THE ORIGIN OF GLACIALLY FLUTED SURFACES - OBSERVATIONS AND THEORY.BOULTON GS.1976; J. GLACIAL.; G.B.; DA. 1976; VOL. 17; NO 76; PP. 287-309; ABS. FR. ALLEM.; BIBL. 17 REF.Article

DYNAMICS OF GLACIERS AND LARGE ICE MASSESHUTTER K.1982; ANN. REV. FLUID. MECH.; ISSN 0066-4189; USA; DA. 1982; VOL. 14; PP. 87-130; BIBL. 7 P.Article

GIANT GROOVES MADE BY CONCENTRATED BASAL ICE STREAMSGOLDTHWAIT RP.1979; J. GLACIOL.; GBR; DA. 1979; VOL. 23; NO 89; PP. 297-307; ABS. FRE/GER; BIBL. 21 REF.Article

SUBGLACIAL REGELATION WATER FILMHALLET B.1979; J. GLACIOL.; GBR; DA. 1979; VOL. 23; NO 89; PP. 321-334; ABS. FRE/GER; BIBL. 42 REF.Article

THE APPLICATION OF FRACTURE MECHANICS TO THE PROBLEM OF CREVASSE PENETRATION.SMITH RA.1976; J. GLACIAL.; G.B.; DA. 1976; VOL. 17; NO 76; PP. 223-228; ABS. FR. ALLEM.; BIBL. 7 REF.Article

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SEDIMENT CONCENTRATION IN MELT WATERS AS AN INDICATOR OF EROSION PROCESSES BENEATH AN ALPINE GLACIERCOLLINS DN.1979; J. GLACIOL.; GBR; DA. 1979; VOL. 23; NO 89; PP. 247-257; ABS. FRE/GER; BIBL. 12 REF.Article

DIRECT MEASUREMENT OF BASAL WATER PRESSURES. A PILOT STUDY.HODGE SM.1976; J. GLACIOL.; G.B.; DA. 1976; VOL. 16; NO 74; PP. 205-218; ABS. FR. ALLEM.; BIBL. 12 REF.; (INT. SYMP. THERM. REGIME GLACIERS ICE SHEETS. PROC.; BURNABY; 1975)Conference Paper

SPACING OF WATER-FREE CREVASSESNEMAT NASSER S; ORANRATNACHAL A; KEER LM et al.1979; J. GEOPHYS. RES.; USA; DA. 1979; VOL. 84; NO B9; PP. 4611-4620; BIBL. 14 REF.Article

GLOBAL CHANGES IN POSTGLACIAL SEA LEVEL: A NUMERICAL CALCULATIONCLARK JA; FARRELL WE; PELTIER WR et al.1978; QUATERN. RES.; USA; DA. 1978; VOL. 9; NO 3; PP. 265-287; BIBL. 2 P.Article

DEEP SEA CARBONATES: ACOUSTIC, PHYSICAL, AND STRATIGRAPHIC PROPERTIESMAYER LA.1979; J. SEDIMENT. PETROL.; USA; DA. 1979; VOL. 49; NO 3; PP. 819-836; BIBL. 2 P.Article

REGIME DES EAUX SOUTERRAINES ET PALEOMORPHOLOGIE. GEOLOGIE ET HYDROGEOLOGIE DE LA BASSE VALLEE DE L'ARVE (HAUTE-SAVOIE).ARMAND CLAUDE.1978; ; FRA; DA. 1978; 323 P.; BIBL. 5 P.; 132 ILL.; TH: GEOL. APPL./GRENOBLE 1/1978Thesis

GLACITECTONIQUE DANS LA PARTIE EST DE LA REGION DU LAC SAINT-JEAN.TREMBLAY G.1967; CAH. GEOGR. QUEBEC; CAN; 1967(12), NUM. 0024, P. 563 A 566Miscellaneous

QUELQUES PARTICULARITES DE LA DEGLACIATION ET DE LA MORPHOGENESE GLACIAIRE EN LETTONIE.DANILANS I JA.1965; KOSMOS-BIBLIOTHEK.-DTSCH; DEU; 1965, P. 65 A 71Miscellaneous

Die Entstehung der dänischen und norddeutschen Rinnentäler (Tunneltäler) - Glaziologische Gesichtspunkte = La formation des rigoles sous-glaciaires au Danemark et en Allemagne du Nord - Point de vue glaciologiqueSMED, P.Eiszeitalter und Gegenwart. 1998, Vol 48, pp 1-18, issn 0424-7116Article

SEDIMENTOLOGY AND GEOMORPHOLOGY OF DRUMLINS IN WESTERN ALLGAEU, SOUTH GERMANY = LA SEDIMENTOLOGIE ET LA GEOMORPHOLOGIE DES DRUMLINS DANS LA PARTIE ORIENTALE DE L'ALLGAEU, SUD DE L'ALLEMAGNEDE JONG MGG; RAPPOL M; RUPKE J et al.1982; BOREAS; ISSN 0300-9483; NOR; DA. 1982; VOL. 11; NO 1; PP. 37-45; BIBL. 20 REF.; ESQUISSE/COUPE GEOL./ILL./ESQUISSE GEOL.Article

EL MODELADO GLACIAL DEL VALLE DEL DURAN, CERDANYA = LE MODELE GLACIAIRE DE LA VALLEE DU DURAN, CERDAGNEGOMEZ ORTIZ A.1978; REV. GEOGR.; ISSN 0048-7708; ESP; DA. 1978-1979; VOL. 12-13; PP. 17-28; ABS. FRE/ENG; BIBL. 9 REF.; ESQUISSEArticle

ZUR GLAZIALMORPHOLOGIE IN DEN TROCKENTAELERN DES TRANSANTARKTISCHEN GEBIRGES (OSTANTARKTIS) = A PROPOS DE LA MORPHOLOGIE GLACIAIRE DANS LES VALLEES SECHES DE LA CHAINE TRANSANTARCTIQUE (ANTARCTIQUE ORIENTAL)HOEFLE HC.1981; POLARFORSCHUNG; ISSN 0032-2490; DEU; DA. 1981; VOL. 51; NO 2; PP. 197-199; ABS. ENG; BIBL. 8 REF.; 1 TAB. ; TABL./ESQUISSE GEOL.Article

ICE-CORED ROCK GLACIER, GALENA CREEK, NORTHERN ABSAROKA MOUTAINS, WYOMINGPOTTER N JR.1972; GEOL. SOC. AMER., BULL.; U.S.A. ; 1972, VOL. 83, NUM. 0010, P. 3025 A 3058Serial Issue

RELIC PLEISTOCENE PERMAFROST, WESTERN ARCTIC, CANADA.MACKAY JR; RAMPTON VN; FYLES JG et al.1972; SCIENCE; 1972, VOL. 176, NUM. 4041, P. 1321 A 1323Miscellaneous

LA PLAINE DE DYSNA.DVARECKAS V; KUDABA C.1968; LIET. T.S.R. AUKSTUJU MOKYKLU MOKSLO DARB., GEOGR. GEOL.; SUN; 1968, NUM. 0005, P. 63 A 77Miscellaneous

STRUCTURES ET DEPOTS GLACIAIRES DANS L'ORDOVICIEN TERMINAL DES CHAINES D'OUGARTA (SAHARA ALGERIEN).ARBEY F.1968; C.R. ACAD SCI., D; FRA; 1968(1), VOL. 266, NUM. 0002Miscellaneous

STABILITY OF SHEET FLOW OF WATER BENEATH TEMPERATE GLACIERS AND IMPLICATIONS FOR GLACIER SURGINGWALDER JS.1982; J. GLACIOL.; ISSN 0022-1430; GBR; DA. 1982; VOL. 28; NO 99; PP. 273-293; ABS. FRE/GER; BIBL. 2 P.Article

ACCRETION PROCESSES AT THE BASE OF TWO ALPINE GLACIERS AS INDICATED BY THE CHEMICAL COMPOSITION OF THE ICE (EXTENDED ABSTRACT ONLY).LEMMENS M; LORRAIN R; PEETERS G et al.1977; I.A.H.S.-A.I.S.H. PUBL.; U.S.A.; DA. 1977; NO 118; PP. 293; (ISOT. IMPURETES NEIGES GLACES. ACTES COLLOQ.; GRENOBLE; 1975)Conference Paper

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