Moraines in the Chilean Lake District : form, process and chronology
The moraines are made up of stratified glaciofluvial sediments overthrust on their proximal flanks by clay-rich tills composed of reworked glaciofluvial and glaciolacustrine sediments. A single model explains the location, morphology, sediments and structures of the moraines. The key point is that o...
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University of Edinburgh
1995
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.641544 |