Topographic map with location of ECRIS rift basins: LG=Limagne Graben, BG=Bresse Graben, URG=Upper Rhine Graben, LRG=Lower Rhine Graben, HG=Hessian Grabens & EG=Eger Graben, and Jura mountains with frontal thin-skinned thrust shown
The European Cenozoic Rift System (ECRIS) is a 1,100 km (680 mi) long system of rifts formed in the foreland of the Alps as the lithosphere responded to the effects of the Alpine and Pyrenean orogenies. The system began to form during the Late Eocene and parts (particularly the Upper and Lower Rhine Grabens) remain seismically active today and are responsible for most of the larger earthquakes in Europe, north of the Alps.
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France–Germany border. It forms part of the EuropeanCenozoicRiftSystem, which extends across Central Europe. The Upper Rhine Graben formed during the...
western Germany, known as the Upper Rhine valley, part of the EuropeanCenozoicRiftSystem The Taupō Volcanic Zone in the north east North Island of New...
of Pangea. When Pangea broke up, Avalonia's remains were divided by the rift which became the Atlantic Ocean. When the term "Avalon" was first coined...
graben structure that formed during the Eocene as part of the EuropeanCenozoicRiftSystem. It forms the Limagne plain in the Massif Central and is filled...
Scientists know less about ocean ridges than they do the planets of the solar system. There is another triple junction where the Eurasian Plate meets the Anatolian...
London-Brabant Massif. The Lower Rhine Graben, part of the EuropeanCenozoicRiftSystem, which has been tectonically active since the Oligocene, affects...
(January 1982). "Western extension of the Iberian-European plate-boundary during early Cenozoic (Pyrenean) convergence: a new model". Marine Geology...
between the African Plate and the Eurasian Plate. The platform is crossed by a rift zone formed of three grabens: the Pantelleria graben, that of Malta, and...
Atlantic Ocean. The Hercynian fold belt is mostly buried by Mesozoic and Cenozoic cover rocks to the east but nevertheless outcrops through the Iberian Chain...
Tasmania, Australia Guanabara Graben, Rio de Janeiro, Brazil EuropeanCenozoicRiftSystem Fossa (geology) – Long, narrow, shallow depressionPages displaying...
Dnieper-Donets Rift, transects Sarmatia, dividing it into the Ukrainian Shield and the Voronezh Massif. The southwestern boundary is known as the Trans European Suture...
scientists believe the hotspot beneath Iceland could have contributed to the rifting of the supercontinent Pangaea and the subsequent formation of the North...
discuss] is an orogenic phase in the Late Mesozoic (Eoalpine) and the current Cenozoic that has formed the mountain ranges of the Alpide belt. The Alpine orogeny...
Eger Graben is part of the EuropeanCenozoicRiftSystem and was created geologically on the same principle as the Rhine Rift Valley. It was formed by the...
present position, overriding the Helvetic and Penninic domains. EuropeanCenozoicRiftSystem Geography of Germany Geology of the Alps Germanic Trias Laacher...
sedimentary deposits ranging from Jurassic to Cenozoic in age. There are two major north–south trending rift structures of Triassic age buried beneath the...
The Alps form part of a Cenozoic orogenic belt of mountain chains, called the Alpide belt, that stretches through southern Europe and Asia from the Atlantic...
depression originated as a series of interconnected rifts that were not active enough to split the East European Craton. Subsidence in the southern parts was...
the southeast of the Netherlands are caused by active rifts of the EuropeanCenozoicRiftSystem. The 1992 Roermond earthquake in the southeastern province...
complex process of rotation and extension of variable magnitude during the Cenozoic era. The northward push of the Adriatic Block initiated the eastward displacement...
Tectonic Framework of Europe. Geological Survey of Finland. ISBN 9516909213. Retrieved 31 August 2015. "Landscapes for living!". European Landscapes. Geological...
Middle Paleozoic the riftsystem was reactivated resulting in intrusion of alkaline magmas. In the Late Cenozoic the riftsystem was reactivated again...
Irish Sea. A basin developed in the Hampshire region around this time. Rifting occurred within and around Great Britain, prior to the breakup of the super-continent...
This list covers all faults and fault-systems that are either geologically important[clarification needed] or connected to prominent seismic activity...
in the Leipzig plain. Germany is transected by parts of the EuropeanCenozoicRiftSystem, particularly the Upper and Lower Rhine Grabens, and these areas...
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