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Quaternary paleoenvironments - methods

Historical data: methods for reconstructing Holocene glacier fluctuations


 

historical etching of glacierGlacial fluctuations in the Holocene can be reconstructed using various methods of differing precision and covering different periods back into the past.

The following table presents an overview of each method with links to further details.
 


 

Methods for reconstructing Holocene glacier fluctuations

Holocene (post-glacial)

10000 yBP Little Ice Age Today
      1000       500     100
   
         
                   

Glaciological methods

Hydrological, meteorogical and glaciological methods Direct measurement of snow and firn accumulation, ablation and estimation of the mass balance

 
Geodesic methods Length variations, calculation of volume and surface fluctuations using serial photographs and measurements
 

Historical methods

Maps and relief models  
Visual records Engravings, paintings, drawings, photographs
 
Written accounts Chronicles, contracts of purchase concerning Alpine pastures near glaciers, hand written documents and travel books, scientific papers and books about the Alps and glaciers
 

 

Archeological methods

Traces of ancient and human activity in the vicinity of glaciers which can be correlated with the development of the glacier (foundations and beams from old buildins, remain of abandoned irrigation channels, particularly in the Valaisian Alps). Dating with written accounts, 14C and dendrochronology
 

Field methods

Mapping the proglacial area with the moraine ridges Fossil soils, dating with 14C
 
Fossil trees (trunks, branches and roots), dating with 14C
 

 

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29 August 2011
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