ABSTRACTS / RESUMES - Comitato Glaciologico Italiano

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Scoffin T.P., . .. ... 350 Seiberth C., . . . . . .. . 343 Seidl M.A., 122 Selivanov A., . . . . . . 347 Seliverstov Y.,.. .... 348 Sen P.K., . . . .. 348 Seppala M.,. . . . . . . .. 348 Serafin A., . .. .... 256 Serebryanny L.R., . . .. 349 Sergeev A.P., . . . . . . .. 289 Serrano E.,. . . . . . . .. 349 Shanahan J.J., · .... · 350 Shannon J.,. · · · · · · .. 350 Sherman D.J., . ..... 351 Sheth H.C.,. . . . . . . .. 110 Shimazu H., . . . . . . .. 351 Shishonok N.A., . . . . .. . 352 Shopov Y.Y., . . . . . . .. 352 Shroder Jr. J.F., · · · · · .. 353 Shuisky Y.D., . 354 Sias S., . . . . . . . . . . 178, 179 Sidorchuk A.,.. 354 Siedin V., . . . . . . . . . . . 270 Sigova K.I., ... . 239, 353 Silva P.G., . . . . . . . .. 200 Silvano E.S., . . . . . . . . . . 53 Silveira C.S., . . .. 356 Simon A., . . . . . . . 136 Simoni A., . . .. . 301 Sinha B.R.K., . . .. 356 Sisterna J.A., . . . . . . 367 Slattery M.C., . . . . . . . . . . 357 Slaymaker 0., 357 Smiraglia C., . . .. 193, 308, 134 Soldati M.,. . . . . . . . . 129, 302 Sollid,].L., . . . . . . . . 77, 158, 357 Solovieva G.D., . . . . . . . 62, 255 Song L., .'. . . . . . . .. 358 Sonoda M.,. . . . . . . . . . . 292 Soriano A., . .... .. 358 Sowter M.,. . . . . . . . . 359, 369 Spencer T.,. . . . . 360 Spitsa R.A.,. . . . . . . .. 244 Sponholz B., . . . . . . 360 Starn M., . . . . . .. 361 Stankoviansky M., .... 361 430 StanleyD.J., . . . . . .. . 112 Stark C.P., . . . .. .... 208 Starkel L., . . . . -. 362 Stetsyuk V.V.,. . . . . .. . 362 Stocker E.,. .. ... . 364 Stokes M., . . . . . . .. . 200 Streletskaya I.D., . ... . 245 Stroeven A.P.,. . . . . . . . . . 364 Strumia G., . . .. . 308 Stuart F.M.,. . .. . 403 Stiiwe K., . . . . . . . 365 Sugai T., . . . . . . . 366 Sugden D.E., . . . . . .. . 227 Summerfield M.A., . 96, 227, 387 SuniJ., . . . . . . 375 Superson J.,. · · · · · .. · 197 Suranyi K.T., . . . . . . 368 Surdeanu V., . . .. .... 366 Surian N., . . . . . . .. . 366 Suvires G.M., . . . . . .. . 367 Suwa H., . 367 Suwabe K.,.. . 269 Suzuki T., . . . . . . .. . 196 Svekla W., . . . . . 318 Swanson F.J., . . .. .... 188 Szabo L., .... . 368 Szalai Z., . . . . . . . 368 Szatmarij., . . . . . . .. . 272 Takahashi K., ... ... 369 Takenaka C., . . . . 294 TaIling P., . . . . . 359, 369 Tanaka K., . . . . . 269, 370 Tanaka Y.,. . . .. 370 Tang C., . .. 371 Tanryverdiyev Kh.E., . . .. . 371 Tarchiani U., ... ... 57 Tarnai T., . . . 69 Tavarnelli E., . . . . . . 187 Tchakerian V.P., . ... . 372 Tchoua M.F., . .. . 223 Tecca P.R.,. . . . . . . . . . . 133 Tegene B., . . .. . 372 Tekeli 0.,. 149 Tellini C.,. 192
Terranova R., . . . . .. .92, 373 Terwindt J., · · · · 208 Thiam M.D., 374 Thiry M., . . . . . . . . . . . 75 Thomas A.,. . . . . . . . . . . 265 Thomas M.F., 374 Thorne C.R., . . . . . . . . . . 375 Thornes J.B., .... .. 350 Thorp M.B., . . . . 374 Thouret J.-C.,. · · · · . . . . . 375 Tikkanen M., . . . . . . . . . . 376 Tindale N.W.,.. 372 Tisnerat N., . . . . . . 304 Titkov S.N., 377 Tochilina S., . 270 Toda M., . 378 Tokunaga E., . . . . . . 378 Toledo M.A., 379 Toraldo L., . 155 Tosaki S., . . . . . . . . . . . 414 Tosatti G., . 301 Touchais G., 170 Tran K.T., . 379 Tribak A., . 380 Trustrum N.A., . . . . . . . . . 380 Tsankov L.T.,. . . . . . . . . . 352 Tucker G.E., . . . . . . . . 381, 391 Tudhope A.W., . . . . . . . . . 360 Tudose C.,. . . . . . . . . . . 212 Turkowska K.,. . . . . . . . . . 381 Turon E., . . . . . . . 210 Tvalchrelidze M.,. . .. ... 382 Twidale C.R., . . . . . . 393 UbedaX., ... Udintsev G.B.,. . Ufimtsev G.F.,. . UmerM., ... Umhoefer P.]., . . Ungureanu I.B., . Urban Lamadrid G.,. . Urbanek ].,. . . . . Urbani A., . . . . . Urushibara-Yoshino K., . . . . . . . . . 383 · .. . 344 · . . . . . 383 · . . . . . 59 · . . . . . 267 · .. . 384 · .. . 384 · . . . . . 384 · . . . . . 133 385 Ushakov S.A.,. . Ushakova I.S.,. . Ushmanov V.V., . 385 . . 385 386 Valadas B.,. . . . . 130 Valente A.,. . . . . 140 Valigi D., . . . . . . .. . 151 van der Beek P., . . . . . 387 Van Huele W., . . . . .. . 387 van Wesemael B.,. . . . . . . . . 313 Vandekerckhove L., .... 295, 388 Vandenberghe]., . . . . . 388 Vanuzzo C., . . . . 167, 389 Vanwesenbeeck V., . 389 Varushenko A.N.,. 62 Vasilichuk A.C., 390 Vasilichuk Y., . 390 Vecchione C., . . 140 Velasquez E., . . 391 Veneziano D., . 291 Veni G.,. . . . . .. 392 Ventura R.,. . . . . . . . . 115, 134 Vergnolle-Mainar C.,.. .... 392 Vetuschi Zuccolini M., . . . 104 Viana R.,. . .. 391 Vidal G.,. . . . . . . . 280 Vidal Romani ].R., 393 Vieira G.T.,.. .. 393 Vijarnsorn P.,.. 135 Viles H.A.,. . . 186, 394 VillavicencioJ.M., · · · . 395 Vita F., . . . . . . . . 91 Vittorini S.,. . . . . . . . . . . 395 Vittuari L.,. . . . . .. .. 105 Vogt H.,. . . . . .. ... 396 Vogt T.,. . . . . . . . .. 396 Vonder Miihll D.,. 396 Vykhovanets G.V., . . . . . . . . 397 Wade S.D., . Wainwright]., . . . . Walling D.E., . Wang Q.]., . . . . 125 . 273, 399 . 297 · . . 337 431
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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
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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
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island lands, answering the top par
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led with debris material of various
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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 423 and 424: Firpo M., .... ..57, 104 Fisher D.M
Page 426 and 427: Lespez L.,. . . . . . . . . . . 247
Page 428 and 429: Palmentola G.,. . . . .. ., 265 Pal
Page 432: Wang Y., . . . . . 253, 399 Waragai
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ABSTRACTS / RESUMES - Comitato Glaciologico Italiano

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