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	<title><![CDATA[Mandakini Study Institute - Patna: Mountains – Types, Characteristics, and Origin]]></title>
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	<guid isPermaLink="true">https://kuntal.org/msipstudentslogin/pages/view/881/mountains-%25E2%2580%2593-types-characteristics-and-origin</guid>
	<pubDate>Tue, 06 May 2025 08:58:21 +0000</pubDate>
	<link>https://kuntal.org/msipstudentslogin/pages/view/881/mountains-%25E2%2580%2593-types-characteristics-and-origin</link>
	<title><![CDATA[Mountains – Types, Characteristics, and Origin]]></title>
	<description><![CDATA[<h3 data-end="58" data-start="0"><strong data-end="58" data-start="8">Mountains &ndash; Types, Characteristics, and Origin</strong></h3><hr data-end="63" data-start="60"><h3 data-end="87" data-start="65">🔹 <strong data-end="87" data-start="72">Definition:</strong></h3><p data-end="379" data-start="88">Mountains are <strong data-end="147" data-start="102">natural elevations of the Earth&#39;s surface</strong> that rise prominently above the surrounding terrain. They are formed due to <strong data-end="243" data-start="224">tectonic forces</strong>, <strong data-end="266" data-start="245">volcanic activity</strong>, or <strong data-end="294" data-start="271">erosional processes</strong>, and usually have <strong data-end="329" data-start="313">steep slopes</strong>, <strong data-end="350" data-start="331">high elevations</strong>, and <strong data-end="378" data-start="356">significant relief</strong>.</p><hr data-end="384" data-start="381"><h3 data-end="434" data-start="386">🔹 <strong data-end="434" data-start="393">Types of Mountains (Based on Origin):</strong></h3><table data-end="1251" data-start="436">
	<thead data-end="552" data-start="436">
		<tr data-end="552" data-start="436">
			<th data-col-size="sm" data-end="463" data-start="436">Type of Mountain</th>
			<th data-col-size="md" data-end="516" data-start="463">Origin Mechanism</th>
			<th data-col-size="sm" data-end="552" data-start="516">Example</th>
		</tr>
	</thead>
	<tbody data-end="1251" data-start="670">
		<tr data-end="786" data-start="670">
			<td data-col-size="sm" data-end="698" data-start="670"><strong data-end="693" data-start="672">1. Fold Mountains</strong></td>
			<td data-col-size="md" data-end="751" data-start="698">Formed by <strong data-end="725" data-start="710">compression</strong> of crust causing folding</td>
			<td data-col-size="sm" data-end="786" data-start="751">Himalayas, Alps, Andes</td>
		</tr>
		<tr data-end="903" data-start="787">
			<td data-col-size="sm" data-end="815" data-start="787"><strong data-end="811" data-start="789">2. Block Mountains</strong></td>
			<td data-col-size="md" data-end="868" data-start="815">Formed by <strong data-end="839" data-start="827">faulting</strong> (uplifted blocks or horsts)</td>
			<td data-col-size="sm" data-end="903" data-start="868">Sierra Nevada (USA), Vosges</td>
		</tr>
		<tr data-end="1019" data-start="904">
			<td data-col-size="sm" data-end="932" data-start="904"><strong data-end="931" data-start="906">3. Volcanic Mountains</strong></td>
			<td data-col-size="md" data-end="984" data-start="932">Formed by <strong data-end="966" data-start="944">volcanic eruptions</strong> and lava buildup</td>
			<td data-col-size="sm" data-end="1019" data-start="984">Mount Fuji, Mount Kilimanjaro</td>
		</tr>
		<tr data-end="1135" data-start="1020">
			<td data-col-size="sm" data-end="1048" data-start="1020"><strong data-end="1047" data-start="1022">4. Residual Mountains</strong></td>
			<td data-col-size="md" data-end="1100" data-start="1048">Formed by <strong data-end="1071" data-start="1060">erosion</strong> of surrounding land</td>
			<td data-col-size="sm" data-end="1135" data-start="1100">Aravalli (India), Ural (Russia)</td>
		</tr>
		<tr data-end="1251" data-start="1136">
			<td data-col-size="sm" data-end="1164" data-start="1136"><strong data-end="1159" data-start="1138">5. Dome Mountains</strong></td>
			<td data-col-size="md" data-end="1216" data-start="1164">Formed by <strong data-end="1205" data-start="1176">upward intrusion of magma</strong></td>
			<td data-col-size="sm" data-end="1251" data-start="1216">Black Hills (USA), Henry Mts.</td>
		</tr>
	</tbody>
</table><p><button></button></p><hr data-end="1256" data-start="1253"><h3 data-end="1288" data-start="1258">🔹 <strong data-end="1286" data-start="1265">1. Fold Mountains</strong></h3><ul data-end="1474" data-start="1289">
	<li data-end="1311" data-start="1289">
	<p data-end="1311" data-start="1291"><strong data-end="1311" data-start="1291">Most common type</strong></p>
	</li>
	<li data-end="1375" data-start="1312">
	<p data-end="1375" data-start="1314">Formed at <strong data-end="1355" data-start="1324">convergent plate boundaries</strong> due to compression.</p>
	</li>
	<li data-end="1435" data-start="1376">
	<p data-end="1435" data-start="1378">Rocks are <strong data-end="1407" data-start="1388">bent into folds</strong> (anticlines and synclines).</p>
	</li>
	<li data-end="1474" data-start="1436">
	<p data-end="1474" data-start="1438">Usually <strong data-end="1473" data-start="1446">young, tall, and rugged</strong>.</p>
	</li>
</ul><p data-end="1523" data-start="1476">✅ <strong data-end="1490" data-start="1478">Examples</strong>: Himalayas, Rockies, Andes, Alps</p><hr data-end="1528" data-start="1525"><h3 data-end="1561" data-start="1530">🔹 <strong data-end="1559" data-start="1537">2. Block Mountains</strong></h3><ul data-end="1734" data-start="1562">
	<li data-end="1651" data-start="1562">
	<p data-end="1651" data-start="1564">Formed when large blocks of crust are <strong data-end="1628" data-start="1602">uplifted or downthrown</strong> along <strong data-end="1650" data-start="1635">fault lines</strong>.</p>
	</li>
	<li data-end="1734" data-start="1652">
	<p data-end="1734" data-start="1654"><strong data-end="1663" data-start="1654">Horst</strong> = uplifted block; <strong data-end="1692" data-start="1682">Graben</strong> = sunken block (can become rift valleys).</p>
	</li>
</ul><p data-end="1781" data-start="1736">✅ <strong data-end="1750" data-start="1738">Examples</strong>: Sierra Nevada, Harz (Germany)</p><hr data-end="1786" data-start="1783"><h3 data-end="1822" data-start="1788">🔹 <strong data-end="1820" data-start="1795">3. Volcanic Mountains</strong></h3><ul data-end="1988" data-start="1823">
	<li data-end="1916" data-start="1823">
	<p data-end="1916" data-start="1825">Formed by the <strong data-end="1892" data-start="1839">accumulation of lava, ash, and volcanic materials</strong> around a volcanic vent.</p>
	</li>
	<li data-end="1946" data-start="1917">
	<p data-end="1946" data-start="1919">Often <strong data-end="1936" data-start="1925">conical</strong> in shape.</p>
	</li>
	<li data-end="1988" data-start="1947">
	<p data-end="1988" data-start="1949">May be <strong data-end="1987" data-start="1956">active, dormant, or extinct</strong>.</p>
	</li>
</ul><p data-end="2045" data-start="1990">✅ <strong data-end="2004" data-start="1992">Examples</strong>: Mount St. Helens, Mauna Loa, Mount Etna</p><hr data-end="2050" data-start="2047"><h3 data-end="2098" data-start="2052">🔹 <strong data-end="2096" data-start="2059">4. Residual (Erosional) Mountains</strong></h3><ul data-end="2245" data-start="2099">
	<li data-end="2186" data-start="2099">
	<p data-end="2186" data-start="2101"><strong data-end="2118" data-start="2101">Old mountains</strong> formed from <strong data-end="2157" data-start="2131">weathering and erosion</strong> of previously larger ranges.</p>
	</li>
	<li data-end="2245" data-start="2187">
	<p data-end="2245" data-start="2189">Harder rock <strong data-end="2220" data-start="2201">resists erosion</strong>, leaving isolated peaks.</p>
	</li>
</ul><p data-end="2293" data-start="2247">✅ <strong data-end="2261" data-start="2249">Examples</strong>: Aravalli Hills, Ural Mountains</p><hr data-end="2298" data-start="2295"><h3 data-end="2330" data-start="2300">🔹 <strong data-end="2328" data-start="2307">5. Dome Mountains</strong></h3><ul data-end="2468" data-start="2331">
	<li data-end="2393" data-start="2331">
	<p data-end="2393" data-start="2333">Formed when magma pushes the crust upwards without erupting.</p>
	</li>
	<li data-end="2424" data-start="2394">
	<p data-end="2424" data-start="2396">Erosion may expose the core.</p>
	</li>
	<li data-end="2468" data-start="2425">
	<p data-end="2468" data-start="2427">Have a <strong data-end="2467" data-start="2434">rounded, dome-like appearance</strong>.</p>
	</li>
</ul><p data-end="2512" data-start="2470">✅ <strong data-end="2484" data-start="2472">Examples</strong>: Black Hills (South Dakota)</p><hr data-end="2517" data-start="2514"><h3 data-end="2566" data-start="2519">🔹 <strong data-end="2566" data-start="2526">Common Characteristics of Mountains:</strong></h3><ul data-end="2757" data-start="2568">
	<li data-end="2615" data-start="2568">
	<p data-end="2615" data-start="2570"><strong data-end="2588" data-start="2570">High elevation</strong> (usually above 600 meters)</p>
	</li>
	<li data-end="2653" data-start="2616">
	<p data-end="2653" data-start="2618"><strong data-end="2653" data-start="2618">Steep slopes and rugged terrain</strong></p>
	</li>
	<li data-end="2682" data-start="2654">
	<p data-end="2682" data-start="2656"><strong data-end="2682" data-start="2656">Often source of rivers</strong></p>
	</li>
	<li data-end="2727" data-start="2683">
	<p data-end="2727" data-start="2685">Influence <strong data-end="2706" data-start="2695">climate</strong> and <strong data-end="2727" data-start="2711">biodiversity</strong></p>
	</li>
	<li data-end="2757" data-start="2728">
	<p data-end="2757" data-start="2730">Act as <strong data-end="2757" data-start="2737">natural barriers</strong></p>
	</li>
</ul><hr data-end="2762" data-start="2759"><h3 data-end="2801" data-start="2764">🔍 <strong data-end="2801" data-start="2771">Significance of Mountains:</strong></h3><ul data-end="3023" data-start="2803">
	<li data-end="2857" data-start="2803">
	<p data-end="2857" data-start="2805"><strong data-end="2819" data-start="2805">Ecological</strong>: Habitats for diverse flora and fauna</p>
	</li>
	<li data-end="2922" data-start="2858">
	<p data-end="2922" data-start="2860"><strong data-end="2876" data-start="2860">Hydrological</strong>: Water towers of the world (glaciers, rivers)</p>
	</li>
	<li data-end="2965" data-start="2923">
	<p data-end="2965" data-start="2925"><strong data-end="2937" data-start="2925">Economic</strong>: Minerals, tourism, forests</p>
	</li>
	<li data-end="3023" data-start="2966">
	<p data-end="3023" data-start="2968"><strong data-end="2980" data-start="2968">Cultural</strong>: Sacred landscapes, indigenous settlements</p>
	</li>
</ul>]]></description>
	<dc:creator>MSIPATNA</dc:creator>
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