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Deposits of dark, fine-grained, thinly bedded sandstone shales and of clay, thought to be deposited by turbidity currents and originally defined as rock formations on the northern and southern borders of the Alps.



a thick sequence of marine sedimentary rocks, primarily detrital in origin, characterized by a cyclic alternation of several lithologic varieties of graded beds with finer grains toward the top, regardless of mineralogical composition. Flysch consists of many thin cycles that are only several centimeters to several decimeters deep (Figure 1). The cycles are also called cyclothems, cyclosomes, or multiple beds and are sometimes inaccurately referred to as rhythms.

Figure 1. A flysch cycle, or multiple bed: (I) aleurolite, (II) light marl with dark fucoid patches, (III) dark clays. The base of a new cycle, or multiple bed, is in the upper part of the figure.

The cycles are formed by two to four beds. The underlying beds consist of granulites, such as sandstone, aleurolite, and cal-carenite, and often display cross-bedded and irregular sediments; the overlying beds are composed of pelites. Hieroglyphs of various shapes and origins are typical on the lower surface of the cycles. Some of the hieroglyphs are the impressions of irregularities on the floor of the body of water; the irregularities resulted from the erosional action of short-lived turbidity currents and from the vital activity of various animals, mostly worms, that crawled along the bottom. Fucoids, which resemble algae in shape and are at least as characteristic of flysch as are hieroglyphs, owe their origin to worms.

The cyclic nature of flysch is caused by specific features of the accumulation of sediment, that is, by more or less periodic turbidity currents.

Flysch is a typical geosynclinal formation that marks the pre-orogenic phase of the development of eugeosynclines, miogeo-synclines, or both. In the preorogenic phase, a cordillera emerged along a flysch trough. A cordillera is a long chain of islands on the slope of which wildflysch and coarse-grained wildflysch formed. Wildflysch is associated with submarine landslide formations, and coarse-grained wildflysch is enriched with conglomerates and sandstone. Away from the source, the wildflysch is typically replaced by flysch, which in turn is replaced by immature flysch and semiflysch, or subflysch (Figure 2). In a vertical sequence of geologic formations, flysch occupies an intermediate position between slate formation and molasses. In folded regions that arose at the sites of geosynclines, strongly dislocated flysch deposits constitute the outer part, or the externides.

Figure 2. Flysch in a sequence of adjacent formations

Flysch has been identified in the Proterozoic, Paleozoic, Mesozoic, and Cenozoic. The Paleozoic deposits are represented by Carboniferous flysch in the Urals. The Mesozoic deposits include Triassic flysch in the Crimea and Jurassic and Cretaceous flysch in the Caucasus and the Alps. Cenozoic flysch is found in the Carpathians.

Deposits of petroleum and mineral water are correlated in time with flysch. Carbonate flysch and subflysch are sometimes good raw materials for cement. Such flysches are found, for example, in the Novorossiisk region.


Vassoevich, N. B. Flish i metodika ego izucheniia. Leningrad-Moscow, 1948.
Vassoevich, N. B. Usloviia obrazovaniia flisha. Leningrad-Moscow, 1951.
Khvorova, I. V. Flishevaia i nizhnemolassovaia formatsiia Iuzhnogo Urala. Moscow, 1961.
Bouma, A. H. Sedimentology of Some Flysch Deposits. Amsterdam, 1962.


References in periodicals archive ?
Surface covered by each geolithological type was obtained using geolithological map from the Geoportale Nazionale (2016), with the types abbreviated as follows: limestones, dolomites, marls, travertines, and glacial deposits (LIT_LIM), alluvial sediments and clays (LIT ALL), volcanic rocks (LIT VOL), arenaceous assemblages and flysch deposits (LIT ARE), sands, conglomerates, and aeolian deposits (LIT SAN), lakes and glaciers (LIT LAK), and gypsum and evaporite deposits (LIT EVA).
2004, Analysis of the stability of slopes, located in the Carpathian flysch.
The main aim of this paper is to describe changes in the durability and geotechnical characteristics of siltstones from flysch rock masses in the Istria Peninsula, Croatia, due to weathering processes.
From north to south, Tibet consists of the Kunlun-Qaidam and Songpan-Ganzi flysch complex, and the Qiangtang and Lhasa terranes, which are separated by the Anyimaqen-Kunlun-Muztagh, Hoh Xil-Jinsha River and Bangong Lake-Nujiang River suture zones, respectively (Fig.
Eocene flysch facies in the study area, set in the South East of Iran, the zone name Zabul - Baluch, Sistan Suture zone and or zone Nehbandan - Kash is Rock units in the study area includes a colorful melange , flysch of Cretaceous, Paleocene and Eocene flysch of the ultrabasic parts, materials, volcanic and clastic rocks are Neogene [1].
The geological substrate in the wider area of Mount Vermio consists mainly of flysch or schist, supporting Quercus frainetto forests; at lower altitudes and in drier and/or more disturbed areas, these forests are replaced by Quercus pubescens and Carpinus orientalis (Tsiripidis et al.
In western part, in Albanian territory the geopark area is covered by Triassic limestone with some rare small outcrops of Upper Cretaceous limestone, flysch and molasses in form of separate stains on surface of Triassic limestone (Serjani, 2009).
VrSka, "Role of position within the windthrow in forest floor chemistry in the flysch zone of the Carpathians," Canadian Journal of Forest Research, vol.
Kryma (Syntaxonomic structure of the vegetation of flysch ranges of the south-eastern Crimea)--Sborn.
Himalayan Bengal model for flysch dispersal in the Appalachian Ouachita system.
The flysch series having mixed volcanic material composed of conglomerate, green and black sandstone, shale, marl, limestone, andesite, tuff and tuffite are deposited in the Upper Cretaceous limestone.