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You might like to read my thoughts on what might really be happening: http://www.itwire.com/opinion-and-analysis/whiskey-tango-foxtrot/51963-a-theory-on-the-christchurch-earthquakes The Darfield fault, which caused the September 2010 earthquake, is the one just to the west of Christchurch. It was during this time that the cyclicality of the Alpine Fault earthquakes and meaning of the increase in metamorphic grade towards the fault was discovered and refined.The Deep Fault Drilling Project (DFDP) was an attempt in 2014 to retrieve rock and fluid samples and make geophysical measurements inside the Alpine Fault zone at depth.A right-lateral strike-slip fault, that runs almost the entire length of New Zealand's South Island.Movement along the Alpine Fault is deforming the microcontinent of In New Zealand, the South Island's alpine fault is a transform fault for much of its length. Many of the larger faults are The North Island Fault System is a major plate boundary feature in the North Island, under constant stress from movement between the Pacific and Australian plates. There are major fault lines running the length of New Zealand. There is paleotsunami evidence of near-simultaneous ruptures of the Alpine Fault and Wellington (and/or other major) faults to the North having occurred at least twice in the past 1,000 years.Richard Norris and Alan Cooper from the University of Otago conducted extensive research on the structure and petrology of the Alpine Fault respectively throughout the later 20th and early 21st centuries. We have secure vaults for you to store your valuables and precious metals such as bullion. Between 25 and 12 million years ago the movement on the proto-Alpine Fault was exclusively strike-slip. Deep earthquakes under North Island form a well defined band (seismic zone) running northeast from Marlborough through White Island. The corporation was founded as the Accident Compensation Commission on 1 April 1974 as a result of the Accident Compensation Act 1972.
Tectonic setting of Wairarapa fault, New Zealand, and spatial relation to Kaikoura Mw 7.8 2016 rupture.
Because of this during the mid 20th century it was speculated that the Alpine Fault creeps without making large earthquakes.There have been no major earthquakes on the Alpine Fault in historic times, its southern and
Can these volcanic earthquakes be as big as regular fault-line earthquakes? Shallow earthquakes tend to occur to the southeast of this seismic zone, while the deeper ones occur towards the northwest. Those that are considered likely to move again in the future are called active faults. Satalites using thermal etc to detect earthquakes upto 4 days b4 it happens, due to the huge amount of energy released from plate movement.
The area of volcanic activity is referred to as the Taupo Volcanic Zone (see map above).The subduction zone in the north is linked to the subduction zone in the south by a series of very large faults that run through Marlborough (Marlborough Fault System) and down the west coast of South Island (Alpine Fault). It runs as a single structure for over 500 km. This map effectively shows the areas where future earthquakes are most likely.This item has been provided for private study purposes (such as school projects, family and local history research) and any published reproduction (print or electronic) may infringe copyright law. Hope this is true and works.The Christchurch quake caused the fault line to appear it wasn't there before the quake. Also any studies being done on earthquake magnetic fields & beached whales in NZ & the possiblity of a new volcano surfacing?
You might like to read my thoughts on what might really be happening: http://www.itwire.com/opinion-and-analysis/whiskey-tango-foxtrot/51963-a-theory-on-the-christchurch-earthquakes The Darfield fault, which caused the September 2010 earthquake, is the one just to the west of Christchurch. It was during this time that the cyclicality of the Alpine Fault earthquakes and meaning of the increase in metamorphic grade towards the fault was discovered and refined.The Deep Fault Drilling Project (DFDP) was an attempt in 2014 to retrieve rock and fluid samples and make geophysical measurements inside the Alpine Fault zone at depth.A right-lateral strike-slip fault, that runs almost the entire length of New Zealand's South Island.Movement along the Alpine Fault is deforming the microcontinent of In New Zealand, the South Island's alpine fault is a transform fault for much of its length. Many of the larger faults are The North Island Fault System is a major plate boundary feature in the North Island, under constant stress from movement between the Pacific and Australian plates. There are major fault lines running the length of New Zealand. There is paleotsunami evidence of near-simultaneous ruptures of the Alpine Fault and Wellington (and/or other major) faults to the North having occurred at least twice in the past 1,000 years.Richard Norris and Alan Cooper from the University of Otago conducted extensive research on the structure and petrology of the Alpine Fault respectively throughout the later 20th and early 21st centuries. We have secure vaults for you to store your valuables and precious metals such as bullion. Between 25 and 12 million years ago the movement on the proto-Alpine Fault was exclusively strike-slip. Deep earthquakes under North Island form a well defined band (seismic zone) running northeast from Marlborough through White Island. The corporation was founded as the Accident Compensation Commission on 1 April 1974 as a result of the Accident Compensation Act 1972.
Tectonic setting of Wairarapa fault, New Zealand, and spatial relation to Kaikoura Mw 7.8 2016 rupture.
Because of this during the mid 20th century it was speculated that the Alpine Fault creeps without making large earthquakes.There have been no major earthquakes on the Alpine Fault in historic times, its southern and
Can these volcanic earthquakes be as big as regular fault-line earthquakes? Shallow earthquakes tend to occur to the southeast of this seismic zone, while the deeper ones occur towards the northwest. Those that are considered likely to move again in the future are called active faults. Satalites using thermal etc to detect earthquakes upto 4 days b4 it happens, due to the huge amount of energy released from plate movement.
The area of volcanic activity is referred to as the Taupo Volcanic Zone (see map above).The subduction zone in the north is linked to the subduction zone in the south by a series of very large faults that run through Marlborough (Marlborough Fault System) and down the west coast of South Island (Alpine Fault). It runs as a single structure for over 500 km. This map effectively shows the areas where future earthquakes are most likely.This item has been provided for private study purposes (such as school projects, family and local history research) and any published reproduction (print or electronic) may infringe copyright law. Hope this is true and works.The Christchurch quake caused the fault line to appear it wasn't there before the quake. Also any studies being done on earthquake magnetic fields & beached whales in NZ & the possiblity of a new volcano surfacing?