<?xml version="1.0"?>
<?xml-stylesheet type="text/xsl" href="https://ontobee.org/ontology/view/MICRO?iri=http://purl.obolibrary.org/obo/ENVO_00000312"?>
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    <!-- http://purl.obolibrary.org/obo/ENVO_00000086 -->

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    <!-- http://purl.obolibrary.org/obo/ENVO_00000312 -->

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        <rdfs:label rdf:datatype="http://www.w3.org/2001/XMLSchema#string">sandur</rdfs:label>
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        <oboInOwl:id rdf:datatype="http://www.w3.org/2001/XMLSchema#string">ENVO:00000312</oboInOwl:id>
        <ns2:IAO_0000115 rdf:datatype="http://www.w3.org/2001/XMLSchema#string">The plain formed by the large amounts of silt and sediment, picked up as a glacier erodes the underlying rocks as it moves slowly downhill, and at the snout of the glacier, meltwater can carry this sediment away from the glacier and deposit it on a broad plain. The material in the outwash plain is often size-sorted by the water runoff of the melting glacier with the finest materials, like silt, being the most distantly re-deposited, whereas larger boulders are the closest to the original terminus of the glacier.</ns2:IAO_0000115>
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