This means that during an earthquake, material is moved both upwards and also sideways. The Alpine fault is an example of one such hybrid fault – specifically a combination of a reverse fault and a strike-slip fault 1. The Alpine Fault is a mature, dextral strike-slip fault that marks the western boundary of the Southern Alps. It forms a transform boundary between the Pacific Plate and the Indo-Australian Plate. The Alpine Fault is called a strike slip or transform fault. The moment tensor solution is typically displayed graphically using a so-called beachball diagram. Check Flow F1-F4.pdf Check Flow Heating Failure.pdf Check Flow SPL & SPH.pdf Check Flow Bubble Failure.pdf Check Flow No Display on Control Panel.pdf Tips：To keep the filter pump and heater at a great performance, proper maintenance and cleaning of filter

In the case of the Alpine Fault, it’s the upward movement that interests me. The pattern of energy radiated during an earthquake with a single direction of motion on a single fault plane may be modelled as a double couple, which is described mathematically as a special case of a second order tensor (similar to those for stress and strain) known as the moment tensor. The Alpine Fault is a geological fault, specifically a right-lateral strike-slip fault, that runs almost the entire length of New Zealand’s South Island. Trouble Shooting Guide 5.1 The following Check Flow is as attached. The Australian plate is sliding horizontally towards the north-east, at the same time as the Pacific plate is pushing up, forming the Southern Alps. Earthquakes along the fault, and the associated earth movements, have formed the Southern Alps. Chapter 5.

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