On bed-slope vs wavelength and height of aeolian ripples and coefficient of friction in aeolian sands = La longueur d'onde et la hauteur des rides éoliennes de versants de dunes ainsi que le coefficient de friction des sables éoliensASOKKUMAR BHATTACHARYA.Current science (Bangalore). 1990, Vol 59, Num 15, pp 740-741, issn 0011-3891, 2 p.Article

Wellen-PhänomeneSTOBER, Ingrid.Beiträge zur Hydrologie. 1991, Vol 12, Num 1, pp 59-69, issn 0343-0987Conference Paper

Subordinate current reactivation surfaces and the recognition of tidal deposits = Surfaces de réactivation de courants subordonnés et la reconnaissance des dépôts de maréeDE MOWBRAY, T; VISSER, M.International association of sedimentologists. European regional meeting. 3. 1982, pp 52-54Conference Paper

Eolian systems = Systèmes éoliensTerrigenous Clastic Depositional Systems. 1983, pp 203-221Book Chapter

Flush marking: a feature related to the biogenic activity of Loimia medusa (Savigny) = Traces de bioturbation: caractéristique relative à l'activité biogénique de Loimia medusa (Savigny)DAS, S; CHAKRABARTI, A.Indian journal of earth sciences. 1984, Vol 11, Num 2, pp 166-168, issn 0379-5128Article

Superposition of aeolian dust ripple patterns as a result of changing wind directionsGOOSSENS, D.Earth surface processes and landforms. 1991, Vol 16, Num 8, pp 689-699, issn 0197-9337Article

The occurrence and formation of ladderback ripples in subtidal, shallow-marine sands, Zululand, South Africa = Occurrence et formation des ripples de type «ladderback» dans des sables subtidaux, Zoulouland, Afrique du SudRAMSAY, P. J; COOPER, J. A. G; WRIGHT, C. I et al.Marine geology. 1989, Vol 86, Num 2-3, pp 229-235, issn 0025-3227Article

Vysledky sedimentologického vyzkumu karpatu pod flysovymi prikrovy ve stredni casti karpatské predhlubne na Morave = Results of sedimentological research of Karpathian beneath Flysch nappes in central part of Carpathian Foredeep in MoraviaKRYSTEK, I.Geologické práce. 1989, Num 88, pp 59-70, issn 0433-4795Article

Study of sand microforms in the nearshore zone = Etude des microformes sableuses de la zone littoraleKOS'YAN, R. D.Marine geology. 1988, Vol 83, Num 1-4, pp 63-78, issn 0025-3227Article

Bedform length and velocity pulsations in alluvial channels = Longueur des structures sédimentaires et pulsations de la vitesse d'écoulement dans des chenaux alluviauxKHALID MAHMOOD; HAQUE, M. I.Journal of waterway, port, coastal, and ocean engineering. 1988, Vol 114, Num 3, pp 315-330, issn 0733-950XArticle

On geomorphic patterns with a focus on stone circles viewed as a free-convection phenomenon = Les figures géomorphologiques en insistant sur les cercles de pierres vus comme un phénomène de convection libreHALLET, B.NATO advanced Study Institute on irreversible phenomena and dynamical systems analysis in geosciences. 1987, pp 533-553Conference Paper

Rotación de lineaciones por ordenador. Aplicación a ripples paleozoicos de Sierra Demanda = Rotation de linéations par ordinateur. Application aux ripples paléozoïques de la Sierra DemandaMARTIN ESCORZA, C.1986, Num 19, pp 36-40, issn 0212-5404Article

Recent ripple marks at Giorgimpopoli, Libya = Ripple marks récents à Giorgimpopoli, LibyeWULF, G.R.Journal of sedimentary petrology. 1964, Vol 33, Num 4, pp 964-965, issn 0022-4472, 2 p.Article

Current directions in the USRI river point bar, Bihar = Direction des courants dans le bourrelet arqué de la Rivière Usri, BiharBARENDRA PURKAIT.Indian journal of earth sciences. 1983, Vol 10, Num 2, pp 170-184, issn 0379-5128Article

The internal structure of ridges, runnels and berms as a result of the interaction of waves and tides on the Foreshore = La structure interne des crêtes, rigoles et bermes: résultats de l'interaction des vagues et des marées sur l'avant côteDABRIO, C. J.International Association of Sedimentology. European regional meeting. 3. 1982, pp 8-9Conference Paper

LONGITUDINAL RIDGES WITH TUNING-FORK JUNCTURES IN THE LAMINATED INTERVAL OF FLYSCH BEDS: EVIDENCE FOR LOW-ORDER HELICOIDAL FLOW IN TURBIDITES.FOLK RL.1977; SEDIMENT. GEOL.; NETHERL.; DA. 1977; VOL. 19; NO 1; PP. 1-6; BIBL. 14 REF.; 4 ILL.Article

OSCILLATORY RIPPLE MARKS AND THE EVALUATION OF ANCIENT WAVE CONDITIONS AND ENVIRONMENTS.KOMAR PD.1974; J. SEDIMENT. PETROL.; USA; 1974, VOL. 44, NUM. 0001, P. 169 A 180Serial Issue

SUR LA STRUCTURE DES SEDIMENTS D'UN DELTA A CRETES.AARIO R.1972; GEOLOGI; FIN; 1972, VOL. 24, NUM. 0002, P. 13 A 17Miscellaneous

INTERFERENCE RIPPLE MARKS FORMED BY EPHEMERAL STREAMSPICARD MD; HIGH LR JR.1970; PROC. UTAH ACAD. SCI. ARTS LETTERS; U.S.A. ; 1970, VOL. 47, NUM. 0002, P. 116Serial Issue

RIPPELN MIT,"VERKEHRTEM" GERFUEGE.(RIPPLES AVEC STRUCTURES "RENVERSEES").WUNDERLICH F.1968; NATUR.U.MUSEUM-DTSCH.; 1968(5), VOL. 98, NUM. 0005, P. 279 A 281Miscellaneous

WERDEN MARKEN IMMER ENTSPRECHEND DER HAEUFIGKEIT IHRES AUFTRETENS FOSSIL.(EST-CE QUE LES TRACES SE FOSSILISENT TOUJOURS EN FONCTION DE LA FREQUENCE DE LEUR APPARITION).WUNDERLICH F.1968; NAT.U.MUS.-DTSCH.; 1968(2), VOL. 98, NUM. 0002, P. 57 A 63Miscellaneous

CURRENT RIPPLES THEIR RELATION TO PATTERNS OF WATER AND SEDIMENT MOTION.ALLEN JRL.1968; NORTH.HOLLAND.PUBLISHING.COMPANY.AMSTERDAM.; 1968, P. 1 A 433Miscellaneous

RIPPLE GROWTH ON FLAT BEDS OF FINE SAND.(ABSTRACT).DINGLER JR; SOUTHARD JB.1968; GEOL. SOC. AMER., ABSTR. PROGRAMS; USA; 1968(11)Miscellaneous

RIPPLE MARK INDICES AND THEIR USES.TANNER WF.1967; SEDIMENTOLOGY; NLD; 1967(9), VOL. 9, NUM. 0002, P. 89 A 104Miscellaneous

CHARACTERISTICS OF OSCILLATORY FLOWS IN RELATION TO RIPPLE TYPES ON OFFSHORE SEA BOTTOM = LES CARACTERES DES FLUX OSCILLATOIRES EN RELATION AVEC LES TYPES DE RIPPLE SUR LE FOND DE LA MER AU LARGE DE LA COTEMATSUMOTO E; TAKEDA I.1978; ANNU. REP. INST. GEOSCI., UNIV. TSUKUBA; JPN; DA. 1978 PUBL. 1979; NO 5; PP. 39-42; BIBL. 4 REF.; ILL.Article