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Lakes Nicaragua and Managua are large, rather shallow, fresh-water bodies that lie in a late Tertiary and Quaternary graben in western Nicaragua. The bottom sediments comprise highly organic diatomaceous volcanic silts and clays in which quartz plagioclase feldspar, dioctahedral montmorillonite and volcanic glass are the principal constituents. ' Organic nitrogen content of the lake sediments r...
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ژورنال
عنوان ژورنال: Hispanic American Historical Review
سال: 1930
ISSN: 0018-2168,1527-1900
DOI: 10.1215/00182168-10.1.90