- Page 1: SUPPLEMENTO III - 1997 TOMO 1 The I
- Page 4 and 5: THE CONFERENCE IS UNDER THE HIGH PA
- Page 6 and 7: Thursday, August 28 th 9.00 Registr
- Page 9 and 10: Sessions / Seance Table of correlat
- Page 11 and 12: BADYUKOVA E.N., VARUSHENKO A.N. & S
- Page 13 and 14: BONDESAN A., A glaciological map of
- Page 15 and 16: CHEVAL S., Relation between the cli
- Page 17 and 18: stern Argentina. Geomorphic compone
- Page 19 and 20: FERNANDES N.F. & SANTI C.B., The co
- Page 22 and 23: HIGGIT D.L. & ALLISON R.J., The for
- Page 24: KERTESZ A., Aridification - Climate
- Page 28 and 29: MITINA N.N., Geomorphologic peculia
- Page 32 and 33: RIVELLI F.R., Les glissements a Vol
- Page 34 and 35: SLAYMAKER 0., Geomorphology and glo
- Page 36: URUS:HIBAM.-YOSHINO K-. &. MIOTKE F
- Page 39: ABSTRACTS / RESUMES Texts / Textres
- Page 42 and 43: asement-related tectonics as it is
- Page 44 and 45: «abandoned landscapes», of extrem
- Page 47: portion of Edc, the more part stays
- Page 51 and 52: the intermontane basins. The anomal
- Page 55: is constituted of four fields withi
- Page 58 and 59: also to the intense erosive action
- Page 60 and 61: iver channels, (6) change of incisi
- Page 63 and 64: magurskie layers, hieroglyphic and
- Page 65 and 66: FULVIO BARALDI 1, DORIANO CASTALDIN
- Page 67 and 68: Land. Abandoned penguin rookeries a
- Page 69 and 70: y mapping the respective moraine ri
- Page 71: identify portions with differential
- Page 75 and 76: een formulated that the activity of
- Page 77 and 78: ecent decades as it was associated
- Page 79 and 80: that it not only geopardises the cu
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This software makes photographic re
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PEDRO BLANCO SEGUNDO, JOSE R. HERNA
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took place: various phases are char
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Together with the Geomorphological
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MARGOT BOSE Glacial landforms in Ta
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data are available maps of palaeote
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BENGT CALLES & LENA KULANDER Erosiv
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The vegetation of the two study are
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MANDY CAROLISSEN Investigating bedl
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GIOVANNI BATTISTA CASTIGLIONI The G
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area. Overall, the geomorphological
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depositional velocity of CaC0 3 •
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EDI CHIARINI 1, MAURIZIO DEL MONTE
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f) deposition of recent and present
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marine succession ranging in age be
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In the first case, it is clear that
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cially during intense rainfall peri
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higher along the softer terrains, o
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and dams) are analysed in relation
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ment gestionnaire des indispensable
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LEANDRO D'ALESSANDRO, LINA DAVOLI,
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GIACOMO D'AMATO AVANZI Landslides t
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The numerical model used in this st
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The underwater geomorphologic surve
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This action has been changed by vol
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Two drainage patterns coexist in th
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therefore result very useful tools
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etter historical data and field obs
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MIHAELA DINU Geomorphological hazar
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press) show that, during the Holoce
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vertines are cyanobacteria. The pre
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the shifts and deflections of the M
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and eastern England are assessed us
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, PATRICIA FANNING Accelerated eros
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vegetation, de frequence et de dist
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area that is roughly 25 km wide run
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events, so that their impact can be
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M. PILAR FUMANAL, CARLOS FERRER & A
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Roman delta; ii) the Renaissance de
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aerial photography data base with a
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to the fluvial dinamics. This proce
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sans partage d'une aire ou les vest
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e readily remobilised and transport
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tive, with a smaller portion of the
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ground surface. The concentrations
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- a detailed geomorphological map w
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une graduelle augmentation jusqu'a
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of these cities, located near activ
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exceed 20-30 m. Presently, most of
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The slopes have an estimated mean a
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aLAVI HEIKKINEN & PETER BRUSILA Fie
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terations to the coastline shape ar
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Britain. Engineering geomorphology
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We have focused our studies on the
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At present ocean floor relief devel
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NANCY L. JACKSON 1 & KARL F. NORDST
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carried out in this area. The above
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JOHN D. JANSEN & GARY J. BRIERLEY L
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include long ridges and isolated es
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se connection with the local morph-
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ALEXANDRE M. KALININ The types of s
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cussed on the interpretation of Sir
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ALASTAIR J. KIRK A field-based rain
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YOSHINORI KODAMA & KEIGO NAKAMURA A
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The formations which are submitted
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F.S. LAI & W. MALANDI Particulate o
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Rondonia, Southwestern Amazonia, ne
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prehistoriques et constructions ant
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from northeast to southwest; coveri
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with the morphological analyses by
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lORGE LOPEZ-BLANCO ', LEOPOLDO GALI
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lOAN MAC & lOAN IRIMUS The evolutio
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Variability in bed elevations was e
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In the Middle - Late Pleistocene, t
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future landsliding. If reforested a
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etc.) - with depressions, saddles o
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tors when studying the mechanism th
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1Pacific Oceanological Institute, F
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erosion might be active due to the
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the most direct connection betweenT
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of the 43-m-high meander could rang
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cal hazard. The geomorphology of th
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north it is limited by the Dauki fa
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VLADIMIR 1. MYSLIVETS The problems
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Classification of seismogravitation
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st Glacial vegetation rather than t
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moved by periglacial processes such
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have been accreting at a noticeable
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are the complete systems of general
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ments are subsequently remobilised.
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tation of a geomorphological map an
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two detailed raster Digital Elevati
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IRINA E. P AVLOVSKAYA The influence
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MANUELA PELFINI 1 & CLAUDIO SMIRAGL
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leozoic sedimentary rocks and was f
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vements during Neogene and Quaterna
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ple monitoring sites (tesserae) and
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ANGELIQUE PRICK Etude experimentale
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MOHAMED QARRO & MOHAMED OUAHID Effe
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LOMBORINCHEN RADNA Periglacial proc
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temporary (Svalbard/Norway) and anc
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has to ensure the existence of beac
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MlRELA RIPEANU & lOAN MAC The evolu
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Swedish-Russian expedition «Tundra
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fragments of roman ceramic, which d
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stly fines to the Gigjukvisl outlet
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show areas of potential sediment so
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PAOLO SANSO The ancient landforms o
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HANS W. SCHENKE 1 & GLEB B. UDINTSE
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96, when approximately 500 mm of pr
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depositional body. The faster the s
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tion analyse of the periglacial lan
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stributed. The lower terraces show
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YURII D. SHUISKY Geomorphology and
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termediate complexes of rocks, The
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All forms show a more or less disti
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more diffusional erosional processe
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land forms conditioned by these pro
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matic conditions (global regulariti
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Our project attempts to model the t
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Observation of debris flows and sed
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CHUAN TANG 1 & JORG GRUNERT 2 Lands
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REMO TERRANOVA The great landslide
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white sand valley fills and terrace
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The movement of rock glaciers is in
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echerches sur la morphogenese perig
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IRINA BRINDUSA UNGUREANU Au sujet d
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V.V. USHMANOV The endogenously orde
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coordinates of the origin and the f
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data. Based on Equation 1, we refor
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and therefore are background ones r
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tend entre la transgression Ouljien
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Quaternary hydrologic budget for th
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were dated using lichenometry and d
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KANGNING XIONG, CAIHUA HE & XING CH
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LILIANA ZAHARIA Les transports soli
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of which there are preserved polish
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AUTHOR INDEX / INDICE DES AUTEURS A
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De Rita D.,. . . . . . . 118 De S.K
- Page 424:
Griboulard R.G.,. . . . . .. 189 Gr
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Melis R.T.,. . . . . . . . . . . 27
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Ramirez-Herrera T., 324 Rutherfurd
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Terranova R., . . . . .. .92, 373 T