Zur Glazialgeologie der chilenischen Anden

@article{BrggenZurGD,
  title={Zur Glazialgeologie der chilenischen Anden},
  author={J. Br{\"u}ggen},
  journal={Geologische Rundschau},
  volume={20},
  pages={1-35}
}
Geomorphological mapping and landforms characterization of a high valley environment in the Chilean Andes
Abstract Despite the wide diversity of landforms, there are only a few geomorphological maps of the Chilean Central Andes. In this study, we present a detailed geomorphological map on a 1:50.000Expand
Sudden glacier advances in the Cachapoal Valley, Southern Central Andes of Chile (34°S)
Abstract Throughout the Andes Mountains of South America, a general trend of glacier shrinkage has taken place in modern times. However, a few glaciers have undergone considerable temporally advancesExpand
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 geologicalExpand
Chapter 53 – The High-Glacial (Last Glacial Maximum) Glacier Cover of the Aconcagua Group and Adjacent Massifs in the Mendoza Andes (South America) with a Closer Look at Further Empirical Evidence
Abstract In the Mendoza Andes, glacier termini have been reconstructed down to 1220 and 1870 m a.s.l. In the E-flank of the Cerros del Chacay, a glacier reached down to 2060 m. Thus, in the AconcaguaExpand
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,Expand
UPPER QUATERNARY LANDSCAPE AND CLIMATE EVOLUTION IN THE NORTE CHICO (NORTHERN CHILE): AN OVERVIEW
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.Expand
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 aExpand
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 aExpand
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