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1
Introduction
2
Research team
3
Where is it
4
Seismic lines
5
Subduction margin
6
Volcanism
7
Weather
8
Canyons
9
The last glacial maximum
10
Kaikoura earthquake simulation
11
Landslide
12
Earthquake shaking
13
Kaikala Canyon
14
Chasing the signal
15
Coseismic turbolite
16
Coseismic event beds
17
Macro tephras
18
Madden Canyon
19
Isotope stratigraphy
20
CT scans
21
Conclusions
22
Sediment waves
23
Hikurangi subduction zone
24
Questions
25
Dan Tech
Description:
Explore the fascinating geological features and processes of the Hikurangi Channel off New Zealand's east coast in this 49-minute lecture. Delve into the complex interplay of earthquakes, volcanism, and sedimentary processes that shape this massive deep marine channel. Learn about the channel's unique characteristics, including its exceptional length and the vast amounts of sediment it transports. Examine how researchers are using turbidite records and core samples to unravel the region's Quaternary earthquake and volcanic history. Gain insights into the Hikurangi Subduction Margin, the Taupō Volcanic Zone, and their impacts on sediment transport. Discover the latest findings from IODP site 1520 and multiple Holocene-aged short cores, and understand how these contribute to our knowledge of this dynamic geological system.

Chasing Earthquake and Volcanism Signals in a Deep Marine Channel - The Hikurangi Channel New Zealand

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