Late-Quaternary Diluvial Floodstreams in the Mountains of Altai and Tuva (Paleoglaciological Base, Geological Effect, Level of Problem Study)

Details Late-Quaternary Diluvial Floodstreams in the Mountains of Altai and Tuva (Paleoglaciological Base, Geological Effect, Level of Problem Study) Late-Quaternary Diluvial Floodstreams in the Mountains of Altai and Tuva (Paleoglaciological Base, Geological Effect, Level of Problem Study)

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1110r&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1110

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Russian works on geological consequences of giant ice-dammed lake
outbursts in Altai were first published 20 years ago. Recent expeditions
have shown that diluvial formations in regions of America and Eurasia
must be characteristic of all areas that experienced quaternary
glaciation.

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