Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Colin Mazengarb"'
Publikováno v:
Pure and Applied Geophysics. 177:1549-1568
The east coast of Tasmania is directly exposed to tsunamis originating from the Puysegur subduction zone, off New Zealand’s southwest coast. However, the potential impacts of tsunami inundation for coastal communities and Hobart Airport, and risks
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::858000a49ef343a0f53cb63e83492eed
https://doi.org/10.1007/s00024-019-02384-0
https://doi.org/10.1007/s00024-019-02384-0
Publikováno v:
Sedimentary Geology. 364:286-301
Two episodes of intense flooding and sediment movement occurred in the Westmorland Stream alluvial system near Caveside, Australia in January 2011 and June 2016. The events were investigated in order to better understand the drivers and functioning o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6562c1fbb94091980e57ad1c720c5f12
https://doi.org/10.1016/j.sedgeo.2017.10.005
https://doi.org/10.1016/j.sedgeo.2017.10.005
Publikováno v:
The Holocene. 21:883-895
Stratigraphic investigations of three coastal waterbodies in southeastern Tasmania reveal major paleoenvironmental phases related to sea level change and anomalous deposits consistent with tsunami inundation. Twenty-two short sediment cores were exam
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::523d387cde82212a8977dc0ef535600b
https://doi.org/10.1177/0959683610391317
https://doi.org/10.1177/0959683610391317
Autor:
Colin Mazengarb, Kate Wilson, Michael Marden, Alan Palmer, Kelvin Berryman, Nicola Litchfield
Publikováno v:
Marine Geology. 270:55-71
Determining the spatial and temporal deliveries of sediment from the Waipaoa River catchment in the post-glacial period is a major goal of integrated source-to-sink landscape evolution studies in the region. In a 2.2 km long section of the Waihuka tr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c1dd46df815a5b3e964e7d18427f5b12
https://doi.org/10.1016/j.margeo.2009.10.001
https://doi.org/10.1016/j.margeo.2009.10.001
Publikováno v:
Geomorphology. 99:404-419
The sediment flux generated by postglacial channel incision has been calculated for the 2150 km 2 , non-glacial, Waipaoa catchment located on the tectonically active Hikurangi Margin, eastern North Island, New Zealand. Sediment production both at a s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fbcbba3cf34ea67e74f169f110044306
https://doi.org/10.1016/j.geomorph.2007.12.003
https://doi.org/10.1016/j.geomorph.2007.12.003
Publikováno v:
Quaternary International. 103:3-21
Auckland, in the north of New Zealand's North Island, is the largest urban area in the country, accommodating over a quarter of its population. The Auckland landscape is one of subdued rolling hills formed on weathered Mesozoic and Early Miocene sedi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3e1d5020ea50a1cadfb18717b7b8bd15
https://doi.org/10.1016/s1040-6182(02)00129-5
https://doi.org/10.1016/s1040-6182(02)00129-5
Publikováno v:
New Zealand Journal of Geology and Geophysics. 43:229-245
Remnants of four aggradational terraces in the lower 45 km of the main branch of the Waipaoa River have been correlated with cold/cool climate episodes of the Otiran glaciation. The youngest of the aggradation levels—the Waipaoa‐1 terrace—has t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3a5ff263f01b6e908fd7f9b3cb752518
https://doi.org/10.1080/00288306.2000.9514883
https://doi.org/10.1080/00288306.2000.9514883
Publikováno v:
Tectonics. 26
[1] Deformation across the active Hikurangi subduction margin, New Zealand, including shortening, extension, vertical-axis rotations, and strike-slip faulting in the upper plate, has been estimated for the last ∼24 Myr using margin-normal seismic r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4bc6301a2284efce61338ecaf1d19dc7
https://doi.org/10.1029/2006tc002090
https://doi.org/10.1029/2006tc002090