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      <title>sea and coasts  by Annalisa Faraghini</title>
      <link>https://padlet.com/annalisa_faraghini/6gcw5yfg8vrx</link>
      <description>water action </description>
      <language>en-us</language>
      <pubDate>2019-04-17 10:13:05 UTC</pubDate>
      <lastBuildDate>2019-05-28 18:51:00 UTC</lastBuildDate>
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         <title>Coastal depositional features are formed as result of longshore drift.As waves approaches a beach they pick up sand,shingle and pebbles and these sediments are carried up the beach (swash) at the same angle;it then moves back down (backwash). </title>
         <author></author>
         <link>https://padlet.com/annalisa_faraghini/6gcw5yfg8vrx/wish/364125160</link>
         <description><![CDATA[<div>Sand spit :a long,narrow stretch of sand with one end attached to the mainland<br>Sand bar: when a spit stretches across a bay linking two headlands and it can create an area of water called Lagoon<br>Tombolo: it forms when a beach or sand spit joins up with an offshore island<br>Barrier islands: sandy islands that run parallel to the coastline forming a tidal lagoon between them and the shore<br>Saltmarsh:a sheltered area where silt collects behind a sand spit or a sand bar<br><br>Longshore drift: the zig-zag movement of sediment along a shore caused by waves going up the beach at an oblique angle and returning at right angles<br>Swash:the advance of a sea wave up a beach after the breaking of a wave<br>Backwash:the retreat of a sea wave down the beach after the breaking of a wave</div>]]></description>
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         <pubDate>2019-05-28 18:34:45 UTC</pubDate>
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