Summaryhttps://peda.net/id/7bde8f583542020-12-03T11:32:38+02:00https://peda.net/:static/539/peda.net.logo.bg.svg<div class="license">Tämän sivun lisenssi <a rel="license" href="https://peda.net/info">Peda.net-yleislisenssi</a></div>
Goalshttps://peda.net/id/7bdee3233542020-06-03T15:12:21+03:00<ul>
<li><span>Being able to describe the causes and effects of post-glacial rebound.</span></li>
<li><span>Being able to describe different Finnish soil types.</span></li>
</ul>2020-12-03T11:32:38+02:00Summaryhttps://peda.net/id/7bdf43e63542020-06-03T15:15:13+03:00<div class="eoppi-summary">
<ul>
<li>During the last Ice Age, a heavy ice mass caused the Earth's crust to sink into the planet's mantle.</li>
<li>When the ice mass retreated and melted, the planet's crust began to rise back to its original level in a process known as post-glacial rebound.</li>
<li>The Baltic Sea has experienced great changes after the last Ice Age.</li>
<li>Finnish mineral and organic soil types have been formed during and after the last ice age.</li>
<li>Key words: mineral soil types, organic soil types, post-glacial rebound, clay valleys, ancient shores, relic species.</li>
</ul>
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2020-12-03T11:32:38+02:00