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	<title>Geologia - Problemas e Materiais do Quotidiano</title>
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		<title>Geologia - Problemas e Materiais do Quotidiano</title>
		<link>http://ocupantropica.wordpress.com</link>
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		<item>
		<title>Página de Biologia</title>
		<link>http://ocupantropica.wordpress.com/2009/06/30/pagina-de-biologia/</link>
		<comments>http://ocupantropica.wordpress.com/2009/06/30/pagina-de-biologia/#comments</comments>
		<pubDate>Tue, 30 Jun 2009 11:13:00 +0000</pubDate>
		<dc:creator>ocupantropica2</dc:creator>
				<category><![CDATA[Não classificado]]></category>

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		<description><![CDATA[Para quem quiser estudar&#8230; disponibilizo um endereço onde pode encontrar materiais relativos a temáticas da área da Biologia: http://sites.google.com/site/adescobertadacelula/<img alt="" border="0" src="http://stats.wordpress.com/b.gif?host=ocupantropica.wordpress.com&amp;blog=2839396&amp;post=73&amp;subd=ocupantropica&amp;ref=&amp;feed=1" width="1" height="1" />]]></description>
			<content:encoded><![CDATA[<p>Para quem quiser estudar&#8230; disponibilizo um endereço onde pode encontrar materiais relativos a temáticas da área da Biologia:</p>
<p style="text-align:center;"><a href="http://sites.google.com/site/adescobertadacelula/">http://sites.google.com/site/adescobertadacelula/</a></p>
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			<media:title type="html">ocupantropica2</media:title>
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		<item>
		<title>Dia da Terra&#8230;</title>
		<link>http://ocupantropica.wordpress.com/2009/04/23/dia-da-terra/</link>
		<comments>http://ocupantropica.wordpress.com/2009/04/23/dia-da-terra/#comments</comments>
		<pubDate>Thu, 23 Apr 2009 00:31:27 +0000</pubDate>
		<dc:creator>ocupantropica2</dc:creator>
				<category><![CDATA[Não classificado]]></category>

		<guid isPermaLink="false">http://ocupantropica.wordpress.com/2009/04/23/dia-da-terra/</guid>
		<description><![CDATA[dia-da-terra_-sete-pecados-da-insustentabilidade-do-desenvolvimento-em-portu3<img alt="" border="0" src="http://stats.wordpress.com/b.gif?host=ocupantropica.wordpress.com&amp;blog=2839396&amp;post=64&amp;subd=ocupantropica&amp;ref=&amp;feed=1" width="1" height="1" />]]></description>
			<content:encoded><![CDATA[<p style="text-align:center;"><a href="http://ocupantropica.files.wordpress.com/2009/04/dia-da-terra_-sete-pecados-da-insustentabilidade-do-desenvolvimento-em-portu3.pdf">dia-da-terra_-sete-pecados-da-insustentabilidade-do-desenvolvimento-em-portu3</a></p>
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			<media:title type="html">ocupantropica2</media:title>
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		<item>
		<title>Mudanças?</title>
		<link>http://ocupantropica.wordpress.com/2008/06/15/mudancas/</link>
		<comments>http://ocupantropica.wordpress.com/2008/06/15/mudancas/#comments</comments>
		<pubDate>Sun, 15 Jun 2008 20:32:13 +0000</pubDate>
		<dc:creator>ocupantropica</dc:creator>
				<category><![CDATA[Não classificado]]></category>

		<guid isPermaLink="false">http://ocupantropica.wordpress.com/?p=61</guid>
		<description><![CDATA[Alguns anos depois e continuamos na mesma, ou pior ainda!<img alt="" border="0" src="http://stats.wordpress.com/b.gif?host=ocupantropica.wordpress.com&amp;blog=2839396&amp;post=61&amp;subd=ocupantropica&amp;ref=&amp;feed=1" width="1" height="1" />]]></description>
			<content:encoded><![CDATA[<p>Alguns anos depois e continuamos na mesma, ou pior ainda!<br />
<span style="text-align:center; display: block;"><a href="http://ocupantropica.wordpress.com/2008/06/15/mudancas/"><img src="http://img.youtube.com/vi/7KY9LaxVkDM/2.jpg" alt="" /></a></span></p>
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			<media:title type="html">ocupantropica</media:title>
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		<item>
		<title>Continue a pesquisar&#8230;</title>
		<link>http://ocupantropica.wordpress.com/2008/06/07/continue-a-pesquisar/</link>
		<comments>http://ocupantropica.wordpress.com/2008/06/07/continue-a-pesquisar/#comments</comments>
		<pubDate>Sat, 07 Jun 2008 22:56:46 +0000</pubDate>
		<dc:creator>ocupantropica</dc:creator>
				<category><![CDATA[Não classificado]]></category>

		<guid isPermaLink="false">http://ocupantropica.wordpress.com/?p=58</guid>
		<description><![CDATA[Continue a viajar pelos diferentes &#8220;separadores&#8221;, vai ver que não se arrepende. Para nos mantermos fiéis ao projecto inicial não alterámos as designações, mas clicando em cada um dos blogues vai surprender-se com o trabalho desenvolvido pelos alunos. Desejo a todos os que por aqui passam um &#8220;óptimo estudo&#8221;&#8230; &#8220;BOM TRABALHO&#8221; para todos aqueles que [...]<img alt="" border="0" src="http://stats.wordpress.com/b.gif?host=ocupantropica.wordpress.com&amp;blog=2839396&amp;post=58&amp;subd=ocupantropica&amp;ref=&amp;feed=1" width="1" height="1" />]]></description>
			<content:encoded><![CDATA[<p style="text-align:justify;">Continue a viajar pelos diferentes &#8220;separadores&#8221;, vai ver que não se arrepende.</p>
<p style="text-align:justify;">Para nos mantermos fiéis ao projecto inicial não alterámos as designações, mas clicando em cada um dos blogues vai surprender-se com o trabalho desenvolvido pelos alunos.</p>
<p style="text-align:justify;">Desejo a todos os que por aqui passam um &#8220;óptimo estudo&#8221;&#8230;</p>
<p style="text-align:justify;">&#8220;BOM TRABALHO&#8221; para todos aqueles que vão realizar o exame final de Biologia e Geologia.</p>
<p style="text-align:justify;">Quem tem trabalhado de forma tão eficiente estará, certamente, preparado para ultrapassar mais esta etapa do seu processo de desenvolvimento.</p>
<p style="text-align:justify;">Um até breve.</p>
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			<media:title type="html">ocupantropica</media:title>
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		<title>Feira de Minerais</title>
		<link>http://ocupantropica.wordpress.com/2008/05/23/feira-de-minerais/</link>
		<comments>http://ocupantropica.wordpress.com/2008/05/23/feira-de-minerais/#comments</comments>
		<pubDate>Fri, 23 May 2008 22:36:58 +0000</pubDate>
		<dc:creator>ocupantropica</dc:creator>
				<category><![CDATA[Não classificado]]></category>
		<category><![CDATA[feira de minerais]]></category>

		<guid isPermaLink="false">http://ocupantropica.wordpress.com/?p=55</guid>
		<description><![CDATA[Se nos dias 30 e 31 de Maio e 1 de Junho estiver no Norte dê um &#8220;salto&#8221; à Universidade do Porto e visite a Feira de Minerais, Pedras Preciosas e Fósseis.  feiraminerais_2008_flyers feiraminerais_2008<img alt="" border="0" src="http://stats.wordpress.com/b.gif?host=ocupantropica.wordpress.com&amp;blog=2839396&amp;post=55&amp;subd=ocupantropica&amp;ref=&amp;feed=1" width="1" height="1" />]]></description>
			<content:encoded><![CDATA[<p style="text-align:justify;">Se nos dias 30 e 31 de Maio e 1 de Junho estiver no Norte dê um &#8220;salto&#8221; à Universidade do Porto e visite a Feira de Minerais, Pedras Preciosas e Fósseis.</p>
<p style="text-align:center;"> <a href="http://ocupantropica.files.wordpress.com/2008/05/feiraminerais_2008_flyers.pdf">feiraminerais_2008_flyers</a></p>
<p style="text-align:center;"><a href="http://ocupantropica.files.wordpress.com/2008/05/feiraminerais_2008.pdf">feiraminerais_2008</a></p>
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			<media:title type="html">ocupantropica</media:title>
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		<title>Deformações das rochas</title>
		<link>http://ocupantropica.wordpress.com/2008/05/11/deformacoes-das-rochas/</link>
		<comments>http://ocupantropica.wordpress.com/2008/05/11/deformacoes-das-rochas/#comments</comments>
		<pubDate>Sun, 11 May 2008 21:00:55 +0000</pubDate>
		<dc:creator>ocupantropica</dc:creator>
				<category><![CDATA[Não classificado]]></category>

		<guid isPermaLink="false">http://ocupantropica.wordpress.com/?p=54</guid>
		<description><![CDATA[Os vulcões e os sismos não representam as únicas manifestações da actividade interna do nosso planeta. No interior da Terra ocorrem, também, processos contínuos muito lentos e menos espectaculares, que provocam deformações nas rochas. Essas deformações podem corresponder a alterações de volume e/ou a alterações de forma.<img alt="" border="0" src="http://stats.wordpress.com/b.gif?host=ocupantropica.wordpress.com&amp;blog=2839396&amp;post=54&amp;subd=ocupantropica&amp;ref=&amp;feed=1" width="1" height="1" />]]></description>
			<content:encoded><![CDATA[<p style="text-align:justify;">Os vulcões e os sismos não representam as únicas manifestações da actividade interna do nosso planeta. No interior da Terra ocorrem, também, processos contínuos muito lentos e menos espectaculares, que provocam deformações nas rochas. Essas deformações podem corresponder a alterações de volume e/ou a alterações de forma.</p>
<p style="text-align:center;"><iframe src='http://www.slideshare.net/slideshow/embed_code/399026' width='425' height='348'></iframe></p>
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			<media:title type="html">ocupantropica</media:title>
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		<title>Metamorfismo</title>
		<link>http://ocupantropica.wordpress.com/2008/05/11/metamorfismo/</link>
		<comments>http://ocupantropica.wordpress.com/2008/05/11/metamorfismo/#comments</comments>
		<pubDate>Sun, 11 May 2008 20:37:50 +0000</pubDate>
		<dc:creator>ocupantropica</dc:creator>
				<category><![CDATA[Não classificado]]></category>

		<guid isPermaLink="false">http://ocupantropica.wordpress.com/?p=53</guid>
		<description><![CDATA[A grande diversidade de rochas metamórficas que afloram à superfície são o resultado de processos muito lentos que ocorrem no interior da crusta.<img alt="" border="0" src="http://stats.wordpress.com/b.gif?host=ocupantropica.wordpress.com&amp;blog=2839396&amp;post=53&amp;subd=ocupantropica&amp;ref=&amp;feed=1" width="1" height="1" />]]></description>
			<content:encoded><![CDATA[<p style="text-align:justify;">A grande diversidade de rochas metamórficas que afloram à superfície são o resultado de processos muito lentos que ocorrem no interior da crusta.</p>
<p style="text-align:center;"><iframe src='http://www.slideshare.net/slideshow/embed_code/398988' width='425' height='348'></iframe></p>
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		<title>Rochas metamórficas</title>
		<link>http://ocupantropica.wordpress.com/2008/05/11/rochas-metamorficas/</link>
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		<pubDate>Sun, 11 May 2008 18:33:38 +0000</pubDate>
		<dc:creator>ocupantropica</dc:creator>
				<category><![CDATA[Não classificado]]></category>
		<category><![CDATA[metamorfismo]]></category>
		<category><![CDATA[minerais índice]]></category>
		<category><![CDATA[recristalização]]></category>
		<category><![CDATA[rochas metamórficas]]></category>

		<guid isPermaLink="false">http://ocupantropica.wordpress.com/?p=52</guid>
		<description><![CDATA[&#8220;Inicialmente a Terra esteve completamente coberta por um oceano que cobria até as montanhas mais altas. Águas profundas e turvas continham em suspensão e em solução todos os materiais que formam agora a crosta terrestre. À medida que passava o tempo, foi-se dispondo uma sucessão de depósitos que eram unicamente precipitados químicos e incluíam, além [...]<img alt="" border="0" src="http://stats.wordpress.com/b.gif?host=ocupantropica.wordpress.com&amp;blog=2839396&amp;post=52&amp;subd=ocupantropica&amp;ref=&amp;feed=1" width="1" height="1" />]]></description>
			<content:encoded><![CDATA[<p style="text-align:justify;"><em>&#8220;Inicialmente a Terra esteve completamente coberta por um oceano que cobria até as montanhas mais altas. Águas profundas e turvas continham em suspensão e em solução todos os materiais que formam agora a crosta terrestre. À medida que passava o tempo, foi-se dispondo uma sucessão de depósitos que eram unicamente precipitados químicos e incluíam, além do granito e de outras rochas ígneas, gnaisses e xistos&#8221;.</em></p>
<p style="text-align:right;"><em>Abraham Werner (1749-1817)</em></p>
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		<title>Características das rochas magmáticas</title>
		<link>http://ocupantropica.wordpress.com/2008/05/11/caracteristicas-das-rochas-magmaticas/</link>
		<comments>http://ocupantropica.wordpress.com/2008/05/11/caracteristicas-das-rochas-magmaticas/#comments</comments>
		<pubDate>Sun, 11 May 2008 17:38:53 +0000</pubDate>
		<dc:creator>ocupantropica</dc:creator>
				<category><![CDATA[Não classificado]]></category>
		<category><![CDATA[características das rochas]]></category>

		<guid isPermaLink="false">http://ocupantropica.wordpress.com/?p=51</guid>
		<description><![CDATA[Devido à grande diversidade de rochas magmáticas, a sua classificação pode ser feita tendo em conta algumas características como: a cor, a textura, a composição química e mineralógica.<img alt="" border="0" src="http://stats.wordpress.com/b.gif?host=ocupantropica.wordpress.com&amp;blog=2839396&amp;post=51&amp;subd=ocupantropica&amp;ref=&amp;feed=1" width="1" height="1" />]]></description>
			<content:encoded><![CDATA[<p style="text-align:justify;">Devido à grande diversidade de rochas magmáticas, a sua classificação pode ser feita tendo em conta algumas características como: a cor, a textura, a composição química e mineralógica.</p>
<p style="text-align:center;"><iframe src='http://www.slideshare.net/slideshow/embed_code/398843' width='425' height='348'></iframe></p>
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			<media:title type="html">ocupantropica</media:title>
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		<title>Rochas magmáticas</title>
		<link>http://ocupantropica.wordpress.com/2008/05/11/rochas-magmaticas/</link>
		<comments>http://ocupantropica.wordpress.com/2008/05/11/rochas-magmaticas/#comments</comments>
		<pubDate>Sun, 11 May 2008 17:16:07 +0000</pubDate>
		<dc:creator>ocupantropica</dc:creator>
				<category><![CDATA[Não classificado]]></category>
		<category><![CDATA[magma]]></category>
		<category><![CDATA[rochas magmáticas]]></category>

		<guid isPermaLink="false">http://ocupantropica.wordpress.com/?p=50</guid>
		<description><![CDATA[No nosso país são abundantes os afloramentos de rochas magmáticas, que condicionam, nalgumas regiões, as paisagens, os solos, o tipo de ocupação humana, a fauna, a flora e a agricultura, ou seja, o ordenamento da superfície do território. As rochas magmáticas resultam da solidificação e arrefecimento do magma. Se essa consolidação ocorre no interior da [...]<img alt="" border="0" src="http://stats.wordpress.com/b.gif?host=ocupantropica.wordpress.com&amp;blog=2839396&amp;post=50&amp;subd=ocupantropica&amp;ref=&amp;feed=1" width="1" height="1" />]]></description>
			<content:encoded><![CDATA[<p style="text-align:justify;">No nosso país são abundantes os afloramentos de rochas magmáticas, que condicionam, nalgumas regiões, as paisagens, os solos, o tipo de ocupação humana, a fauna, a flora e a agricultura, ou seja, o ordenamento da superfície do território.</p>
<p style="text-align:justify;">As rochas magmáticas resultam da solidificação e arrefecimento do magma. Se essa consolidação ocorre no interior da Terra, a grande profundidade, origina rochas intrusivas ou plutónicas; se o magma ascende à superfície ou consolida perto dela, dá origem a rochas extrusivas ou vulcânicas.</p>
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<p style="text-align:justify;"> </p>
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