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      <title>Remake Of The Wonder Of Nature by Amirul</title>
      <link>https://padlet.com/m10585470/d0dpv1i6mh6625a3</link>
      <description></description>
      <language>en-us</language>
      <pubDate>2024-07-15 01:15:49 UTC</pubDate>
      <lastBuildDate>2024-07-15 01:42:51 UTC</lastBuildDate>
      <webMaster>hello@padlet.com</webMaster>
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      <item>
         <title>CAVE IN MALAYSIA</title>
         <author>m10585470</author>
         <link>https://padlet.com/m10585470/d0dpv1i6mh6625a3/wish/3053038462</link>
         <description><![CDATA[<p><strong>cave</strong> or <strong>cavern</strong> is a natural void in the <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Earth#Surface">ground</a>,<a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Cave#cite_note-1"><sup>[1]</sup></a><a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Cave#cite_note-2"><sup>[2]</sup></a> specifically a space large enough for a human to enter. Caves often form by the <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Weathering">weathering</a> of rock and often extend deep underground. The word <em>cave</em> can refer to smaller openings such as <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Sea_cave">sea caves</a>, <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Rock_shelter">rock shelters</a>, and <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Grotto">grottos</a>, that extend a relatively short distance into the rock and they are called <em>exogene</em> caves. Caves which extend further underground than the opening is wide are called <em>endogene</em> caves</p>]]></description>
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         <pubDate>2024-07-15 01:15:49 UTC</pubDate>
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      <item>
         <title>CLIFF</title>
         <author>m10585470</author>
         <link>https://padlet.com/m10585470/d0dpv1i6mh6625a3/wish/3053038464</link>
         <description><![CDATA[<p>a cliff is <strong>an area of rock which has a general angle defined by the vertical, or nearly vertical</strong>. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers.</p>]]></description>
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         <pubDate>2024-07-15 01:15:49 UTC</pubDate>
         <guid>https://padlet.com/m10585470/d0dpv1i6mh6625a3/wish/3053038464</guid>
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      <item>
         <title>COAST </title>
         <author>m10585470</author>
         <link>https://padlet.com/m10585470/d0dpv1i6mh6625a3/wish/3053038466</link>
         <description><![CDATA[<p>The <strong>coast</strong>&nbsp;– also called the <strong>coastline</strong>, <strong>shoreline</strong>, or <strong>seashore</strong>&nbsp;– is defined as the area where <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Land">land</a> meets the <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Ocean">ocean</a>, <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Coast#cite_note-1"><sup>[1]</sup></a><a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Coast#cite_note-2"><sup>[2]</sup></a> or as "a line that forms the boundary between the land and the ocean or a <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Lake">lake</a>".<a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Coast#cite_note-3"><sup>[3]</sup></a> Shores are influenced by the <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Topography">topography</a> of the surrounding landscape, as well as by water induced <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Erosion">erosion</a>, such as <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Wind_wave">waves</a>. The <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Geology">geological</a> composition of <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Rock_(geology)">rock</a> and <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Soil">soil</a> dictates the type of shore that is created. <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Earth">Earth</a> contains roughly 620,000&nbsp;km (390,000&nbsp;mi) of coastline.</p>]]></description>
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         <pubDate>2024-07-15 01:15:49 UTC</pubDate>
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      <item>
         <title>GLACIER</title>
         <author>m10585470</author>
         <link>https://padlet.com/m10585470/d0dpv1i6mh6625a3/wish/3053038468</link>
         <description><![CDATA[<p>A <strong>glacier</strong> (<a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/American_English">US</a>: <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Help:IPA/English">/ˈɡleɪʃər/</a>; <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/British_English">UK</a>: <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Help:IPA/English">/ˈɡlæsiər, ˈɡleɪsiər/</a>) is a persistent body of dense ice that is constantly moving downhill under its own weight. A glacier forms where the accumulation of snow exceeds its <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Ablation#Glaciology">ablation</a> over many years, often <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Century">centuries</a>. It acquires distinguishing features, such as <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Crevasse">crevasses</a> and <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Serac">seracs</a>, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Cirque">cirques</a>, <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Moraine">moraines</a>, or <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Fjord">fjords</a>. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Sea_ice">sea ice</a> and lake ice that form on the surface of bodies of water.</p>]]></description>
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         <pubDate>2024-07-15 01:15:49 UTC</pubDate>
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         <title>POND</title>
         <author>m10585470</author>
         <link>https://padlet.com/m10585470/d0dpv1i6mh6625a3/wish/3053038470</link>
         <description><![CDATA[<p>A <strong>pond</strong> is a small, still, land-based <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Body_of_water">body of water</a> formed by pooling inside a <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Depression_(geology)">depression</a>, either naturally or <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Artificiality">artificially</a>. A pond is smaller than a <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Lake">lake</a><a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Pond#cite_note-1"><sup>[1]</sup></a> and there are no official criteria distinguishing the two, although defining a pond to be less than 5 hectares (12 acres) in area, less than 5 metres (16&nbsp;ft) in depth and with less than 30% with <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Aquatic_plant">emergent vegetation</a> helps in distinguishing the <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Ecology">ecology</a> of ponds from those of lakes and <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Wetland">wetlands</a>.<a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Pond#cite_note-2"><sup>[2]</sup></a><a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Pond#cite_note-:02-3"><sup>[3]</sup></a><sup>: 460 </sup> Ponds can be created by a wide variety of natural processes (e.g. on <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Floodplain">floodplains</a> as cutoff <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/River">river</a> channels, by glacial processes, by peatland formation, in coastal dune systems, by beavers), or they can simply be isolated depressions (such as a <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Kettle_(landform)">kettle</a> hole, <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Vernal_pool">vernal pool</a>, <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Prairie_Pothole_Region">prairie pothole</a>, or simply natural undulations in undrained land) filled by runoff, groundwater, or precipitation, or all three of these.<a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Pond#cite_note-4"><sup>[4]</sup></a> They can be further divided into four zones: vegetation zone, open water, bottom mud and surface film.<a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Pond#cite_note-:02-3"><sup>[3]</sup></a><sup>: 160–163 </sup> The size and depth of ponds often varies greatly with the time of year; many ponds are produced by spring flooding from rivers. Ponds are usually <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Fresh_water">freshwater</a> but may be <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Brackish_water">brackish</a> in nature. <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Saline_water">Saltwater</a> pools, with a direct connection to the sea to maintain full salinity, may sometimes be called 'ponds' but these are normally regarded as part of the marine environment. They do not support fresh or brackish water-based organisms, and are rather <a rel="noopener noreferrer nofollow" class="mw-redirect" href="https://en.wikipedia.org/wiki/Tidal_pools">tidal pools</a> or <a rel="noopener noreferrer nofollow" class="mw-redirect" href="https://en.wikipedia.org/wiki/Lagoons">lagoons</a>.</p>]]></description>
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         <pubDate>2024-07-15 01:15:49 UTC</pubDate>
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         <title>RAINFOREST</title>
         <author>m10585470</author>
         <link>https://padlet.com/m10585470/d0dpv1i6mh6625a3/wish/3053038472</link>
         <description><![CDATA[<p><strong>Rainforests</strong> are <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Forest">forests</a> characterized by a closed and continuous tree <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Canopy_(biology)">canopy</a>, moisture-dependent vegetation, the presence of <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Epiphyte">epiphytes</a> and <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Liana">lianas</a> and the absence of wildfire. Rainforests can be generally classified as <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Tropical_rainforest">tropical rainforests</a> or <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Temperate_rainforest">temperate rainforests</a>, but other types have been described.</p><p>Estimates vary from 40% to 75% of all <a rel="noopener noreferrer nofollow" class="mw-redirect" href="https://en.wikipedia.org/wiki/Biotic_community">biotic</a> <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Species">species</a> being <a rel="noopener noreferrer nofollow" class="mw-redirect" href="https://en.wikipedia.org/wiki/Indigenous_(ecology)">indigenous</a> to the rainforests.<a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Rainforest#cite_note-Variables-1"><sup>[1]</sup></a> There may be many millions of species of plants, insects and <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Microorganism">microorganisms</a> still undiscovered in tropical rainforests. Tropical rainforests have been called the "jewels of the Earth" and the "<a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Medicine_chest_(idiom)">world's largest pharmacy</a>", because over one quarter of natural <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Medicine">medicines</a> have been discovered there.<a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Rainforest#cite_note-2"><sup>[2]</sup></a></p><p>Rainforests as well as endemic rainforest species are rapidly disappearing due to <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Rainforest#Deforestation">deforestation</a>, the resulting <a rel="noopener noreferrer nofollow" class="mw-redirect" href="https://en.wikipedia.org/wiki/Habitat_loss">habitat loss</a> and <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Air_pollution">pollution of the atmosphere</a>.<a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Rainforest#cite_note-3"><sup>[3]</sup></a></p>]]></description>
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         <pubDate>2024-07-15 01:15:49 UTC</pubDate>
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         <title>STREAM</title>
         <author>m10585470</author>
         <link>https://padlet.com/m10585470/d0dpv1i6mh6625a3/wish/3053038477</link>
         <description><![CDATA[<p>A <strong>stream</strong> is a continuous <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Body_of_water">body</a> of <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Surface_water">surface water</a><a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Stream#cite_note-definitions-1"><sup>[1]</sup></a> <a rel="noopener noreferrer nofollow" class="mw-redirect" href="https://en.wikipedia.org/wiki/Current_(stream)">flowing</a> within the <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Stream_bed">bed</a> and <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Bank_(geography)">banks</a> of a <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Channel_(geography)">channel</a>. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long, large streams are usually called <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/River">rivers</a>, while smaller, less voluminous and more <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Intermittent_river">intermittent</a> streams are known as <strong>streamlets</strong>, <strong>brooks</strong> or <strong>creeks</strong>.</p>]]></description>
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         <pubDate>2024-07-15 01:15:49 UTC</pubDate>
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         <title>VALLEY</title>
         <author>m10585470</author>
         <link>https://padlet.com/m10585470/d0dpv1i6mh6625a3/wish/3053038479</link>
         <description><![CDATA[<p>A <strong>valley</strong> is an elongated low area often running between <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Hill">hills</a> or <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Mountain">mountains</a>, which typically contains a <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/River">river</a> or <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Stream">stream</a> running from one end to the other. Most valleys are formed by <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Erosion">erosion</a> of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by <a rel="noopener noreferrer nofollow" href="https://en.wikipedia.org/wiki/Glacier">glacial ice</a>. These glaciers may remain present in valleys in high mountains or polar areas.</p>]]></description>
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         <pubDate>2024-07-15 01:15:49 UTC</pubDate>
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