ABSTRACTS / RESUMES - Comitato Glaciologico Italiano

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THE CONFERENCE IS UNDER THE HIGH PATRONAGE OF THE PRESIDENT OF THE ITALIAN REPUBLIC LA CONFERENCE EST PATRONEEPAR LE PRESIDENT DE LA REPUBLIQUE ITALIEl'fNE PATRONAGE Presidenza del Consiglio dei Ministri Ministero degli Affari Esteri Ministero dell' Ambiente Ministero dei Lavori Pubblici Ministero dell'Universita e della Ricerca Scientifica e Tecnologica Regione Emilia-Romagna . Provincia di Bologna Comune di Bologna Universita degli Studi di Bologna Cogeoenvironment of the International Union of Geological Sciences SPONSORSHIPS / SPONSORISATIONS European Commission - Directorate General XII for Science, Research and Development CNR - <strong>Comitato</strong> Nazionale per Ie Scienze Geologiche e Minerarie CNR - Gruppo Nazionale per la Difesa dalle Catastrofi Idrogeologiche MURST - Programma Nazionale di Ricerche in Antartide Dipartimento di Scienze della Terra e Geologico-Ambientali dell'Universita di Bologna Dipartimento di Scienze della Terra dell'Universita di Modena Ferrino & C. s.p.a., Torino Grafiche A&G, Bologna Pagani Geotechnical Equipment di Pagani Ermanno, Calendasco (Piacenza) S.E.M. Sorgenti Emiliane Modena s.r.1., Modena . 4 Banca popolare dell'Emilia Romagna
FOREWORD The «Gruppo Nazionale Geografia Fisica e Geomorfologia» of Italy, on behalf of the International Association of Geomorphologists, takes pleasure to give a warm welcome to Italy to all partecipants to Fourth International Conference on Geomorphology. The Conference intends to collect all new results in the geomorphological research. It intends also to focus on some of the topical problems and of the environment (with particular regard to the Mediterranean) with the contribution of the geomorphological studies. Italy has examples of several different types of landscape ranging from coastal cliffs and beaches to glacial and periglacial alpine peaks, from lakes to alluvial plains and karst morphology, from active volcanoes to seismic areas, all supported by a complex geological structure. Furthermore Italy isatfected by numerous natural or man-induced hazards. In fact, Italy is a country of ancient civilization and the landscape is partially modified by human activity but the intensive development of economic and urban patterns could provide an interesting subject for a study in man-made geomorphology. The organizing committee invited «Geografia Fisica e Dinamica Quaternaria» to publish the main proceedings of the Conference and the journal put at disposal its editions. Hoping that you enjoy the Conference and Italy, very best wishes on behalf of the Italian Organizing Committee and the International Association of Geomorphologists. AVANT-PROPOS The Editor in Chief PAOLO ROBERTO FEDERICI Le «Gruppo Nazionale Geografia Fisica e Ceomorfologiaxd'Italie, au nom de l'Association Internationale de Geomorphologues, est heureux de souhaiter une bienvenue chaleureuse en Italie atout les participants ala Quatrieme Conference Internationale de Ceomorphologie. Le but de la Conference est de rassembler les derniers resultats de la recherche en geomorphologie. Son objectif est egalment de mettre l'accent sur certains problemes d'actualite et concernants 1'environnement (en particulier de la Mediterranee) avec la contribution des etudes en Ceomorphologie. L'Italie presente de nombreux exemples des types de paysage geomorphologique differents qui vont des cotes afalaise et des cotes basses jusq'aux sommets alpins glaciaires et periglaciaires, des lacs aux plaines alluviales et aux morphologies karstiques, des volcans actifs aux zones seismiques, Le tout dans un cadre structural complexe. Par ailleurs, l'Italie possedede nombreux exemples de risques naturals ou d'origine anthropique. En effet l'Italie est un pays d' ancienne civilisation et le paysage est partiellement modifie par l' activite humaine, cependant, 1'intense develloppement de l'economie et de 1'urbanisation ouvrent la possibilite d'une suggestive extension du champ de recherche en geomorphologie. Le Comite d'Organisation a invite «Geografia Fisica e Dinamica Quaternaria» apublier les actes principaux de la Conference et la Revue a mis adisposition ses editions speciales. Dans 1'espoir que votre participation ala Conference soit agreable je vous salue au nom du Comite d'Organisation et de l'Association Internationale de Geomorphologues. le Directeur PAOLO ROBERTO FEDERICI / 5
Page 1: SUPPLEMENTO III - 1997 TOMO 1 The I
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 31 and 32: PSUTY N.P., GARES P.A., SVEKLA W. &
Page 33 and 34: SCHICK A.P., WOLMAN M.G. & GRdDEK T
Page 35 and 36: TANRYVERDIYEV KH.K. & SAFAROV A.S.,
Page 38 and 39: ZERE!\1SKI M., Les morphostructures
Page 41 and 42: TIM B. ABBE & D'AVID R. MONTGOMERY
Page 43 and 44: VALERIO AGNESI 1, MAURIZIO DEL MONT
Page 45: - La troisieme unite est limitee au
Page 50 and 51: ANNALISA AMATO Estimating Pleistoce
Page 52: creased aridity in the southwest US
Page 57 and 58:
DANIELE AROBBA 1, MARIA CRISTINA BO
Page 59 and 60:
planation affecting calcareous succ
Page 61:
SOKOL AxHEMI The geomorphological f
Page 64 and 65:
DAN BALTEANU Slope instability in t
Page 66 and 67:
grass plots in the dolines where an
Page 68 and 69:
een drawn by photogrammetry, From t
Page 70 and 71:
large non-karstic area which gives
Page 74 and 75:
was above average and caused very h
Page 76 and 77:
les niveaux phreatiques a different
Page 78 and 79:
Finse (60 035'N, 7°30'E, 1,350 m a
Page 80 and 81:
On the Po Valley side, the evolutio
Page 83:
SABINA BIGI 1 , ERNESTO CENTAMORE 1
Page 86 and 87:
streams related to periglacial soli
Page 88 and 89:
of the largest biogenic ones (their
Page 90 and 91:
Referring to a topographic basis 1:
Page 94:
en alternance d'un litho-facies imp
Page 99 and 100:
lic roughness [i.e., bedforms, larg
Page 101 and 102:
ERIK L.H. CAMMERAAT A hierarchical
Page 104 and 105:
CLAUDIO A. CARIGNANO & MARCELA A. C
Page 107 and 108:
3. field survey for the control and
Page 110 and 111:
lief formed by glaciers was transfo
Page 112 and 113:
4. The forming of strain basins alo
Page 114 and 115:
With the South Dobroudja Plateau th
Page 116:
Vasilevichy-rnore than 30. Par all
Page 119 and 120:
SIRIO CICCACCI 1, VINCENZO DEL GAUD
Page 121 and 122:
draining south-east part of the mos
Page 123 and 124:
iophysical and sociocultural condit
Page 125 and 126:
ANDREW J.e. COLLISON Simulating the
Page 127 and 128:
Depressions and similar features in
Page 129 and 130:
The Fuegian Andes range extend a in
Page 131 and 132:
The Arlanc plain area of 100 km 2 i
Page 133 and 134:
configuration through the analysis
Page 135:
ges, photographs, maps and the data
Page 138 and 139:
termined from the area-rank relatio
Page 140 and 141:
flow and subsurface flow would trig
Page 142 and 143:
EMMANUELLE DEFIVE 1, JEAN-FRAN\=OIS
Page 146 and 147:
edrock incision. Finally, additiona
Page 148 and 149:
ley. We hypothesize that this ice l
Page 150 and 151:
te Tertiary-Quaternary. In summary,
Page 152 and 153:
niest month of each year (mm); P =
Page 154 and 155:
VALENTINA A. DROUCHITS Formation of
Page 156 and 157:
duse. The human activities, althoug
Page 159 and 160:
e mapped by photogrammetric methods
Page 161 and 162:
stems to external forcing, and in p
Page 164 and 165:
glaciers with the surface method (A
Page 166 and 167:
the xx- Century and its implication
Page 169 and 170:
logical province. Gypsum bedrock ou
Page 171 and 172:
sis are considered. In the northern
Page 173 and 174:
GIOVANNI GABBIANELLI 1 & PAOLO COLA
Page 175:
Northwest of the Cocos Ridge along
Page 178 and 179:
Traditionally to identify periglaci
Page 180 and 181:
Such a lack of finds can only be ex
Page 182 and 183:
common accessory mineral in many ro
Page 185 and 186:
scale slumping of banks observed du
Page 187 and 188:
sponse times are examined for a thu
Page 189:
dence, however, that local Torngat
Page 192 and 193:
2. permafrost very poor in ice with
Page 194 and 195:
Analytical results reveal that long
Page 197 and 198:
ALI HAMZA Crue et erosion des terre
Page 199 and 200:
different.decades show that hydrolo
Page 201:
£85-10 ka, based on the stratigrap
Page 204 and 205:
IRENEE HEYSE The Middelkerke Sandba
Page 206 and 207:
combined in a geographical informat
Page 210 and 211:
FRANCIS HUGUET Haute Ardenne et Hun
Page 212 and 213:
MARIA LAURA IBSEN & EDWARD N. BROMH
Page 214 and 215:
that of West Gujarat coast. It is c
Page 216 and 217:
landslides, and disruption of drain
Page 218 and 219:
tion of particular types of landfor
Page 220 and 221:
ien, il existe merne des cirques ex
Page 222 and 223:
ANNETTE KADEREIT & ANDREAS LANG Col
Page 224 and 225:
Sur le plan volcanologique, le mont
Page 227 and 228:
A.K. KERR 1, DAVID E. SUGDEN 1, HER
Page 230 and 231:
«Pali» d'Hawaii et supposent un e
Page 232 and 233:
is located near the southern margin
Page 235 and 236:
The systematic and multiyear studie
Page 237:
The following major tectonic units
Page 241 and 242:
ANDREAS LANG Optical-dating of Late
Page 246:
2. The reasons for such difference
Page 249 and 250:
examples described in the literatur
Page 251 and 252:
Iinitic deepweathering and subseque
Page 253 and 254:
ZECHUN LIU 1, YONGJIN WANG 1 & XUES
Page 255:
XIXI Lu & DAVID L. HIGGITT Recent c
Page 258 and 259:
In relation with the existence of t
Page 260:
trend (the Arsiani, Sarnsari, J ava
Page 263 and 264:
Large amount of information about m
Page 265:
with large amounts of large woody d
Page 268 and 269:
and impact sediment transport syste
Page 270 and 271:
NASIP MECAJ Physical environment an
Page 272 and 273:
cirque (hanging glacier) and valley
Page 274 and 275:
(maille de 80 m) puis echantillonna
Page 276 and 277:
flows, where flow competence increa
Page 278 and 279:
of 5-20 m in the zone of wave trans
Page 280:
Bulk density is shown to be a very
Page 283 and 284:
MUSEYIB AGABABA MUSEYIBOV The influ
Page 287 and 288:
per streams. In DEM-based networks,
Page 289 and 290:
CHIAKI T. OGUCHl l & YUKINORI MATSU
Page 291 and 292:
Relation between mean altitude of m
Page 293 and 294:
MERVIN OLIVIER 1,2 & GERALD GARLAND
Page 295 and 296:
D. OOSTWOUD WIIDENES, J. POESEN, L.
Page 297 and 298:
process, the character and duration
Page 299:
JOSE LUIS PALACIO-PRIETO & ]OSEFINA
Page 303 and 304:
A «typical» deposit was chosen, a
Page 305 and 306:
vations (continuous cross sections)
Page 307 and 308:
ced a longer, more gentle gradient
Page 309 and 310:
a dendrochronological data series a
Page 311 and 312:
Sediment delivery from a watershed
Page 314 and 315:
pass with a duckfoot chisel, expres
Page 316:
ve (central figure). Feed-back proc
Page 319 and 320:
events have an immediate direct imp
Page 321:
JORGE RABASSA 1, MARCELO ZARATE 2,
Page 324 and 325:
TERESA RAMIREZ-HERRERA Active tecto
Page 326 and 327:
of associated rainfall. In optimal
Page 328:
ock glaciers, the conditions of for
Page 331 and 332:
FELIPE R. RrVELLI Les glissements a
Page 333 and 334:
The influence of groundwater icings
Page 335 and 336:
MARK E. RUSE & MR. PEART The spatia
Page 337 and 338:
T AREK M. SADEK, CHRIS J. GIPPEL, R
Page 339 and 340:
Initially these measurements were m
Page 343 and 344:
JOSE MANUEL SAYAGO Geomorphic indic
Page 345 and 346:
to the theoretical maximum predicte
Page 347 and 348:
culated. Even without considering t
Page 349 and 350:
lowed any more and problems arose.
Page 351 and 352:
with flow through the soil, we reco
Page 353 and 354:
ture and other thermodynamic parame
Page 355 and 356:
solutions that predict the continuo
Page 357 and 358:
and features of various types, size
Page 359 and 360:
part of the basin. These deposits a
Page 361 and 362:
tiated by salt dissolution in the m
Page 363 and 364:
The prevailing part of greater form
Page 365 and 366:
preservation of these remnants is p
Page 367 and 368:
The Piave River is an alpine stream
Page 369:
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 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 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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