Anagram & Information om | Engelska ordet GRABENS

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• Fecunditatis basin meets Nectaris basin along Fecunditatis' western edge, with the area along this zone faulted by arcuated grabens.
• In geology, horst and graben (or range and valley) refers to topography consisting of alternating raised and lowered fault blocks known as horsts and grabens.
• The Davis Strait is underlain by complex geological features of buried grabens (basins) and ridges, formed by strike-slip faulting of the Ungava Fault Zone during Paleogene times about 45 million to 62 million years ago.
• On the other hand, north–south extensional movements, yet unexplained, are pulling the plate apart, creating normal extensional faults and generating a parallel sequence of horsts and grabens, or rift valleys, running in a north–south direction.
• The northern flanks of the volcano are highly faulted with grabens and normal faults concentric to the volcano's summit caldera.
• The outer rim of the crater consists of remnants of semi-circular grabens in highly deformed Permo-Carboniferous sediments.
• The Ohrid and Prespa Lakes are the two largest in a north–south chain of tectonic basins (grabens) including the Korçë basin, and Lake Ioannina in North West of Greece, known as the Dessaret group.
• Maat Mons is surrounded by a radial dike swarm, with grabens extending over 1,500 kilometres from the volcano's centre.
• However, other crater chains, such as many of those on Mars, represent chains of collapse pits associated with grabens (see, for example, the Tithoniae Catenae near Tithonium Chasma).
• Tectonics explains the large-scale structure of the Earth's crust and its constituent rocks in terms of blocks moving along faults, uplifted into horsts or downthrown into grabens.
• Volcanoes within the Northern Cordilleran Volcanic Province are located along short northerly trending segments which in the northern part of the volcanic province are unmistakenably involved with north-trending rift structures, including synvolcanic grabens and grabens with one major fault line along only one of the boundaries (half-grabens).
• The landslide morphology comprises horsts and grabens typical of spreads and also a large quantity of remolded material that flowed out of a pear-shaped crater with a narrow bottleneck, typical of flowslides.
• Large listric regional faults dipping towards the ocean develop with rollover anticlines and related crestal collapse grabens.
• The northern part of the plate is currently a region of crustal extension caused by slab rollback on the Hellenic Subduction Zone to the south, causing extensive normal faulting and the formation of horsts and grabens on the seafloor.
• The basin is floored by a northwest-southeast-trending mosaic of narrow horsts and grabens, an important structural characteristic that distinguishes it from the adjacent intracratonic Kufra, Murzuk, and Ghadames basins.
• This second set of earth movements, known as the Kaikoura Orogeny, elevated large fault-bounded blocks to form the horsts (upfaulted blocks of land) of the Hunua and Coromandel Ranges, and threw down the grabens (down-faulted blocks) of the Firth of Thames and Hauraki Gulf which Omana now overlooks.
• This broad, multistate zone of intraplate seismicity lay just to the north of the New Madrid Seismic Zone and comprises both strike-slip and dip-slip earthquake mechanisms across numerous named faults, grabens, and anticlines.
• The Matzen fault system in the Matzen oil field has been recast as extensional grabens produced by pull-apart basins of the Vienna Basin.
• The Saxothuringian Zone is in some places transected by Permo-Triassic grabens and intramontane basins filled with Rotliegend sediments and older deposits.
• The Northern Cordilleran volcanoes of northwestern British Columbia are disposed along short, northerly trending segments which are unmistakably involved with north-trending rift structures including synvolcanic grabens and grabens with one major fault line along only one of the boundaries (half-grabens) similar to those associated with the East African Rift, which extends from the Afar Triple Junction southward across eastern Africa.

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