title: History of vertical displacement of Kerepehi Fault at Kopouatai bog, Hauraki Lowlands, New Zealand, since c. 10 700 years ago

authors: de Lange, P.J.

subjects: Faults

abstract: Thirteen tephra layers interbedded with peat, and a basal peathorizon, in four pairs of cores provide radiocarbon-dated reference horizons that indicate vertical displacement on the Kerepehi Fault at Kopouatai bog, Hauraki Lowlands. Progressive offset of the horizons with time shows that vertical fault movement, downthrown to the west, has been occurring for the past c. 10 700 radiocarbon years at an approximately uniform rate of c. 0.13 mm/yr. Step functions indicate faulting events earthquakes at c. 1400, c. 5600, c. 6800, and C. 9000 years ago, a mean recurrence interval of c. 2500 years. These findings support geophysical and geological evidence that the Hauraki Depression is an active rift, and show that active faulting occurs along the northern as well as southern extensions of the Kerepehi Fault. 
If such earthquakes occur randomly in time, and based on the return period of 2500 years, there are 2%, 18%, and 33% probabilities of a major earthquake affecting the Kerepehi Fault at Kopouatai bog in the next 50, 500, and 1000 years, respectively.

text: History of vertical displacement of Kerepehi Fault at Kopouatai bog, Hauraki Lowlands, New Zealand, since c. 10 700 years ago Thirteen tephra layers interbedded with peat, and a basal peathorizon, in four pairs of cores provide radiocarbon-dated reference horizons that indicate vertical displacement on the Kerepehi Fault at Kopouatai bog, Hauraki Lowlands. Progressive offset of the horizons with time shows that vertical fault movement, downthrown to the west, has been occurring for the past c. 10 700 radiocarbon years at an approximately uniform rate of c. 0.13 mm/yr. Step functions indicate faulting events earthquakes at c. 1400, c. 5600, c. 6800, and C. 9000 years ago, a mean recurrence interval of c. 2500 years. These findings support geophysical and geological evidence that the Hauraki Depression is an active rift, and show that active faulting occurs along the northern as well as southern extensions of the Kerepehi Fault. 
If such earthquakes occur randomly in time, and based on the return period of 2500 years, there are 2%, 18%, and 33% probabilities of a major earthquake affecting the Kerepehi Fault at Kopouatai bog in the next 50, 500, and 1000 years, respectively.

year: 1990

title: Stratigraphy, age, composition, and correlation of late Quaternary tephras interbedded with organic sediments in Waikato lakes, North Island, New Zealand

authors: Lowe, David J.

subjects: stratigraphy

abstract: Cores from 14 peaty lakes in the central Waikato region, northern North Island, contain a sequence of 41 well-preserved, mainly macroscopic, occasionally bedded, ash and lapilli layers ranging in thickness from c. 2 to 110 mm and interbedded with fine-grained organic lake sediment. The layers, whose field and compositional properties are described in detail, are distal airfall tephras that were erupted between c. 17000 and c. 1800 ¹⁴C years ago from six rhyolitic and andesitic volcanic centres located c. 70-200 km from the Waikato sites: Taupo (5 tephras), Okataina (7), Maroa (1) (rhyolitic); Mayor Island (2) (peralkaline); Tongariro (11), and Egmont (15) (andesitic).

text: Stratigraphy, age, composition, and correlation of late Quaternary tephras interbedded with organic sediments in Waikato lakes, North Island, New Zealand Cores from 14 peaty lakes in the central Waikato region, northern North Island, contain a sequence of 41 well-preserved, mainly macroscopic, occasionally bedded, ash and lapilli layers ranging in thickness from c. 2 to 110 mm and interbedded with fine-grained organic lake sediment. The layers, whose field and compositional properties are described in detail, are distal airfall tephras that were erupted between c. 17000 and c. 1800 ¹⁴C years ago from six rhyolitic and andesitic volcanic centres located c. 70-200 km from the Waikato sites: Taupo (5 tephras), Okataina (7), Maroa (1) (rhyolitic); Mayor Island (2) (peralkaline); Tongariro (11), and Egmont (15) (andesitic).

year: 1988

title: From mainstream to manaaki: Indigenising our approach to immigration

authors: Kukutai, Tahu

abstract: In recent years, discontent with migration and migrants in the wealthy global north has manifested in disturbing ways: cue Brexit, xenophobia, border paranoia, far-right nationalism and its bedfellow white supremacy. On the surface, Aotearoa New Zealand appears to have escaped the uglier aspects of this nativism. Despite the grumblings of the New Zealand First Party, no serious popular or political anti-immigration movement has appeared, and racially motivated attacks against migrants are relatively rare. This is despite the fact that Aotearoa has a much higher relative foreign-born population share than the United States or United Kingdom,1 and ‘superdiverse’ Auckland – which comprises at least 40 per cent migrants – now has the ignominious claim to being the fourthleast affordable city in the world, far outstripping London and New York.

text: From mainstream to manaaki: Indigenising our approach to immigration In recent years, discontent with migration and migrants in the wealthy global north has manifested in disturbing ways: cue Brexit, xenophobia, border paranoia, far-right nationalism and its bedfellow white supremacy. On the surface, Aotearoa New Zealand appears to have escaped the uglier aspects of this nativism. Despite the grumblings of the New Zealand First Party, no serious popular or political anti-immigration movement has appeared, and racially motivated attacks against migrants are relatively rare. This is despite the fact that Aotearoa has a much higher relative foreign-born population share than the United States or United Kingdom,1 and ‘superdiverse’ Auckland – which comprises at least 40 per cent migrants – now has the ignominious claim to being the fourthleast affordable city in the world, far outstripping London and New York.

year: 2017