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<a accesskey="3" href="page.php?w=chalk_stream&amp;p=2">3.Next</a>
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<p><a href="page.php?w=Image%3AChalkstream.jpg">thumb</a><b>Chalk streams</b> are rivers that rise from springs in landscapes with <a href="page.php?w=chalk">chalk</a> <a href="page.php?w=bedrock">bedrock</a>. Since chalk is <a href="page.php?w=Permeability_%28Earth_sciences%29">permeable</a>, water easily percolates through the ground to the <a href="page.php?w=water_table">water table</a> and chalk streams therefore receive little <a href="page.php?w=surface_runoff">surface runoff</a>. As a result, the water in the streams contains little <a href="page.php?w=sedimentary_organic_matter">organic matter</a></p><p>
<a accesskey="3" href="page.php?w=chalk_stream&amp;p=2">3.Next</a>
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