Late Quaternary Landscape Evolution and Fluvial Dynamics of the Hautapu River Catchment, New Zealand

2022 ◽  
Author(s):  
Szabolcs Kósik ◽  
Callum Rees ◽  
Alan S. Palmer ◽  
Malcolm Todd ◽  
Manuela Tost ◽  
...  
Keyword(s):  
New Zealand ◽  
Landscape Evolution ◽  
Late Quaternary ◽  
River Catchment ◽  
Fluvial Dynamics

scholarly journals Late Quaternary Tectonics, Incision, and Landscape Evolution of the Calchaquí River Catchment, Eastern Cordillera, NW Argentina

2019 ◽  
Vol 124 (8) ◽  
pp. 2265-2287 ◽  
Author(s):  
James A. McCarthy ◽  
Lindsay M. Schoenbohm ◽  
Paul R. Bierman ◽  
Dylan Rood ◽  
Alan J. Hidy
Keyword(s):  
Landscape Evolution ◽  
Late Quaternary ◽  
River Catchment ◽  
Eastern Cordillera

Late Quaternary loess landscape evolution on an active tectonic margin, Charwell Basin, South Island, New Zealand

Geomorphology ◽  
2010 ◽  
Vol 122 (3-4) ◽  
pp. 294-308 ◽  
Author(s):  
Matthew W. Hughes ◽  
Peter C. Almond ◽  
Joshua J. Roering ◽  
Philip J. Tonkin
Keyword(s):  
New Zealand ◽  
Landscape Evolution ◽  
Late Quaternary ◽  
Active Tectonic

Late Quaternary paleolimnology of Onepoto maar, Auckland, New Zealand: Implications for the drivers of regional paleoclimate

2012 ◽  
Vol 253 ◽  
pp. 18-31 ◽  
Author(s):  
Paul Augustinus ◽  
Ursula Cochran ◽  
Giri Kattel ◽  
Donna D’Costa ◽  
Phil Shane
Keyword(s):  
New Zealand ◽  
Late Quaternary

scholarly journals Holocene landscape evolution in the Baza Basin (SE-Spain) as indicated by fluvial dynamics of the Galera River

2021 ◽  
pp. 100030
Author(s):  
D. Wolf ◽  
F.J. García-Tortosa ◽  
C. Richter ◽  
J. Dabkowski ◽  
C. Roettig ◽  
...  
Keyword(s):  
Landscape Evolution ◽  
Se Spain ◽  
Fluvial Dynamics

Geodetic strain and the deformational history of the North Island of New Zealand during the late Cainozoic

1987 ◽  
Vol 321 (1557) ◽  
pp. 163-181 ◽  
Keyword(s):  
New Zealand ◽  
Subduction Zone ◽  
East Coast ◽  
Late Quaternary ◽  
Plate Boundary ◽  
Boundary Zone ◽  
Metamorphic Belt ◽  
Volcanic Region ◽  
The North ◽  
Plate Boundary Zone

The subduction zone under the east coast of the North Island of New Zealand comprises, from east to west, a frontal wedge, a fore-arc basin, uplifted basement forming the arc and the Central Volcanic Region. Reconstructions of the plate boundary zone for the Cainozoic from seafloor spreading data require the fore-arc basin to have rotated through 60° in the last 20 Ma which is confirmed by palaeomagnetic declination studies. Estimates of shear strain from geodetic data show that the fore-arc basin is rotating today and that it is under extension in the direction normal to the trend of the plate boundary zone. The extension is apparently achieved by normal faulting. Estimates of the amount of sediments accreted to the subduction zone exceed the volume of the frontal wedge: underplating by the excess sediments is suggested to be the cause of late Quaternary uplift of the fore-arc basin. Low-temperature—high-pressure metamorphism may therefore be occurring at depth on the east coast and high-temperature—low-pressure metamorphism is probable in the Central Volcanic Region. The North Island of New Zealand is therefore a likely setting for a paired metamorphic belt in the making.

Geomorphological features drive spatiotemporal dynamics of young‐of‐the‐year brown trout populations in a large New Zealand river catchment

2020 ◽  
Vol 65 (8) ◽  
pp. 1392-1400
Author(s):  
Pavel B. Mikheev ◽  
Matt G. Jarvis ◽  
Christoph D. Matthaei ◽  
Travis Ingram ◽  
Andrey I. Nikiforov ◽  
...  
Keyword(s):  
New Zealand ◽  
Brown Trout ◽  
Spatiotemporal Dynamics ◽  
River Catchment ◽  
Young Of The Year ◽  
Geomorphological Features
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