Significance of slope sediments layering on physical characteristics and interflow within the Critical Zone - Examples from the Colorado Front Range, USA

Applied Geochemistry

Volumn 26, Issue SUPPL., 2011, Pages

  Völkel, Jörg ^a   Huber, Juliane ^a   Leopold, Matthias ^a  

^a TECHNICAL UNIVERSITY OF MUNICH   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

COLORADO FRONT RANGE; INTERFLOW; LAST GLACIAL; LUMINESCENCE DATING; MULTI-LAYERED; PERIGLACIAL; PHYSICAL AND CHEMICAL PROPERTIES; PHYSICAL CHARACTERISTICS; PLEISTOCENE; SEDIMENT LAYERS; SLOPE DEPOSIT; SLOPE SEDIMENT; SOIL FORMING PROCESS;

CHEMICAL PROPERTIES; CLAY MINERALS; DEPOSITS; GLACIAL GEOLOGY; SEDIMENTOLOGY;

ANOXIC SEDIMENTS;

CLAY MINERAL; GEOMORPHOLOGY; GLACIATION; LAST GLACIAL; LUMINESCENCE DATING; MOUNTAIN REGION; PHYSICOCHEMICAL PROPERTY; SEDIMENT ANALYSIS; SEDIMENTOLOGY; SLOPE; SUBALPINE ENVIRONMENT;

COLORADO; FRONT RANGE; ROCKY MOUNTAINS; UNITED STATES;

EID: 79955963072     PISSN: 08832927     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.apgeochem.2011.03.052     Document Type: Article

References (1)

1. Völkel J., Leopold M., Roberts M.C. The radar signatures and age of periglacial slope deposits in the Central European Highlands of Germany. Permafrost Periglacial Process. 2001, 12:379-387.