsp; * **Divergent boundaries** &rarr; mid-ocean ridges, rift valleys (e.g., Mid-Atlantic Ridge).<br />
&nbsp; * **Convergent boundaries** &rarr; subduction zones, mountain building (e.g., Himalayas, Andes).<br />
&nbsp; * **Transform boundaries** &rarr; lateral sliding, earthquakes (e.g., San Andreas Fault).</p><p>---</p><p>### **Geological Significance**</p><p>* Explains distribution of **earthquakes, volcanoes, and mountain belts**.<br />
* Provides a unifying theory for **crustal movements, orogeny, and continental evolution**.<br />
* Crucial for understanding **paleogeography, ocean basins, and natural resources**.</p><p>---</p><p>✅ **In short**:</p><p>* *Continental Drift* showed that continents move.<br />
* *Sea-floor Spreading* explained how new oceanic crust forms and spreads.<br />
* *Plate Tectonics* unified both, showing that lithospheric plates move and interact, shaping Earth&rsquo;s surface.<br />
&nbsp;</p>]]></description>
	<dc:creator>MSIPATNA</dc:creator>
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