Zur Glazialgeologie der chilenischen Anden

@article{BrggenZurGD,
  title={Zur Glazialgeologie der chilenischen Anden},
  author={Jens Vor der Br{\"u}ggen},
  journal={Geologische Rundschau},
  volume={20},
  pages={1-35}
}
  • J. Brüggen
  • Published 1 April 1929
  • Geology
  • Geologische Rundschau

Geomorphologic and Glacial Evolution of the Cachapoal and southern Maipo catchments in the Andean Principal Cordillera, Central Chile (34°-35º S)

We present here a reconstruction of the post late Miocene landscape evolution of the western slope of the Andean Cordillera Principal near 34°20’ S. We base our analysis on the available geological

International Lateinamerika-Kolloquium 2009

s and Program Göttingen, April 7-9, 2009 G er ha rd W ör ne r, S te fa n M öl le rM cN et t ( Ed s. ) In te rn at io na l L at ei na m er ik aKo llo qu iu m 2 00 9 Ab st ra ct s an d Pr og ra m

Miocene Landscape Evolution and Geomorphologic Controls on Epithermal Processes in the El Indio-Pascua Au-Ag-Cu Belt, Chile and Argentina

The world-class breccia-, stockwork-, and vein-hosted epithermal Au-Ag-Cu deposits of the central Andean El Indio-Pascua belt, latitudes 29°20' to 30°30' S, were emplaced between 6.2 and 9.4 Ma,

UPPER QUATERNARY LANDSCAPE AND CLIMATE EVOLUTION IN THE NORTE CHICO (NORTHERN CHILE): AN OVERVIEW

  • H. Veit
  • Environmental Science, Geography
  • 1993
The distribution of geoecological units in the Norte Chico is the result of a complex evolution, which is reconstructed here for Upper Quaternary time, based on geomorphologic and pedologic studies.

Ice marginal ramps: An indicator of semi-arid piedmont glaciations

  • M. Kuhle
  • Environmental Science, Geography
  • 1989
Ice marginal ramps are depositional landforms that often developed over several tens of kilometres along the ice margins of large piedmont glaciers in semi-arid environments. The ramps extend with a

Ice marginal ramps: An indicator of semi-arid piedmont glaciations

Ice marginal ramps are depositional landforms that often developed over several tens of kilometres along the ice margins of large piedmont glaciers in semi-arid environments. The ramps extend with a

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