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deposits. As the basin fills up, shallow-water sandstones and continental deposits form. Most of the resulting rocks have little deformation, but near the edge of the mountain chain they can be subject to folding and thrusting. After the basin fills up, continental sediments
184:, then sea water may rush in, and the first sedimentary deposits are deep water deposits. If the mountain slope is steep enough at the edge of the basin, it will shed material in rapidly moving sedimentary flows called
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form, and a mountain chain rises. On the upper plate, the land between the mountains and the undeformed continent bends downward, forming a
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in 1827. Studer used the term for the typical alternations of sandstone and shale in the foreland of the Alps. The name comes from the
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The name flysch is currently used in many mountain chains belonging to the Alpine belt. Well-known flysch deposits are found in the
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132:. Flysch typically consists of a sequence of shales rhythmically interbedded with thin, hard,
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290:"Urola Kosta: Things to do in Orio, Zarautz, Getaria and Zumaia | Bodega Katxiña"
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445:. Vol. 10 (11th ed.). Cambridge University Press. p. 586.
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at the bottom of each cycle, which gradually evolve upwards into
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404:] (in German) (7th ed.). Bern: Ott Verlag. p. 64.
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Sedimentary Basins : Evolution, Facies, and
Sediment Budget
310:"La ruta del Flysch, un viaje distinto al País Vasco - Vipealo"
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The name flysch was introduced in geologic literature by the
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tectonic plate pushes on the plate above it, making the rock
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Flysch consists of repeated sedimentary cycles with upwards
339:(3rd print ed.). New York: Freeman. pp. 265–266.
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136:-like sandstones. Typically the shales do not contain many
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27:Type of sedimentary rock sequence
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241:setting came only much later.
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450:Stanley, Steven M. (2005).
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80:deposits to shallow-water
396:Labhart, Toni P. (2005).
363:Einsele, Gerhard (2000).
237:typical for a particular
182:North American Cordillera
90:North American Cordillera
312:(in Spanish). 2020-12-11
442:Encyclopædia Britannica
42:, Basque Country, Spain
402:Geology of Switzerland
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158:continental collision
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452:Earth System History
398:Geologie der Schweiz
72:) is a sequence of
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186:turbidity currents
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480:Sedimentary rocks
209:Carpathian flysch
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314:. Retrieved
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293:. Retrieved
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201:Name and use
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254:Carpathians
102:Carpathians
474:Categories
346:0716724375
316:2023-07-03
295:2023-07-03
276:References
217:geologist
162:subducting
146:glauconite
86:sandstones
337:Tectonics
246:forelands
190:turbidite
152:Tectonics
134:graywacke
126:sandstone
18:Flyschoid
250:Pyrenees
227:fliessen
122:breccias
100:and the
98:Pyrenees
264:and on
262:Balkans
248:of the
231:to flow
195:molasse
138:fossils
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375:–211.
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272:unit.
266:Cyprus
260:, the
223:German
114:fining
96:, the
92:, the
82:shales
47:Flysch
40:Zumaia
400:[
258:Italy
225:word
215:Swiss
156:In a
142:micas
38:, at
456:ISBN
406:ISBN
377:ISBN
341:ISBN
252:and
166:fold
160:, a
144:and
128:and
94:Alps
84:and
373:210
120:or
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