Does the topographic distribution of the central Andean Puna Plateau result from climatic or geodynamic processes ?

@inproceedings{Strecker2009DoesTT,
  title={Does the topographic distribution of the central Andean Puna Plateau result from climatic or geodynamic processes ?},
  author={Manfred R. Strecker and Ricardo N. Alonso and Bodo Bookhagen and B. Carrapa and I. Coutand and Mathis P Hain and George E. Hilley and Elizabeth Mortimer and L. Schoenbohm and Edward R. Sobel},
  year={2009}
}
Figure 3. West-east swath (location shown in Fig. 1) showing mean topography (solid line), mean of long-wavelength component of topography (dashed line), and mean of short-wavelength component of topography (dotted line) as functions of distance from eastern Puna margin. Vertical line shows transition from internal to external drainage, which we defi ne as the plateau boundary. Scales for mean observed and long-wavelength component of topography are denoted on left y axis; scale for mean of… CONTINUE READING

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