Schorre morphology on the south shore of theSaint Lawrence Estuary

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ID: 298820
1968
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Abstract
The salt marshes are characteristic of a cold-temperature region. Ice is an important morpho-sedimentological agent. A large quantity of boulders and coarse sediments are brought by drift ice which also digs and ploughs the surface of the schorre during winter and spring. Four types of salt marshes are common: The first is characterized by numerous shallow subcircular or irregular shaped pans, the second by an abundance of erratics, mostly crystalline boulders, the third by a rocky platform overlaid by a thin veneer of mud, and the fourth is a muddy schorre similar to common marshes of the Atlantic coast of southeastern Canada. The first three have never been described as such in coastal literature. Schorre is a Dutch word that refers to that part of a salt marsh covered by high tides.
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openalex_W2312474781 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Jean‐Claude Dionne
Journal american journal of science
Year 1968
DOI
10.2475/ajs.266.5.380
URL
https://ajs.scholasticahq.com/article/59247.pdf
Keywords Keywords not found

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