The critical role of climate and saprolite weathering in landscape evolution

Earth Surface Processes and Landforms

Volumn 34, Issue 11, 2009, Pages 1507-1521

  Dixon, Jean L ^a   Heimsath, Arjun M ^a   Amundson, Ronald ^b  

^a ARIZONA STATE UNIVERSITY   (United States)

^b UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

Chemical weathering; Climate; Cosmogenic radionuclides; Erosion; Saprolite

Indexed keywords

ARRHENIUS TEMPERATURE; CALIFORNIA; CHEMICAL WEATHERING; CLIMATE; CLIMATE GRADIENTS; COSMOGENIC RADIONUCLIDES; DENUDATION RATES; EROSION RATES; EXTERNAL FORCE; FASTER RATES; INFLUENCE SURFACES; INTERNAL FEEDBACK; LANDSCAPE EVOLUTIONS; LINEAR RELATIONSHIPS; MASS BALANCE; PRODUCTION RATES; RESIDENCE TIME; SAPROLITE; SIERRA NEVADA; SIMILAR PATTERN; SOIL COLUMN; SOIL TRANSPORTS; SOIL WEATHERING; WEATHERED SOILS; WEATHERING RATES;

CHEMICAL REACTIONS; CLIMATE CONTROL; EROSION; FEEDBACK; FORESTRY; GEOCHEMISTRY; MOISTURE CONTROL; RADIOISOTOPES; RADIOMETRY; REACTION RATES; ROCKS; SILICA; SOILS; TECTONICS; ZIRCONIUM;

WEATHERING;

CHEMICAL WEATHERING; CLIMATE EFFECT; COSMOGENIC RADIONUCLIDE; DENUDATION; EROSION; LANDSCAPE EVOLUTION; SAPROLITE; SOIL EROSION;

CALIFORNIA; NORTH AMERICA; SIERRA NEVADA [CALIFORNIA]; UNITED STATES;

EID: 70349188847     PISSN: 01979337     EISSN: 10969837     Source Type: Journal    
DOI: 10.1002/esp.1836     Document Type: Article

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