ABSTRACTS / RESUMES - Comitato Glaciologico Italiano

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De Rita D.,. . . . . . . 118 De S.Kr., 137 De Stefanis E., . 93 Debashis D., . . . . . . 141 Decker V., . . . . . 188 Decleir H.,. . . . . . . . . . . 387 Defive E., .. .. 142 Degiovanni S.B., 142 Degraer G., . . . . . . 78 Dehn M., . .. 125, 143 Del Gaudio V., 119 Del Monte M., 43,74, 114, 118, 132, 143, 144 Delaloye R., . . . .. 174 Delcaillau B., . 298, 280 Denefle M., . . . . . . . . . . 170 Densmore A.L., 145 Di Bucci D., . .. 49 Di Grande A., . 140, 139 Di Maggio C.,. . . . . . .. 43 Di Nocera S., . . . . . . 146 Diaz Diaz J.L., . 85 Diener A., .. 31"8 Dieu J.J., · .. .. 147 Dikareva T.V.,.. 148 Dikau R., . .. 148 Dilek Y., . . . . . . . .. 149 Ding G., . . . . .. ... 111 Dini M., . . . . . . . . . 150 Dinu M., . . . . . . . .. 151 do Eirado Silva L.G.,. . . . .. 136 Do T.-K., . . . . . . . . . . . 379 Doffo N.C.,. . .. 151 Donadio C.,. 140 D'Orefice M., 66, 114, 115, 134 Dorsey R.J., . . . . . . . . 267 Dragoni W., . . . . . . . . . . 151 Dragovich D., 152 Dramis F., . 59, 76, 83, 84, 117, 152 Driscoll K.G.,. . . . . . . . . . 153 Droppo I.G., . . .. 310 Drouchits V.A., . . . . . .. 154 Drysdale R.,. . . . . . . . . . . 154 Ducci D., . . . . . . . .. 155 Dufaure J.-J., · · · · · · · · · · 170 Dukov R., . . .. ... 352 Dumas B., . . . . . . . . . . . 156 422 Dumont J.F., · · Dunkl I., Dunsford H.M., · 156 · 170 · 157 EhlenJ., . 158 Eiken T., 77 Eissen J.-Ph., 375 Ellis M.A., 145 Elmi C., . 158, 173, 301 Enzel Y., 402 Ermini L., 106 Eswaran H., 135 Etzelmiiller B., . 77, 158, 357 Evangelista S., . 159 Evans D.J.A.,. 159, 344 Evans I.S., 160 Evans M., 160 Eze B.E., 161 Fabbri A.G., . . . . . . . . . . 413 Faniran A.,.. .... . 161 Fanning P.,. . . . . . . 162 Fanti R.,. . . . 108 Fantozzi P., . . . . . 83, 187 Fanucci F.,. . . . .. ... 158 Fanzutti G.P., . . . . 138 Farabegoli E.,. . . . .. 105, 162 Farabollini P., . . . . 83 Farrell E.J., · . . . . . . . . . 351 Faugeres J.C.,. . . .. ... 189 Favis-Mortlock D., . . . . . . . 85, 163 Federici P.R., ... . 163 Fedolino M., . . . . 373 Feiznia S., . . . . . . . 164 Felix-Henningsen P.,. . . . 73 Fernandes E., . . . . . . 164 Fernandes M.C., . . . . .. . 123 Fernandes N.F., . . . . . . . . . 165 Ferrari R., . . . . .. 45 Ferreira D.B., . . . .. 165 Ferrer C.S., . . . . . . . . 171 Fielding E.J., . . . . . .. . 166 Fierz S.,. . . . . . . . . . . . 91 Finocchiaro F., . . . . . . . . . 131
Firpo M., .... ..57, 104 Fisher D.M., . .. ..... 174 Fleming A.,. . . . . . . . . . . 167 Folladori L., 167 Fombutu N.F.,. . . . . . .. 168 Fontugne M., . . . . . . . . . . 304 Ford D.C.,. . . . . . . . . 168, 352 Fort M.,. . . . . .. ... 169 Forti P.,. . . . . . . . 131 Fouache E.,. ... ... 170 Fragoso M., . . . . . . . . . . 92 Franzinelli E., . . . . . . 241 Frasheri E.,. .. 235 Fredi P.,. . 43, 74, 115, 118, 132, 143, 144 Freire Allemao A.V.,. . . . . . . . 123 French J.R.,. . . . . . . . . . . 360 Frisch W., . . . . . .. .. 170 Frumkin A., . . 171 Full W.E., . . . 159 Fumanal M.P.,. . . . . . 171 Funiciello R., . . . . . . . . . . 74 Gabbani G., . . . .. ... 106 Gabbianelli G., . . . . . . . 158, 173 Gaki-Papanastassiou K., . . . . . . 261 Galicia-Sarmiento L., 254 Gallagher K., .. 96 Gallo A., . . . . . .. .. 155 Gandolfi M., . . . . . 129 Garcia Lozano L.C., . .... 138 Garcia M.T., . . . . . . .. 255 Garcia-Oliva F., . . . . . . . . . 254 Gardaz J.-M., . . . . . . . . . . 174 Gardner T.W., . . . . . . . 174, 306 Gares P.A., . 318, 357 Gargini A., . 106 Garland G., 293 Gasperi G., . . . . 301 Gatti M., . .. 88 Gavrilov A.A.,.. 175 Gebhardt A., 304 Gebica P., . . . . . . . 176 Geczi R., . . . . .. ... 176 Geitner C., . . . . . . . 73 Gendugov V.M., . 238 Genevois R., . . . . 301, 133 Gentili B., . . . . 55, 83 Gentili G., . . . . . . . 176 Georgiev L.N.,. . . . . . . . . . 352 Georgiev S., . . 352 Gerasimenko N.P., . . 177 Ghersi A., . . . . . 70 Ghirotti M., . . . . 301 Giardini G., . . . . 66 Gibertini M., . . . . . . 301 Gil Sauri M.A.,. . . . 84 Giles D.P., ... . . 177 Ginesu S., . . . 178, 179 Giorgi G., . . . . . . . . . . . 179 Giovannini A.,. .. ..... 180 Gippel C.J.,. . . . . . . 337' Giusti C., . . . . . . . . . . . 180 Giusti E., . .. . ..... 176 Glade T., . . . . . . . . . 130, 181 Gleadow A.J.W.,. . . . . 181 Golosov V.N.,. . . . . . . . 182, 183 Gomez B., .. ... 183, 380 Gonthier E., . . . . . . 189 Gore D., . . . . . . . .. 60 Gorelikova N.V.,. . . . . . . . . 305 Gosse J.,. · · · · · . . . . . . 188 Goswami D.C., . . . . . . . . . 184 Goswami S.C.,. . . . . . . . . . 185 Gottesfeld A.S.,. 185 Goudie A., . . . 186 Gourari L.,. . . . . . . 186 Govers G.,. . . . . . . . . . 78, 313 Goy J., · · . . . . . . 200 Grab S.W.,. . . . .. ... 186 Graciotti R., '" .. 66, 114 Grandgirard V.,. 187 Granger D.E.,. . . . . . . . . . 187 Grangie P.F., . . . .. ... 80 Grant G.E., . . . . . . . 388 Grante P., . ... . 313 Gray J.T., . . . . .. 188 Grayson R.B., ... 337 Grecu P., . . . . . . . . . . . 189 Green A.A.,. 282 Green P.F.,. . . . . . . 401 Greenberg H.M.,. . .. ... 98 423
Page 1:
SUPPLEMENTO III - 1997 TOMO 1 The I
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THE CONFERENCE IS UNDER THE HIGH PA
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Thursday, August 28 th 9.00 Registr
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Sessions / Seance Table of correlat
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BADYUKOVA E.N., VARUSHENKO A.N. & S
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BONDESAN A., A glaciological map of
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CHEVAL S., Relation between the cli
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stern Argentina. Geomorphic compone
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FERNANDES N.F. & SANTI C.B., The co
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HIGGIT D.L. & ALLISON R.J., The for
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KERTESZ A., Aridification - Climate
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MITINA N.N., Geomorphologic peculia
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PSUTY N.P., GARES P.A., SVEKLA W. &
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SCHICK A.P., WOLMAN M.G. & GRdDEK T
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TANRYVERDIYEV KH.K. & SAFAROV A.S.,
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ZERE!\1SKI M., Les morphostructures
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TIM B. ABBE & D'AVID R. MONTGOMERY
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VALERIO AGNESI 1, MAURIZIO DEL MONT
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- La troisieme unite est limitee au
Page 50 and 51:
ANNALISA AMATO Estimating Pleistoce
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creased aridity in the southwest US
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DANIELE AROBBA 1, MARIA CRISTINA BO
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planation affecting calcareous succ
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SOKOL AxHEMI The geomorphological f
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DAN BALTEANU Slope instability in t
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grass plots in the dolines where an
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een drawn by photogrammetry, From t
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large non-karstic area which gives
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was above average and caused very h
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les niveaux phreatiques a different
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Finse (60 035'N, 7°30'E, 1,350 m a
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On the Po Valley side, the evolutio
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SABINA BIGI 1 , ERNESTO CENTAMORE 1
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streams related to periglacial soli
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of the largest biogenic ones (their
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Referring to a topographic basis 1:
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en alternance d'un litho-facies imp
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lic roughness [i.e., bedforms, larg
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ERIK L.H. CAMMERAAT A hierarchical
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CLAUDIO A. CARIGNANO & MARCELA A. C
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3. field survey for the control and
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lief formed by glaciers was transfo
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4. The forming of strain basins alo
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With the South Dobroudja Plateau th
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Vasilevichy-rnore than 30. Par all
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SIRIO CICCACCI 1, VINCENZO DEL GAUD
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draining south-east part of the mos
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iophysical and sociocultural condit
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ANDREW J.e. COLLISON Simulating the
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Depressions and similar features in
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The Fuegian Andes range extend a in
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The Arlanc plain area of 100 km 2 i
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configuration through the analysis
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ges, photographs, maps and the data
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termined from the area-rank relatio
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flow and subsurface flow would trig
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EMMANUELLE DEFIVE 1, JEAN-FRAN\=OIS
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edrock incision. Finally, additiona
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ley. We hypothesize that this ice l
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te Tertiary-Quaternary. In summary,
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niest month of each year (mm); P =
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VALENTINA A. DROUCHITS Formation of
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duse. The human activities, althoug
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e mapped by photogrammetric methods
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stems to external forcing, and in p
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glaciers with the surface method (A
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the xx- Century and its implication
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logical province. Gypsum bedrock ou
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sis are considered. In the northern
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GIOVANNI GABBIANELLI 1 & PAOLO COLA
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Northwest of the Cocos Ridge along
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Traditionally to identify periglaci
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Such a lack of finds can only be ex
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common accessory mineral in many ro
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scale slumping of banks observed du
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sponse times are examined for a thu
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dence, however, that local Torngat
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2. permafrost very poor in ice with
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Analytical results reveal that long
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ALI HAMZA Crue et erosion des terre
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different.decades show that hydrolo
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£85-10 ka, based on the stratigrap
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IRENEE HEYSE The Middelkerke Sandba
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combined in a geographical informat
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FRANCIS HUGUET Haute Ardenne et Hun
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MARIA LAURA IBSEN & EDWARD N. BROMH
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that of West Gujarat coast. It is c
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landslides, and disruption of drain
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tion of particular types of landfor
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ien, il existe merne des cirques ex
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ANNETTE KADEREIT & ANDREAS LANG Col
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Sur le plan volcanologique, le mont
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A.K. KERR 1, DAVID E. SUGDEN 1, HER
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«Pali» d'Hawaii et supposent un e
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is located near the southern margin
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The systematic and multiyear studie
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The following major tectonic units
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ANDREAS LANG Optical-dating of Late
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2. The reasons for such difference
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examples described in the literatur
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Iinitic deepweathering and subseque
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ZECHUN LIU 1, YONGJIN WANG 1 & XUES
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XIXI Lu & DAVID L. HIGGITT Recent c
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In relation with the existence of t
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trend (the Arsiani, Sarnsari, J ava
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Large amount of information about m
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with large amounts of large woody d
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and impact sediment transport syste
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NASIP MECAJ Physical environment an
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cirque (hanging glacier) and valley
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(maille de 80 m) puis echantillonna
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flows, where flow competence increa
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of 5-20 m in the zone of wave trans
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Bulk density is shown to be a very
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MUSEYIB AGABABA MUSEYIBOV The influ
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per streams. In DEM-based networks,
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CHIAKI T. OGUCHl l & YUKINORI MATSU
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Relation between mean altitude of m
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MERVIN OLIVIER 1,2 & GERALD GARLAND
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D. OOSTWOUD WIIDENES, J. POESEN, L.
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process, the character and duration
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JOSE LUIS PALACIO-PRIETO & ]OSEFINA
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A «typical» deposit was chosen, a
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vations (continuous cross sections)
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ced a longer, more gentle gradient
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a dendrochronological data series a
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Sediment delivery from a watershed
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pass with a duckfoot chisel, expres
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ve (central figure). Feed-back proc
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events have an immediate direct imp
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JORGE RABASSA 1, MARCELO ZARATE 2,
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TERESA RAMIREZ-HERRERA Active tecto
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of associated rainfall. In optimal
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ock glaciers, the conditions of for
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FELIPE R. RrVELLI Les glissements a
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The influence of groundwater icings
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MARK E. RUSE & MR. PEART The spatia
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T AREK M. SADEK, CHRIS J. GIPPEL, R
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Initially these measurements were m
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JOSE MANUEL SAYAGO Geomorphic indic
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to the theoretical maximum predicte
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culated. Even without considering t
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lowed any more and problems arose.
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with flow through the soil, we reco
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ture and other thermodynamic parame
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solutions that predict the continuo
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and features of various types, size
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part of the basin. These deposits a
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tiated by salt dissolution in the m
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The prevailing part of greater form
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preservation of these remnants is p
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The Piave River is an alpine stream
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KENICHI TAKAHASHI l , YUKINORI MATS
Page 372 and 373: island lands, answering the top par
Page 374 and 375: led with debris material of various
Page 377 and 378: location, as a result of the deglac
Page 381 and 382: lake deposition, and deviations fro
Page 383 and 384: XAVIER UBEDA, LOURDES REINA & MARIA
Page 385 and 386: There is certain traditional hypoth
Page 387 and 388: PETER VAN DER BEEK\ MIKE SUMMERFIEL
Page 390: posmon, height, orientation and asy
Page 394: Serra do Geres (NW Portugal). This
Page 399: JOHN WAINWRIGHT\ ANTHONY J. PARSONS
Page 402 and 403: Thus burial-related heating cannot
Page 404 and 405: expression and underground, present
Page 406: stern Australia. Earlier workers us
Page 409: SHU]I YAMADA The role of soil creep
Page 415: HUNAN ZHANG & WEIGUANG CHEN Feature
Page 418 and 419: the rainy season 1995: a deep chann
Page 420: Benn D.I., .. 324 Bera A.K., . 76 B
Page 426 and 427: Lespez L.,. . . . . . . . . . . 247
Page 428 and 429: Palmentola G.,. . . . .. ., 265 Pal
Page 430 and 431: Scoffin T.P., . .. ... 350 Seiberth
Page 432: Wang Y., . . . . . 253, 399 Waragai
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ABSTRACTS / RESUMES - Comitato Glaciologico Italiano

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