FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2100916801> ?p ?o ?g. }

• W2100916801 endingPage "2299" @default.
• W2100916801 startingPage "2279" @default.
• W2100916801 abstract "Abstract. The Alpine Fault in New Zealand's South Island has not sustained a large magnitude earthquake since ca. AD 1717. The time since this rupture is close to the average inferred recurrence interval of the fault (~300 yr). The Alpine Fault is therefore expected to generate a large magnitude earthquake in the near future. Previous ruptures of this fault are inferred to have generated Mw = 8.0 or greater earthquakes and to have resulted in, amongst other geomorphic hazards, large-scale landslides and landslide dams throughout the Southern Alps. There is currently 85% probability that the Alpine Fault will cause a Mw = 8.0+ earthquake within the next 100 yr. While the seismic hazard is fairly well understood, that of the consequential geomorphic activity is less well studied, and these consequences are explored herein. They are expected to include landsliding, landslide damming, dam-break flooding, debris flows, river aggradation, liquefaction, and landslide-generated lake/fiord tsunami. Using evidence from previous events within New Zealand as well as analogous international examples, we develop first-order estimates of the likely magnitude and possible locations of the geomorphic effects associated with earthquakes. Landsliding is expected to affect an area > 30 000 km2 and involve > 1billion m3 of material. Some tens of landslide dams are expected to occur in narrow, steep-sided gorges in the affected region. Debris flows will be generated in the first long-duration rainfall after the earthquake and will continue to occur for several years as rainfall (re)mobilises landslide material. In total more than 1000 debris flows are likely to be generated at some time after the earthquake. Aggradation of up to 3 m will cover an area > 125 km2 and is likely to occur on many West Coast alluvial fans and floodplains. The impact of these effects will be felt across the entire South Island and is likely to continue for several decades." @default.
• W2100916801 created "2016-06-24" @default.
• W2100916801 creator A5014558631 @default.
• W2100916801 creator A5053245975 @default.
• W2100916801 date "2013-09-23" @default.
• W2100916801 modified "2023-09-30" @default.
• W2100916801 title "Review Article: Potential geomorphic consequences of a future great (&lt;i&gt;M&lt;/i&gt;&lt;sub&gt;w&lt;/sub&gt; = 8.0+) Alpine Fault earthquake, South Island, New Zealand" @default.
• W2100916801 cites W101505841 @default.
• W2100916801 cites W1589061952 @default.
• W2100916801 cites W1590834344 @default.
• W2100916801 cites W1670416866 @default.
• W2100916801 cites W1963876943 @default.
• W2100916801 cites W1969127085 @default.
• W2100916801 cites W1970574080 @default.
• W2100916801 cites W1971175518 @default.
• W2100916801 cites W1972597182 @default.
• W2100916801 cites W1975896034 @default.
• W2100916801 cites W1977180247 @default.
• W2100916801 cites W1979658879 @default.
• W2100916801 cites W1982538836 @default.
• W2100916801 cites W1982899902 @default.
• W2100916801 cites W1984272292 @default.
• W2100916801 cites W1988158662 @default.
• W2100916801 cites W1988342284 @default.
• W2100916801 cites W1990138297 @default.
• W2100916801 cites W1990844281 @default.
• W2100916801 cites W1994784358 @default.
• W2100916801 cites W1999287311 @default.
• W2100916801 cites W1999304749 @default.
• W2100916801 cites W2000300037 @default.
• W2100916801 cites W2006463062 @default.
• W2100916801 cites W2008832455 @default.
• W2100916801 cites W2010046639 @default.
• W2100916801 cites W2015652987 @default.
• W2100916801 cites W2019499646 @default.
• W2100916801 cites W2020287411 @default.
• W2100916801 cites W2021022235 @default.
• W2100916801 cites W2022753823 @default.
• W2100916801 cites W2023434032 @default.
• W2100916801 cites W2023707808 @default.
• W2100916801 cites W2026911033 @default.
• W2100916801 cites W2027029024 @default.
• W2100916801 cites W2027459844 @default.
• W2100916801 cites W2030201095 @default.
• W2100916801 cites W2030389398 @default.
• W2100916801 cites W2034360407 @default.
• W2100916801 cites W2034755071 @default.
• W2100916801 cites W2036183794 @default.
• W2100916801 cites W2036404469 @default.
• W2100916801 cites W2039510518 @default.
• W2100916801 cites W2042826870 @default.
• W2100916801 cites W2047465867 @default.
• W2100916801 cites W2048870428 @default.
• W2100916801 cites W2051696361 @default.
• W2100916801 cites W2058079476 @default.
• W2100916801 cites W2060378572 @default.
• W2100916801 cites W2060382151 @default.
• W2100916801 cites W2066402172 @default.
• W2100916801 cites W2067161726 @default.
• W2100916801 cites W2067371720 @default.
• W2100916801 cites W2070602091 @default.
• W2100916801 cites W2072804171 @default.
• W2100916801 cites W2078780733 @default.
• W2100916801 cites W2079928247 @default.
• W2100916801 cites W2080540100 @default.
• W2100916801 cites W2080657965 @default.
• W2100916801 cites W2081160872 @default.
• W2100916801 cites W2085419512 @default.
• W2100916801 cites W2086282120 @default.
• W2100916801 cites W2098681477 @default.
• W2100916801 cites W2110879957 @default.
• W2100916801 cites W2121188386 @default.
• W2100916801 cites W2124278013 @default.
• W2100916801 cites W2129419327 @default.
• W2100916801 cites W2130833734 @default.
• W2100916801 cites W2139435483 @default.
• W2100916801 cites W2141424304 @default.
• W2100916801 cites W2144405045 @default.
• W2100916801 cites W2147663465 @default.
• W2100916801 cites W2152325549 @default.
• W2100916801 cites W2156976082 @default.
• W2100916801 cites W2158115012 @default.
• W2100916801 cites W2167866074 @default.
• W2100916801 cites W2170188862 @default.
• W2100916801 cites W2210476293 @default.
• W2100916801 cites W2233328806 @default.
• W2100916801 cites W2241748382 @default.
• W2100916801 cites W2313049760 @default.
• W2100916801 cites W2394675756 @default.
• W2100916801 cites W2525516836 @default.
• W2100916801 cites W2525546086 @default.
• W2100916801 cites W3047479297 @default.
• W2100916801 cites W4247502213 @default.
• W2100916801 cites W80055876 @default.
• W2100916801 doi "https://doi.org/10.5194/nhess-13-2279-2013" @default.
• W2100916801 hasPublicationYear "2013" @default.
• W2100916801 type Work @default.
• W2100916801 sameAs 2100916801 @default.

• next