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Search references for FLYSCH. Phrases containing FLYSCH
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Type of sedimentary rock sequence
Flysch (/flɪʃ/) is a sequence of sedimentary rock layers that progress from deep-water and turbidity flow deposits to shallow-water shales and sandstones
Flysch
Tectonic zone in the Carpathian Mountains
The Carpathian Flysch Belt is an arcuate tectonic zone included in the megastructural elevation of the Carpathians on the external periphery of the mountain
Carpathian_Flysch_Belt
Mountain range in Central and Eastern Europe
orogenic belt is a Tertiary accretionary wedge of a so-called Flysch belt (the Carpathian Flysch Belt) created by rocks scraped off the sea bottom and thrust
Carpathian_Mountains
Geopark in Basque Country
flysch of late Cretaceous to Palaeogene age and hills and mountains characterised by limestone which has given rise to karstic landscapes. The flysch
Basque_Coast_Geopark
Sedimentary rock deposit associated with the formation of mountain chains
The molasse deposits accumulate in a foreland basin, especially on top of flysch-like deposits, for example, those that are left from the rising Alps, or
Molasse
Italy: Geology
the Liguride Units, flysch units with ophiolite were incorporated in the orogenic arc (Cilento Flysch, Flysch Rosso and Frido Flysch). The deformational
Geology_of_Italy
Turbidite (Gorgoglione Flysch), Miocene, South Italy
List_of_rock_types
Mountain range in the Czech Republic
Protected Area. They are built mainly of flysch deposits and their high sediments in both Bečva rivers valleys. The flysch slopes are rather unstable and thus
Hostýn-Vsetín_Mountains
Geological formation in the European Alps
W. (2003): The Middle to Late Jurassic carbonate clastic radiolaritic flysch sediments in the Northern Calcareous Alps: sedimentology, basin evolution
Austroalpine_nappes
Northern Flysch Nappes into the lower Uentschen Nappe and the upper Liechtenstein Flysch. The Southern Flysch Nappe includes the Prattigau Flysch, which
Geology_of_Liechtenstein
Religious mountain in Tibet Autonomous Region
volcanic forms interspersed with Cretaceous and Eocene sediments. The Kailash flysch zone extends about 20 km (12 mi) from the mountain and marks the northern
Mount_Kailash
Microstate in Central Europe
the north, rise from the Rhine Valley and belong to the Helvetic cover or flysch zone of the Alps. Eschnerberg represents an important settlement area in
Liechtenstein
Mountain on the border between Albania and Montenegro
198 ft), with its effusive-carbonate core, gradually descending along the flysch edges towards the Dobku Pass in the south and Gadusë in the north. Maja
Mount_Trojan
Mountain range in Albania
periods, forming belts amid the Paleogene flysch. Ultrabasic rocks are also present, and the older flysch appears in the form of surface bands on the
Skanderbeg_Mountains
Mountain on the Albanian-Greek border
east. The mountain mass consists mainly of paleogene flysch, with smaller amounts of lower flysch and limestone, resulting in a complex tectonic structure
Gramos
Geological formation in the Pennine Alps
and rocks Bündner schist flysch molasse Geological structures Aarmassif Dent Blanche klippe Engadine Line Engadine window Flysch zone Giudicárie line Greywacke
Dent_Blanche_nappe
Foreland basin north of the Alps
north of the developing orogen it formed a small oceanic trench, in which flysch sediments were deposited. The huge amounts of sediments eroded from the
Molasse_basin
Municipality in Basque Country, Spain
set of continuous rock strata in the world. These formations are termed flysch and they date from the mid-cretaceous period to the present, a time period
Zumaia
Geologic formation in New Zealand
The Group is predominantly composed of deep water sandstone and mudstone (flysch). The sandstone dominated units form the cliffs around the Waitemata Harbour
Waitemata_Group
Mountain range in Europe
the crust of Carpathian Flysch Basins caused the formation of the Outer Western Carpathian accretionary wedge (Carpathian Flysch Belt). Vladár, J. (Editor)
Western_Carpathians
Significant mountain range
Alpine Rhine-Danube Flysch can be seen. The Flysch Belt continues through Bohemia, Slovakia, and Poland, and joins the Moldavian Flysch in Ukraine and Romania
Geology of the Western Carpathians
Geology_of_the_Western_Carpathians
Portion of the Alps mountain range within France
Provence-Alpes-Côte d'Azur Borders on Swiss Alps, Italian Alps Geology Orogeny Alpine orogeny Rock age Tertiary Rock types Bündner schist flysch molasse
French_Alps
mountain range is Radziejowa at 1262 metres. The mountains are built from flysch rocks. The Beskid Sądecki links with three other mountain ranges: Jaworzyny
Beskid_Sądecki
Geologic deposit of a turbidity current
Contourite Flysch High-density turbidity currents (Lowe sequence) Sediment gravity flows Tempestite Bouma, Arnold H. (1962) Sedimentology of some Flysch deposits:
Turbidite
Geological formation in the Alps
sedimentary rocks include thin Cretaceous limestones (now marbles) and Tertiary flysch which is now turned into (mica-) schists. rocks from the former Briançonnais
Penninic
Mountain in Albania
vegetation while the lower section, up to 600 m (2,000 ft), consists of flysch. The undulating mountain ridge features a steep eastern slope and a western
Dajti
Summit in Albania
Southern Mountain Region Municipality Skrapar Parent range Tomorr-Kulmak-Miçan Geology Rock age Quaternary Mountain type peak Rock type(s) limestone, flysch
Çuka_Partizani
Type Geological formation Underlies Unconformity Overlies Bozeș Formation, Flysch Lithology Primary Claystone Other Sandstone, Conglomerate Location Region
Sebeș_Formation
Austrian Central Eastern Alps region with exposed Penninic nappes
and rocks Bündner schist flysch molasse Geological structures Aarmassif Dent Blanche klippe Engadine Line Engadine window Flysch zone Giudicárie line Greywacke
Hohe_Tauern_window
are found: the Helvetic nappes, the Penninic nappes (as the Rhenodanubian Flysch Zone) and the Eastern Alps (as the Northern Limestone Alps). North of the
Geology_of_Germany
Earth's highest mountain
be the result of the metamorphism of Middle to Early Cambrian deep sea flysch composed of interbedded, mudstone, shale, clayey sandstone, calcareous sandstone
Mount_Everest
Subducted ocean basin. Remnants found in the Alps in the North Penninic nappes.
Sion-Courmayeur Zone, the Niesen nappe, the Schlieren flysch, the Antrona unit, the Wägital flysch and the Prätigau Bündnerschiefer. Oceans portal Piemont-Liguria
Valais_Ocean
parts of the Alps and the groups at its northern and southern fringes: Flysch zone (up from the Vienna Woods to the Bregenz Forest). Northern Limestone
Geography_of_the_Alps
Geographical composition is varied, with a real "petrographic mosaic". (flysch, crystalline schists, limestones, igneous rocks, metamorphic rocks) From
Western_Romanian_Carpathians
Mountain range in the Northern Limestone Alps
Siplingerkopf. The summits rising to the south consist of flysch. This is the more northerly of the two flysch zones in the Allgäu Alps. The mountains have a more
Allgäu_Alps
Geologic group in Ireland
SE Ireland. The others are: the Bray group (made up of laterally-derived flysch) which is conformably overlain by the Ribband Group; the Duncannon Group
Ribband_Group
Region in Vorarlberg, Austria
belong to a range of the Northern Limestone Alps, specifically the northern flysch zone. It is the drainage basin of the Bregenzer Ach river and has a population
Bregenz_Forest
Summit in Albania
entirely within a flysch-dominated terrain. It occupies a synclinal structure bounded by compressional tectonic faults. Erosion of the flysch formations has
Grebeni
Mountain in Albania
is composed primarily of Cretaceous and Paleogene limestone and less of flysch, forming an anticlinal arch-shaped structure with asymmetrical arms. The
Mali_i_Buretos
Mountain range in Arkansas and Oklahoma, United States
R.J. (1995). "Reinterpretation of Depositional Processes in a Classic Flysch Sequence (Pennsylvanian Jackfork Group), Ouachita Mountains, Arkansas and
Ouachita_Mountains
Mountain in Albania
Eocene limestone, while its lower slopes are largely covered by Oligocene flysch. Morphologically, the mountain represents a folded linear structure, with
Mali_i_Krujës
Major mountain range in Central Europe
thrust faults. As the rising peaks underwent erosion, a layer of marine flysch sediments was deposited in the foreland basin, and the sediments became
Alps
Formation of mountain ranges
fill of many such basins shows a change in time from deepwater marine (flysch-style) through shallow water to continental (molasse-style) sediments. While
Orogeny
the north-easternmost part of the Alps. Geologically, it belongs to the flysch Alps. The main top of the wooded mountain range carries a high observation
Schöpfl
Mountain in Albania
National Park. The mountain is composed mainly of limestone and Paleogene flysch formations. These sedimentary rocks have influenced the development of its
Melesin
Border between the Adriatic and European plates
and rocks Bündner schist flysch molasse Geological structures Aarmassif Dent Blanche klippe Engadine Line Engadine window Flysch zone Giudicárie line Greywacke
Periadriatic_Seam
Mountain in Albania
155 m (7,070 ft). The mountain is composed primarily of limestone with some flysch, creating an anticlinal structure shaped by tectonic forces. The ridge dividing
Mali_i_Lunxhërisë
Mountain group in Torres del Paine, Chile
foothills and dark cap rocks are the sedimentary country rock, in this case flysch deposited in the Cretaceous and later folded. The radiometric age for the
Cordillera_Paine
Mountain in Albania
mountain chain. The mountain is composed primarily of Paleogene limestone and flysch deposits. Structurally, it forms a distinct monoclinal ridge, separated
Mali_i_Postenanit
Mountain range in Western Ukraine
(1,804 m), Lopushna [uk] (1,772 m) and Grofa. The mountains are made of flysch rock, mostly sandstone, which create debris fields (local names: gorgan
Gorgany
Geologic massif in the Swiss Alps
and rocks Bündner schist flysch molasse Geological structures Aarmassif Dent Blanche klippe Engadine Line Engadine window Flysch zone Giudicárie line Greywacke
Aarmassif
Mountain in Albania
its name. Along the sides of the massif, where the limestone meets the flysch, numerous karst springs emerge, contributing to the water supply of the
Mali_me_Gropa
in the Trieste Karst: agriculture was and is limited to small areas of flysch such as near Botazzo, grazing is today almost completely abandoned and even
Rosandra_Valley
Lake in Switzerland
western basin, particularly during periods of high discharge from the steep, flysch-dominated catchment area. This has led to the formation of a substantial
Lake_Lauerz
Italian wine and winemaking region
comune of Cormons. The soil of the region is composed of calcareous marl and flysch sandstone. The 4th largest DOC in the Friuli-Venezia Giulia in terms of
Collio_Goriziano
Prehistoric shallow inland sea in Eurasia
of this ecosystem is known from the Oligocene-aged Menilite Formation, a flysch containing fossils of pelagic and deep-sea fish taxa, as well as microbial
Paratethys
Highest mountain in Vienna, Austria
north-eastern chain of foothills belonging to the eastern Alps. It is composed of flysch containing quartz, limestone, marl, and other conglomerates. The many cliff-like
Hermannskogel
Alemannic dialects spoken in Switzerland
müesli, and rösti have become English words, as did loess (fine grain), flysch (sandstone formation), kepi, landammann, kilch, schiffli, and putsch in
Swiss_German
Riffkalkketten (less 333.7) (to 94 Flysch Alps) 940 Vorarlberg and West Allgäu Flysch Alps (to 941 East Allgäu Flysch Alps) 941.0 Flysch Mountains around the Imberger
Natural_regions_of_Germany
Mountain range in Slovakia
Bukovec Mountains (Slovak: Bukovské vrchy; Hungarian: Ungi-határhegység) is a flysch mountain range in north-eastern Slovakia, part of the Eastern Beskids of
Bukovec_Mountains
Early Ordovician gives way to 200 meters of shale and chert, followed by flysch up to 3.5 kilometers thick and another thick sequence of andesite, basalt
Geology_of_Kazakhstan
and rocks Bündner schist flysch molasse Geological structures Aarmassif Dent Blanche klippe Engadine Line Engadine window Flysch zone Giudicárie line Greywacke
Helvetic_(geology)
history of the region remains poorly understood. Complex assemblages of flysch, ophiolite, mélange and igneous plutons together with thick sedimentary
Geology of Bosnia and Herzegovina
Geology_of_Bosnia_and_Herzegovina
Mountain on the border between Albania and North Macedonia
372 m (7,782 ft) and Kërçinë 2,342 m (7,684 ft). Composed predominantly of flysch and partially of Mesozoic limestone, the massif presents a rugged structure
Deshat
Mountain range in Poland
out in sedimentary rock and its conglomerates which form the Carpathian Flysch Belt. High annual rainfall is caused by the air forced up by the mountains
Gorce_Mountains
Place in Poland
and 1000 m.a.s.l. It is formed from Eocene marlstone slates (Podhalański Flysch). In Poland, the area has a total length of 20 km and a total surface area
Sub-Tatra_Trench
Mountain in Albania
neighboring territory. Kokojka is composed primarily of limestone and Paleogene flysch formations and features two peaks: Kokojka (1,553 m) and the higher Tabori
Kokojka
transitional area. The range consists mainly of limestone and Carpathian flysch. The rock forms a predominantly north–south ridge, from which structured
Piatra_Mare_Mountains
six Protected Biotopes: Inurritza, Leizaran and the abrasion platform (Flysch) in Gipuzkoa; Itxina and Gaztelugatxe in Biscay; and the Laguardia Lagoons
Tourism in the Basque Autonomous Community
Tourism_in_the_Basque_Autonomous_Community
Mountain in Albania
Cretaceous limestone, locally interbedded with effusive volcanic rocks and flysch deposits. Karst landforms are widespread and include sinkholes and other
Rungajë
and rocks Bündner schist flysch molasse Geological structures Aarmassif Dent Blanche klippe Engadine Line Engadine window Flysch zone Giudicárie line Greywacke
Southern_Alps_(Europe)
country's karstic wellsprings belong to Dinaric Alps systems of limestone, flysch, and/or their tectonic contact zone. These are almost regularly large founts
List of karst springs in Bosnia and Herzegovina
List_of_karst_springs_in_Bosnia_and_Herzegovina
and rocks Bündner schist flysch molasse Geological structures Aarmassif Dent Blanche klippe Engadine Line Engadine window Flysch zone Giudicárie line Greywacke
Bündner_schist
Mountain in Albania
the Krastë-Cukal tectonic zone. Composed primarily of Mesozoic limestone, flysch, Paleogene and less of shale and effusive rocks, it has a wrinkled, blocky
Cukal
Volcanic mountain in Iran
mafic volcanic rocks and metamorphic rocks. At Taftan, the Nehbandan-Khash flysch borders the Makran zone. The oldest rocks are limestones from the Cretaceous
Taftan_(volcano)
Mountain range in southeast Asia
The Indo–Burman Range is a sedimentary belt mainly consisted of Cenozoic flysch sediments and a core of Mesozoic ophiolites dated back to late Jurassic
Indo-Burman_Ranges
Mountain in Albania
Cretaceous limestone, forming a prominent anticline, with Paleogene–Neogene flysch deposits appearing along the outer margins. Its western slopes descend abruptly
Mali_i_Konjakut
European regional geology
cover sequence of Upper Cretaceous flysch sediments. a narrow band of flysch in the south. This fairly thick flysch sequence was also deposited in the
Geology_of_the_Pyrenees
Mountain in Albania
primarily of Mesozoic and Paleogene limestones, with lesser amounts of flysch, giving it an asymmetrical anticlinal structure. Its ridge is marked by
Griba
Municipality of Slovenia
expose rocks from Carboniferous shales (c. 300 Ma) through Paleocene–Eocene flysch (35–65 Ma) within a compact area. Noteworthy geoheritage features include
Municipality_of_Idrija
Massif in Albania
and dolomite, the mountain has an anticlinal structure, with a band of flysch emerging in the north and south. It forms a sharp ridge between the northeastern
Shkëlzen
Wine made in the northeastern Italian region of Friuli-Venezia Giulia
September. The soils of the region vary from the calcium rich marl and flysch sandstone in the more hilly regions to clay, sand and gravel in the valley
Friuli-Venezia_Giulia_wine
Summit in Albania
Region Municipality Tepelenë Parent range Kurvelesh Highlands Geology Rock age(s) Mesozoic, Paleogene Mountain type summit Rock type(s) limestone, flysch
Këndrevica
Mountain region in Albania, Kosovo and Montenegro
rocks like Paleozoic shale and volcanic rocks from Cretaceous-Paleogene flysch. Their physical structure is shaped by recent tectonic movements, forming
Albanian_Alps
Mountain range in the Balkan Peninsula of Southeastern Europe
October 2018). "A diverse deep-sea trace fossil assemblage from the Adriatic Flysch Formation (middle Eocene – middle Miocene), Montenegro (central Mediterranean)"
Dinaric_Alps
Mountain range in Slovakia
Beskids of the Outer Eastern Carpathians. The range is composed of Carpathian flysch. Bordered in the north by the Polish national border and to the west by
Laborec_Highlands
state, where accommodation space is created as fast as it is filled with flysch, to an overfilled one (stage 3). The orogenic wedge then provides a significant
Windermere_Supergroup
Piece of continental crust in the Penninic nappes of the Alps
and rocks Bündner schist flysch molasse Geological structures Aarmassif Dent Blanche klippe Engadine Line Engadine window Flysch zone Giudicárie line Greywacke
Briançonnais_zone
Geologic formation in Italy
basins. The San Cassiano Formation overlays the Wengen Formation (a volcanic flysch sequence); the limit between this two formations is arbitrary; usually considered
San_Cassiano_Formation
National park in Greece
also occurs, and on the northwestern slopes, between 600 and 1,200 metres, flysch dating from the Eocene is found. The dominant presence of limestone has
Olympus_National_Park
Valley in Italy
environments: the upper Tiber basin, composed mainly of terrigenous sediment in flysch facies of Tuscan origin (on the right bank north of Lake Trasimeno) and
Tiber_Valley
Place in Slovenian Littoral, Slovenia
altitude of 70 meters above sea. Its tip on the west end is characterised by flysch cliffs raging from 12 to 21 metres in height, and below them a narrow abrasion
Debeli_Rtič
described in 1948 as the Old Montenegro Overthrust and includes Anisian age flysch and limestone, thin Ladinian volcano-sedimentary rock, Late Triassic carbonates
Geology_of_Montenegro
Mountain chain in Albania
orientation and is composed primarily of limestone, with a smaller presence of flysch, forming an asymmetrical anticlinal structure. The western slope is more
Dhëmbel
Mountain on the Italy-France border in the Alpi Cozie
from the Middle Triassic, resting on a base of fractured marbles and black flysch. The rock is notably friable; alpinistic activity therefore preferentially
Monte_Oronaye
north-eastern chain of foothills belonging to the eastern Alps. It is composed of flysch containing quartz, limestone, marl, and other conglomerates. The name Meiselberg
Meiselberg
foothills and dark cap rocks are the sedimentary country rock, in this case flysch deposited in the Cretaceous and later folded. The radiometric age for the
Cerro_Catedral_(Chile)
Slovakia, rugged highlands along the Myjava River composed of Carpathian flysch. Geologically it is one range of the Slovak-Moravian Carpathians of the
Myjava_Hills
Point-counting technique used in geology
classification Gazzi, P., 1966, "Le Arenarie del Flysch Sopracretaceo dell'Appennino Modenese: Correlazioni con il Flysch di Monghidoro". Mineralogica e Petrografica
Gazzi-Dickinson_method
Sedimentary basin in France
developed into which flysch sediments (and partially also wildflysch breccias) from the Pyrenean realm were shed. Near Saint-Gaudens, the flysch sediments are
Aquitaine_Basin
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